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description Publicationkeyboard_double_arrow_right Article 2024 ItalyPublisher:Elsevier BV Morabito, C.; Papazzoni, C. A.; Lehrmann, D. J.; Payne, J. L.; Al-Ramadan, K.; Morsilli, M.;handle: 11392/2535353
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You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106575&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, SpainPublisher:Elsevier BV Authors: Criniti S.; Martin-Martin M.; Martin-Algarra A.;Criniti S.; Martin-Martin M.; Martin-Algarra A.;handle: 10045/138123 , 20.500.11770/360938
Carboniferous sandstone within the Paleo-Mesomediterranean Domain (Malaguide Subdomain), in southern Spain, represents a key detrital mode within the sedimentary budget of convergent plate boundaries during the Variscan s.s. to Paleotethysian orogenic time span (≈ 420–300 Ma). This Carboniferous detritus corresponds with Culm lithostratigraphic depositional unit, and it covers an important gap of information (paleogeographic, paleotectonic, source areas) to the area located between the Iberian-French massifs and the African Paleo-Atlas, in the western Paleotethys. Sandstone composition is quartzolithic and records an important high-to-medium-low grade metamorphic content. The source area was a lithic and transitional recycled orogen with a signature of volcanic and ophiolitic detritus (≈ 330 Ma and/or older). These supplies seem to be derived from a mid-crustal deformed and thrusted Cambrian to lower Carboniferous terrane, involved in the plate convergence (the southern Europe Iberian-French massifs overriding the north African area) of the Variscan s.s. orogenic system, rapidly exhumed and uplifted. Consequently, in the overriding hinterland (southern Europe: Iberian-French massifs), a Pre-middle Carboniferous metamorphic basement should be already structured during middle Carboniferous when thrusting took place, suggesting Proterozoic-Early Carboniferous (most probably, ≈ 420 to 330 Ma) metamorphic highlands. The presence of serpentinite-like detritus (≈ 330 Ma and/or older) seems to indicate a metamorphosed oceanic crust being dismantled at that time, thus, ophiolitic sutures (most probably developed at ≈ 420–330 Ma) zones are tentatively proposed at the northern Gondwana. The occurrence of a synsedimentary volcanic activity (andesitic) should be related to a lost magmatic arc (most probably developed at ≈ 360–330 Ma), reinforcing the idea of a nearby subduction area. Therefore, the thick terrigenous Culm deposits (≈ 330–300 Ma) from the Malaguide Subdomain could be deposited in a complex foreland system basin connected northward with carbonate platforms and with a crystalline highland uplifted domain from the southern Europe Iberian-French massifs and southward with the African Paleo-Atlas Domain. The studied middle-late Carboniferous sandstone petrofacies deeply contributes to paleogeographic reconstructions since blocks fragmentation and spreading, during the Paleotethysian and Alpine orogenies, rearranged the Paleozoic paleogeography now part of the Cenozoic Perimediterranean Chains. After the correlation with the Carboniferous from other western Paleotethys domains, new paleogeographic-paleotectonic constraints are proposed for the transitional area between the Iberian-French massifs and the African Paleo-Atlas Domain. Research Project PID2020-114381GB-I00 to M. Martín-Martín, Spanish Ministry of Education and Science; Research Groups and Projects of the Generalitat Valenciana, Alicante University (CTMA-IGA) are acknowledged. Support from Ministero Italiano dell'Università e della Ricerca Scientifica to S. Criniti, is also acknowledged.
Sedimentary Geology;... arrow_drop_down Sedimentary Geology; Archivio Istituzionale dell'Università della CalabriaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106534Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Sedimentary Geology;... arrow_drop_down Sedimentary Geology; Archivio Istituzionale dell'Università della CalabriaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106534Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106534&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, GermanyPublisher:Elsevier BV Angana Chaudhuri; Jan Schönig; Emilia Le Pera; Hilmar von Eynatten; Gaurav Chauhan; Nils Keno Lünsdorf;handle: 20.500.11770/350737
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For further information contact us at helpdesk@openaire.eu3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2023 Spain, GermanyPublisher:Elsevier BV Authors: Martín Martín, Manuel; Tosquella Angrill, Josep; Guerrera, Francesco; Maaté, Ali; +4 AuthorsMartín Martín, Manuel; Tosquella Angrill, Josep; Guerrera, Francesco; Maaté, Ali; Hlila, Rachid; Maaté, Soufian; Tramontana, Mario; Le Breton, Eline;handle: 10045/134551 , 10272/22413
The Eocene platforms deposits in the Moroccan Ghomarides have been studied in this paper. These marine carbonate platforms were located in the westernmost Tethys approximately 30°N and 0°–10°W during the Cuisian to Bartonian. This study includes observations from fossiliferous assemblages (such as larger benthic foraminifera and colonial corals), their paleoenvironment as well as rock texture and fabric. Eight microfacies were identified that represent different ramp environments in a ‘distally-steepened carbonate ramp’ type of platform. The studied deposits are organised into a transgressive succession composed of three sedimentary cycles: lower Cuisian, middle Cuisian and middle Lutetian to Bartonian. In the lower cycle, photic inner to middle ramp environments in mesotrophic conditions were prevalent. In the second cycle, photic inner ramp (sea-grass) to mid ramp environments in mesotrophic to oligotrophic conditions were observed. The upper cycle, which is more extensive and variable, represents mesophotic mid ramp to aphotic slope environments and change gradually from oligotrophic to eutrophic conditions. During the Eocene, larger benthic foraminifera were dominant overtaking the zooxanthellate corals in the Tethys regions. Nevertheless, our study and the performed comparison with other Tethyan sectors have revealed that in some areas both coexisted in similar proportions. In some western Tethys regions close to the Atlantic Ocean, coinciding with areas influenced by upwelling currents, larger benthic foraminifera and coral build-ups were replaced by oyster reefs. The Ghomaride Domain represents an intermediate case between fossil assemblages of northern Tethyan margin and eastern sector of the southern margin of the Tethys, with a dominance of larger benthic foraminifera but with a certain presence of corals as well. A good correlation exists between Eocene warm intervals and carbonate platform deposits in these domains. Contrarily, during cooling ones shallowing and gaps in the sedimentation is registered. Two anomalies have been detected in the Ghomaride Domain during Ypresian and Bartonian times indicating particular climatic conditions or local tectonics interferences. Research supported by: Research Project PID2020-114381GB-I00, Spanish Ministry of Science and Innovation; Research Groups and Projects from M. Martín-Martín, Alicante University (CTMA-IGA).
Refubium - Repositor... arrow_drop_down Refubium - Repositorium der Freien Universität BerlinArticle . 2023License: CC BY NC NDData sources: Refubium - Repositorium der Freien Universität BerlinSedimentary Geology; Arias Montano, Repositorio Institucional de la Universidad de HuelvaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106423Data sources: Recolector de Ciencia Abierta, RECOLECTAhttps://doi.org/10.17169/refub...Other literature type . 2023License: CC BY NC NDData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Average influence Average impulse Average Powered by BIP!more_vert Refubium - Repositor... arrow_drop_down Refubium - Repositorium der Freien Universität BerlinArticle . 2023License: CC BY NC NDData sources: Refubium - Repositorium der Freien Universität BerlinSedimentary Geology; Arias Montano, Repositorio Institucional de la Universidad de HuelvaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106423Data sources: Recolector de Ciencia Abierta, RECOLECTAhttps://doi.org/10.17169/refub...Other literature type . 2023License: CC BY NC NDData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Andrea Sorci; Simonetta Cirilli; Amalia Spina; Mansour Ghorbani; Roberto Rettori;handle: 11391/1548724
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You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106370&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106370&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Spain, GermanyPublisher:Elsevier BV Authors: Martín-Martín, Manuel; Guerrera, Francesco; Cañaveras, Juan C.; Alcalá, Francisco J.; +7 AuthorsMartín-Martín, Manuel; Guerrera, Francesco; Cañaveras, Juan C.; Alcalá, Francisco J.; Serrano, Francisco; Maaté, Ali; Hlila, Rachid; Maaté, Soufian; Tramontana, Mario; Sánchez-Navas, Antonio; Le Breton, Eline;handle: 10045/132880 , 10481/82240
The Paleogene evolution of the NW margin of the African Plate (Western External Rif Zone) was studied by means of multidisciplinary analyses of twenty-one stratigraphic logs, including tectofacies recognition, petro-mineralogical results, and thicknesses analysis. Four stratigraphic intervals were recognized separated by three unconformities coarsely aligned with the Cretaceous–Paleogene, Eocene–Oligocene and Oligocene–Miocene boundaries, respectively. Tectofacies appear from the late Ypresian being more frequents from the Oligocene as the tectonic activity increases. The petrology of detrital suites indicates recycled orogen-derived sediments, with quartz supplied from metamorphic rocks of the Atlas orogen and/or the African craton. On the basis of Mesozoic clay mineral assemblages reported in the literature, the clay mineralogy of mudstones suggests upper Jurassic to upper Cretaceous terrains from the Internal Intrarif as the main source area of the Paleocene–Eocene successions, with sediment provenance reversion during the Oligocene and additional contribution of Paleocene to lower Eocene suites. The different displacement capability of the identified aluminic-magnesic clay mineralogy enabled to deduce the relative proximity of the source area. These findings point out a complex sedimentary evolution characterized by a mixture of different lithotypes dating back to upper Jurassic. X-ray parameters helped to identify evidences of synsedimentary tectonics overprinting the inherited mineralogy during some periods with weak burial diagenesis at most. During the Paleogene a foreland basin is formed mainly in the Mesorif and Prerif sub-domains. This foredeep was represented by two ‘sub-geosynclines’ separated by a relative bulge located in the External Mesorif. The Internal Intrarif could represent the relative orogenic front, advancing on the External Intrarif. The Eocene forebulge was located in the Ridges Domain, while the Gharb Basin was the backbulge of the system. During the Oligocene the depocentral area migrated southward and a homogeneization of thicknesses took also place in the whole margin. In this new configuration, the foredeep would be located in the External Mesorif (previously a relative bulge) while the Ridges Domain and the Gharb Basin continued to act as the system forebulge and backbulge, respectively. A comparison with the Paleogene evolution of other western Tethys external margins (Betic Chain, Tunisian Tell, Sicilian Maghrebids, and Apennines) has revealed more similarities than differences. The effects of the Eo-Alpine tectonics are recognized everywhere even if they decrease both from N to S, and from W to E in the different considered margins. The evolution of the compared margins shows a common pre-foredeed (Paleocene-Eocene) and beginning of foredeep (Oligocene) stages in the foreland basins. Research supported by PID2020-114381GB-I00 research project (Spanish Ministry of Education and Science), Research Groups and projects of the Generalitat Valenciana from Alicante University (CTMA-IGA).
Repositorio Instituc... arrow_drop_down Repositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRefubium - Repositorium der Freien Universität BerlinOther literature type . Article . 2023License: CC BY NC NDRepositorio Institucional Universidad de GranadaArticle . 2023Data sources: Repositorio Institucional Universidad de GranadaRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106367Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Repositorio Instituc... arrow_drop_down Repositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRefubium - Repositorium der Freien Universität BerlinOther literature type . Article . 2023License: CC BY NC NDRepositorio Institucional Universidad de GranadaArticle . 2023Data sources: Repositorio Institucional Universidad de GranadaRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106367Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, NetherlandsPublisher:Elsevier BV Authors: 1 Athina Tzevahirtzian; 1 Antonio Caruso; 2 Federico Andreetto; 3 Sergio Bonomo; +1 Authors1 Athina Tzevahirtzian; 1 Antonio Caruso; 2 Federico Andreetto; 3 Sergio Bonomo; 2 Wout Krijgsman;The late Miocene deposits from core 3AGN2S04, located in the northern Caltanissetta Basin (Sicily), display the pre-Messinian Salinity Crisis (MSC) and the MSC events. The present study describes the entire core in terms of lithology, biostratigraphy and magnetostratigraphy and aims to enlighten the relationship between MSC evaporite cyclicity and astronomical forcing. The lithological and micro-/macro-paleontological descriptions document the MSC record, with Stage 1 (onset and Calcare di Base member), Stage 2 (Messinian Erosional Surface) and part of Stage 3 (Upper Gypsum and Lago Mare). Detailed micro-fossil analyses of the pre-evaporites reveal several biostratigraphic events that permit correlations to the well-dated Mediterranean planktonic foraminiferal biostratigraphic zonation of the late Tortonian and Messinian. An integrated bio-cyclostratigraphic analysis allows bed-to-bed correlations of core 3AGN2S04 with the reference sections of Falconara/Gibliscemi (Sicily) and Sorbas (Spain), but also with various other sections from the Caltanissetta Basin. Our cyclostratigraphic correlations show a stratigraphical gap in the core between the late Tortonian Terravecchia Formation and the pre-evaporitic Messinian Tripoli Formation. This hiatus is probably related to the tectonically active geological setting of the northern Caltanissetta Basin. Finally, we show that the repercussions of the paleoenvironmental evolution towards evaporitic deposition and the MSC onset seem to have been diachronous throughout the various perched basins on Sicily characterized by different paleobathymetries. In particular, the onset of the Calcare di Base took place around 40-100 ka before the deposition of the first gypsum bed of the Primary Lower Gypsum units.(c) 2023 Elsevier B.V. All rights reserved.
Utrecht University R... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Utrecht University R... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Authors: Riaz, Muhammad; Jafarian, Arman; Koeshidayatullah, Ardiansyah; Frontalini, Fabrizio; +3 AuthorsRiaz, Muhammad; Jafarian, Arman; Koeshidayatullah, Ardiansyah; Frontalini, Fabrizio; Jiang, Lei; Latif, Khalid; Zafar, Tehseen;handle: 11576/2709219
Archivio istituziona... arrow_drop_down Sedimentary Geology; Archivio istituzionale della ricerca - Università di UrbinoArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Sedimentary Geology; Archivio istituzionale della ricerca - Università di UrbinoArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2022 Germany, ItalyPublisher:Elsevier BV Authors: Timothy O. Tella; Gerd Winterleitner; Michele Morsilli; Maria Mutti;Timothy O. Tella; Gerd Winterleitner; Michele Morsilli; Maria Mutti;handle: 11392/2507230
Although distally steepened carbonate ramps have been studied by numerous researchers, the processes that control the development of these carbonate systems, including tectonics, differential carbonate production along the ramp profile, or antecedent physiography of the slopes, are an ongoing discussion. We use a stratigraphic forward model to test different hypotheses to unravel controls over distally steepened ramp development, referenced to the well-known Upper Miocene Menorca carbonate ramp (Spain). Sensitivity tests show that distally steepened ramps develop under complex interaction among accommodation, carbonate production and sediment transport parameters. Ramp slope initiation is favoured by still stands and falls of sea-level, in a setting with high-frequency sea-level fluctuations with amplitude between 20 m and 40 m. Low-frequency and higher amplitude sea-level fluctuations of about 115 m tend to form models with no significant slope development. The impact of antecedent slope on the geometry of ramps is determined by the paleoslope inclination, with flat to subhorizontal paleosurfaces resulting in ramps that mirror the antecedent slope. In contrast, steeper paleosurfaces tend to result in ramps with well-defined slopes. Our models, therefore, show that the ramp profile becomes more influenced by the depth constraints on the carbonate sediment producers than by the geometry of the underlying topography as the inclination of the paleosurface increases. The presented models also show that seagrass-dominated shallow carbonate production tends to result in steep slopes due to the low-transport characteristic imposed by seagrass trapping. This steepness can, however, be altered by the introduction of high transport sediment grains from deeper carbonate producers, which fill the slopes and more distal sections of the ramp profile.
GFZ German Research ... arrow_drop_down GFZ German Research Centre for GeosciencesArticle . 2022Data sources: GFZ German Research Centre for GeosciencesArchivio istituzionale della ricerca - Università di Ferrara; Sedimentary GeologyArticle . 2022 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106267&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert GFZ German Research ... arrow_drop_down GFZ German Research Centre for GeosciencesArticle . 2022Data sources: GFZ German Research Centre for GeosciencesArchivio istituzionale della ricerca - Università di Ferrara; Sedimentary GeologyArticle . 2022 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2022 ItalyPublisher:Elsevier BV Brandano M.; Tomassetti L.; Di Bella L.; Barberio D. M.; Barbieri M.; Ferrini A.;handle: 11573/1661052
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106235&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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description Publicationkeyboard_double_arrow_right Article 2024 ItalyPublisher:Elsevier BV Morabito, C.; Papazzoni, C. A.; Lehrmann, D. J.; Payne, J. L.; Al-Ramadan, K.; Morsilli, M.;handle: 11392/2535353
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You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106575&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, SpainPublisher:Elsevier BV Authors: Criniti S.; Martin-Martin M.; Martin-Algarra A.;Criniti S.; Martin-Martin M.; Martin-Algarra A.;handle: 10045/138123 , 20.500.11770/360938
Carboniferous sandstone within the Paleo-Mesomediterranean Domain (Malaguide Subdomain), in southern Spain, represents a key detrital mode within the sedimentary budget of convergent plate boundaries during the Variscan s.s. to Paleotethysian orogenic time span (≈ 420–300 Ma). This Carboniferous detritus corresponds with Culm lithostratigraphic depositional unit, and it covers an important gap of information (paleogeographic, paleotectonic, source areas) to the area located between the Iberian-French massifs and the African Paleo-Atlas, in the western Paleotethys. Sandstone composition is quartzolithic and records an important high-to-medium-low grade metamorphic content. The source area was a lithic and transitional recycled orogen with a signature of volcanic and ophiolitic detritus (≈ 330 Ma and/or older). These supplies seem to be derived from a mid-crustal deformed and thrusted Cambrian to lower Carboniferous terrane, involved in the plate convergence (the southern Europe Iberian-French massifs overriding the north African area) of the Variscan s.s. orogenic system, rapidly exhumed and uplifted. Consequently, in the overriding hinterland (southern Europe: Iberian-French massifs), a Pre-middle Carboniferous metamorphic basement should be already structured during middle Carboniferous when thrusting took place, suggesting Proterozoic-Early Carboniferous (most probably, ≈ 420 to 330 Ma) metamorphic highlands. The presence of serpentinite-like detritus (≈ 330 Ma and/or older) seems to indicate a metamorphosed oceanic crust being dismantled at that time, thus, ophiolitic sutures (most probably developed at ≈ 420–330 Ma) zones are tentatively proposed at the northern Gondwana. The occurrence of a synsedimentary volcanic activity (andesitic) should be related to a lost magmatic arc (most probably developed at ≈ 360–330 Ma), reinforcing the idea of a nearby subduction area. Therefore, the thick terrigenous Culm deposits (≈ 330–300 Ma) from the Malaguide Subdomain could be deposited in a complex foreland system basin connected northward with carbonate platforms and with a crystalline highland uplifted domain from the southern Europe Iberian-French massifs and southward with the African Paleo-Atlas Domain. The studied middle-late Carboniferous sandstone petrofacies deeply contributes to paleogeographic reconstructions since blocks fragmentation and spreading, during the Paleotethysian and Alpine orogenies, rearranged the Paleozoic paleogeography now part of the Cenozoic Perimediterranean Chains. After the correlation with the Carboniferous from other western Paleotethys domains, new paleogeographic-paleotectonic constraints are proposed for the transitional area between the Iberian-French massifs and the African Paleo-Atlas Domain. Research Project PID2020-114381GB-I00 to M. Martín-Martín, Spanish Ministry of Education and Science; Research Groups and Projects of the Generalitat Valenciana, Alicante University (CTMA-IGA) are acknowledged. Support from Ministero Italiano dell'Università e della Ricerca Scientifica to S. Criniti, is also acknowledged.
Sedimentary Geology;... arrow_drop_down Sedimentary Geology; Archivio Istituzionale dell'Università della CalabriaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106534Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Sedimentary Geology;... arrow_drop_down Sedimentary Geology; Archivio Istituzionale dell'Università della CalabriaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106534Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106534&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, GermanyPublisher:Elsevier BV Angana Chaudhuri; Jan Schönig; Emilia Le Pera; Hilmar von Eynatten; Gaurav Chauhan; Nils Keno Lünsdorf;handle: 20.500.11770/350737
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For further information contact us at helpdesk@openaire.eu3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2023 Spain, GermanyPublisher:Elsevier BV Authors: Martín Martín, Manuel; Tosquella Angrill, Josep; Guerrera, Francesco; Maaté, Ali; +4 AuthorsMartín Martín, Manuel; Tosquella Angrill, Josep; Guerrera, Francesco; Maaté, Ali; Hlila, Rachid; Maaté, Soufian; Tramontana, Mario; Le Breton, Eline;handle: 10045/134551 , 10272/22413
The Eocene platforms deposits in the Moroccan Ghomarides have been studied in this paper. These marine carbonate platforms were located in the westernmost Tethys approximately 30°N and 0°–10°W during the Cuisian to Bartonian. This study includes observations from fossiliferous assemblages (such as larger benthic foraminifera and colonial corals), their paleoenvironment as well as rock texture and fabric. Eight microfacies were identified that represent different ramp environments in a ‘distally-steepened carbonate ramp’ type of platform. The studied deposits are organised into a transgressive succession composed of three sedimentary cycles: lower Cuisian, middle Cuisian and middle Lutetian to Bartonian. In the lower cycle, photic inner to middle ramp environments in mesotrophic conditions were prevalent. In the second cycle, photic inner ramp (sea-grass) to mid ramp environments in mesotrophic to oligotrophic conditions were observed. The upper cycle, which is more extensive and variable, represents mesophotic mid ramp to aphotic slope environments and change gradually from oligotrophic to eutrophic conditions. During the Eocene, larger benthic foraminifera were dominant overtaking the zooxanthellate corals in the Tethys regions. Nevertheless, our study and the performed comparison with other Tethyan sectors have revealed that in some areas both coexisted in similar proportions. In some western Tethys regions close to the Atlantic Ocean, coinciding with areas influenced by upwelling currents, larger benthic foraminifera and coral build-ups were replaced by oyster reefs. The Ghomaride Domain represents an intermediate case between fossil assemblages of northern Tethyan margin and eastern sector of the southern margin of the Tethys, with a dominance of larger benthic foraminifera but with a certain presence of corals as well. A good correlation exists between Eocene warm intervals and carbonate platform deposits in these domains. Contrarily, during cooling ones shallowing and gaps in the sedimentation is registered. Two anomalies have been detected in the Ghomaride Domain during Ypresian and Bartonian times indicating particular climatic conditions or local tectonics interferences. Research supported by: Research Project PID2020-114381GB-I00, Spanish Ministry of Science and Innovation; Research Groups and Projects from M. Martín-Martín, Alicante University (CTMA-IGA).
Refubium - Repositor... arrow_drop_down Refubium - Repositorium der Freien Universität BerlinArticle . 2023License: CC BY NC NDData sources: Refubium - Repositorium der Freien Universität BerlinSedimentary Geology; Arias Montano, Repositorio Institucional de la Universidad de HuelvaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106423Data sources: Recolector de Ciencia Abierta, RECOLECTAhttps://doi.org/10.17169/refub...Other literature type . 2023License: CC BY NC NDData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Average influence Average impulse Average Powered by BIP!more_vert Refubium - Repositor... arrow_drop_down Refubium - Repositorium der Freien Universität BerlinArticle . 2023License: CC BY NC NDData sources: Refubium - Repositorium der Freien Universität BerlinSedimentary Geology; Arias Montano, Repositorio Institucional de la Universidad de HuelvaArticle . 2023 . Peer-reviewedLicense: CC BY NC NDRepositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106423Data sources: Recolector de Ciencia Abierta, RECOLECTAhttps://doi.org/10.17169/refub...Other literature type . 2023License: CC BY NC NDData sources: Dataciteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Andrea Sorci; Simonetta Cirilli; Amalia Spina; Mansour Ghorbani; Roberto Rettori;handle: 11391/1548724
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For further information contact us at helpdesk@openaire.euAccess Routeshybrid 3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Spain, GermanyPublisher:Elsevier BV Authors: Martín-Martín, Manuel; Guerrera, Francesco; Cañaveras, Juan C.; Alcalá, Francisco J.; +7 AuthorsMartín-Martín, Manuel; Guerrera, Francesco; Cañaveras, Juan C.; Alcalá, Francisco J.; Serrano, Francisco; Maaté, Ali; Hlila, Rachid; Maaté, Soufian; Tramontana, Mario; Sánchez-Navas, Antonio; Le Breton, Eline;handle: 10045/132880 , 10481/82240
The Paleogene evolution of the NW margin of the African Plate (Western External Rif Zone) was studied by means of multidisciplinary analyses of twenty-one stratigraphic logs, including tectofacies recognition, petro-mineralogical results, and thicknesses analysis. Four stratigraphic intervals were recognized separated by three unconformities coarsely aligned with the Cretaceous–Paleogene, Eocene–Oligocene and Oligocene–Miocene boundaries, respectively. Tectofacies appear from the late Ypresian being more frequents from the Oligocene as the tectonic activity increases. The petrology of detrital suites indicates recycled orogen-derived sediments, with quartz supplied from metamorphic rocks of the Atlas orogen and/or the African craton. On the basis of Mesozoic clay mineral assemblages reported in the literature, the clay mineralogy of mudstones suggests upper Jurassic to upper Cretaceous terrains from the Internal Intrarif as the main source area of the Paleocene–Eocene successions, with sediment provenance reversion during the Oligocene and additional contribution of Paleocene to lower Eocene suites. The different displacement capability of the identified aluminic-magnesic clay mineralogy enabled to deduce the relative proximity of the source area. These findings point out a complex sedimentary evolution characterized by a mixture of different lithotypes dating back to upper Jurassic. X-ray parameters helped to identify evidences of synsedimentary tectonics overprinting the inherited mineralogy during some periods with weak burial diagenesis at most. During the Paleogene a foreland basin is formed mainly in the Mesorif and Prerif sub-domains. This foredeep was represented by two ‘sub-geosynclines’ separated by a relative bulge located in the External Mesorif. The Internal Intrarif could represent the relative orogenic front, advancing on the External Intrarif. The Eocene forebulge was located in the Ridges Domain, while the Gharb Basin was the backbulge of the system. During the Oligocene the depocentral area migrated southward and a homogeneization of thicknesses took also place in the whole margin. In this new configuration, the foredeep would be located in the External Mesorif (previously a relative bulge) while the Ridges Domain and the Gharb Basin continued to act as the system forebulge and backbulge, respectively. A comparison with the Paleogene evolution of other western Tethys external margins (Betic Chain, Tunisian Tell, Sicilian Maghrebids, and Apennines) has revealed more similarities than differences. The effects of the Eo-Alpine tectonics are recognized everywhere even if they decrease both from N to S, and from W to E in the different considered margins. The evolution of the compared margins shows a common pre-foredeed (Paleocene-Eocene) and beginning of foredeep (Oligocene) stages in the foreland basins. Research supported by PID2020-114381GB-I00 research project (Spanish Ministry of Education and Science), Research Groups and projects of the Generalitat Valenciana from Alicante University (CTMA-IGA).
Repositorio Instituc... arrow_drop_down Repositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRefubium - Repositorium der Freien Universität BerlinOther literature type . Article . 2023License: CC BY NC NDRepositorio Institucional Universidad de GranadaArticle . 2023Data sources: Repositorio Institucional Universidad de GranadaRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106367Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Repositorio Instituc... arrow_drop_down Repositorio Institucional de la Universidad de AlicanteArticle . 2023Data sources: Repositorio Institucional de la Universidad de AlicanteRefubium - Repositorium der Freien Universität BerlinOther literature type . Article . 2023License: CC BY NC NDRepositorio Institucional Universidad de GranadaArticle . 2023Data sources: Repositorio Institucional Universidad de GranadaRecolector de Ciencia Abierta, RECOLECTAArticle . 2023Full-Text: https://doi.org/10.1016/j.sedgeo.2023.106367Data sources: Recolector de Ciencia Abierta, RECOLECTAadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106367&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Italy, NetherlandsPublisher:Elsevier BV Authors: 1 Athina Tzevahirtzian; 1 Antonio Caruso; 2 Federico Andreetto; 3 Sergio Bonomo; +1 Authors1 Athina Tzevahirtzian; 1 Antonio Caruso; 2 Federico Andreetto; 3 Sergio Bonomo; 2 Wout Krijgsman;The late Miocene deposits from core 3AGN2S04, located in the northern Caltanissetta Basin (Sicily), display the pre-Messinian Salinity Crisis (MSC) and the MSC events. The present study describes the entire core in terms of lithology, biostratigraphy and magnetostratigraphy and aims to enlighten the relationship between MSC evaporite cyclicity and astronomical forcing. The lithological and micro-/macro-paleontological descriptions document the MSC record, with Stage 1 (onset and Calcare di Base member), Stage 2 (Messinian Erosional Surface) and part of Stage 3 (Upper Gypsum and Lago Mare). Detailed micro-fossil analyses of the pre-evaporites reveal several biostratigraphic events that permit correlations to the well-dated Mediterranean planktonic foraminiferal biostratigraphic zonation of the late Tortonian and Messinian. An integrated bio-cyclostratigraphic analysis allows bed-to-bed correlations of core 3AGN2S04 with the reference sections of Falconara/Gibliscemi (Sicily) and Sorbas (Spain), but also with various other sections from the Caltanissetta Basin. Our cyclostratigraphic correlations show a stratigraphical gap in the core between the late Tortonian Terravecchia Formation and the pre-evaporitic Messinian Tripoli Formation. This hiatus is probably related to the tectonically active geological setting of the northern Caltanissetta Basin. Finally, we show that the repercussions of the paleoenvironmental evolution towards evaporitic deposition and the MSC onset seem to have been diachronous throughout the various perched basins on Sicily characterized by different paleobathymetries. In particular, the onset of the Calcare di Base took place around 40-100 ka before the deposition of the first gypsum bed of the Primary Lower Gypsum units.(c) 2023 Elsevier B.V. All rights reserved.
Utrecht University R... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106330&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Utrecht University R... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2023.106330&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Authors: Riaz, Muhammad; Jafarian, Arman; Koeshidayatullah, Ardiansyah; Frontalini, Fabrizio; +3 AuthorsRiaz, Muhammad; Jafarian, Arman; Koeshidayatullah, Ardiansyah; Frontalini, Fabrizio; Jiang, Lei; Latif, Khalid; Zafar, Tehseen;handle: 11576/2709219
Archivio istituziona... arrow_drop_down Sedimentary Geology; Archivio istituzionale della ricerca - Università di UrbinoArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106301&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 3 citations 3 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Sedimentary Geology; Archivio istituzionale della ricerca - Università di UrbinoArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106301&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2022 Germany, ItalyPublisher:Elsevier BV Authors: Timothy O. Tella; Gerd Winterleitner; Michele Morsilli; Maria Mutti;Timothy O. Tella; Gerd Winterleitner; Michele Morsilli; Maria Mutti;handle: 11392/2507230
Although distally steepened carbonate ramps have been studied by numerous researchers, the processes that control the development of these carbonate systems, including tectonics, differential carbonate production along the ramp profile, or antecedent physiography of the slopes, are an ongoing discussion. We use a stratigraphic forward model to test different hypotheses to unravel controls over distally steepened ramp development, referenced to the well-known Upper Miocene Menorca carbonate ramp (Spain). Sensitivity tests show that distally steepened ramps develop under complex interaction among accommodation, carbonate production and sediment transport parameters. Ramp slope initiation is favoured by still stands and falls of sea-level, in a setting with high-frequency sea-level fluctuations with amplitude between 20 m and 40 m. Low-frequency and higher amplitude sea-level fluctuations of about 115 m tend to form models with no significant slope development. The impact of antecedent slope on the geometry of ramps is determined by the paleoslope inclination, with flat to subhorizontal paleosurfaces resulting in ramps that mirror the antecedent slope. In contrast, steeper paleosurfaces tend to result in ramps with well-defined slopes. Our models, therefore, show that the ramp profile becomes more influenced by the depth constraints on the carbonate sediment producers than by the geometry of the underlying topography as the inclination of the paleosurface increases. The presented models also show that seagrass-dominated shallow carbonate production tends to result in steep slopes due to the low-transport characteristic imposed by seagrass trapping. This steepness can, however, be altered by the introduction of high transport sediment grains from deeper carbonate producers, which fill the slopes and more distal sections of the ramp profile.
GFZ German Research ... arrow_drop_down GFZ German Research Centre for GeosciencesArticle . 2022Data sources: GFZ German Research Centre for GeosciencesArchivio istituzionale della ricerca - Università di Ferrara; Sedimentary GeologyArticle . 2022 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106267&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert GFZ German Research ... arrow_drop_down GFZ German Research Centre for GeosciencesArticle . 2022Data sources: GFZ German Research Centre for GeosciencesArchivio istituzionale della ricerca - Università di Ferrara; Sedimentary GeologyArticle . 2022 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106267&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2022 ItalyPublisher:Elsevier BV Brandano M.; Tomassetti L.; Di Bella L.; Barberio D. M.; Barbieri M.; Ferrini A.;handle: 11573/1661052
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106235&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.sedgeo.2022.106235&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu