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description Publicationkeyboard_double_arrow_right Article 2015 Netherlands, France, Netherlands, NetherlandsPublisher:Elsevier BV Jean-Pierre Suc; Speranta Maria Popescu; Damien Do Couto; Georges Clauzon; Jean Loup Rubino; Mihaela Carmen Melinte-Dobrinescu; Frédéric Quillévéré; Jean-Pierre Brun; Nikola Dumurdžanov; Ivan Zagorchev; Vesna Lesić; Dragana Tomić; Dimitrios Sokoutis; Bertrand Meyer; Rodica Macaleţ; Helena Rifelj;handle: 1874/329916
Since the discovery of calcareous nannofossils, dinoflagellate cysts and planktonic foraminifers in deposits from the Dacic Basin, intensive research has been performed in order to evidence which gateway this microplankton used to connect Paratethys and the Mediterranean prior and after the Messinian Salinity Crisis (MSC). Such a gateway is also to be regarded at the origin of successive influxes of Paratethyan organisms (molluscs, ostracods, dinoflagellates) into the Mediterranean Basin ("Lago Mare" events). Observing that the İ stanbul area, usually proposed for this purpose, was inefficient, we examine the succession of marine well-dated pre-MSC and post-MSC deltaic deposits through the Balkans, from northern Greece to southern Romania, that constitutes a reliable candidate for such a marine corridor, the origin of which was caused by the regional tectonic extension. The reconstructed palaeogeography for high sea level episodes that encompassed the MSC clarifies the context of the so-called North Aegean Lake. This marine gateway probably evolved as a powerful river during the peak of the MSC, contributing to the deposition of clastics in the hydrocarbon Prinos Field. A tectonically controlled subsidence to the north and south of the Skopje region caused the closure of such a gateway. International audience
HAL-Rennes 1; HAL-EN... arrow_drop_down NARCIS; Utrecht University RepositoryArticle . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2015add 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.marpetgeo.2015.01.003&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 28 citations 28 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert HAL-Rennes 1; HAL-EN... arrow_drop_down NARCIS; Utrecht University RepositoryArticle . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2015add 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.marpetgeo.2015.01.003&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2009 FrancePublisher:Springer Science and Business Media LLC Funded by:FCT | LA 1FCT| LA 1Mary Kovacheva; Annick Chauvin; Neli Jordanova; Philippe Lanos; Vassil Karloukovski;doi: 10.1186/bf03353179
The effect of magnetic anisotropy on the palaeointensity results has been evaluated in different materials. including samples from archaeological Structures of various ages, Such as baked clay from prehistoric domestic ovens or pottery kilns, burnt soil from ancient fires, and bricks and bricks or tiles used in the kiln's construction. The remanence anisotropy was estimated by the thermoremanent (TRM) anisotropy tensor and isothermal remanence (IRM) tensor methods. The small anisotropy effect (less than 5%) observed in the palaeointensity results of baked clay from the relatively thin prehistoric oven's floors estimated previously through IRM anisotropy was confirmed by TRM anisotropy of this material. The new results demonstrate the possibility of using IRM anisotropy evaluation to correct baked clay palaeointensity data instead of the more difficult to determine TRM anisotropy ellipsoid. This is not always the case for the palaeointensity results from bricks and tiles. The anisotropy correction to palaeointensity results seems negligible for materials other than pottery. It would therefore appear that the palaeointensity determination is more sensitive to the degree of remanence anisotropy P and the angle between the natural remanent magnetization (NRM) vector and the laboratory field direction, than to the angle between the NRM and the maximum axis of the remanence anisotropy ellipsoid (K-max). International audience
Earth, Planets and S... arrow_drop_down HAL-Rennes 1; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2009License: CC BY NC NDHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hyper Article en LigneOther literature type . Article . 2009add 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=10.1186/bf03353179&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 42 citations 42 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert Earth, Planets and S... arrow_drop_down HAL-Rennes 1; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2009License: CC BY NC NDHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hyper Article en LigneOther literature type . Article . 2009add 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=10.1186/bf03353179&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu
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description Publicationkeyboard_double_arrow_right Article 2015 Netherlands, France, Netherlands, NetherlandsPublisher:Elsevier BV Jean-Pierre Suc; Speranta Maria Popescu; Damien Do Couto; Georges Clauzon; Jean Loup Rubino; Mihaela Carmen Melinte-Dobrinescu; Frédéric Quillévéré; Jean-Pierre Brun; Nikola Dumurdžanov; Ivan Zagorchev; Vesna Lesić; Dragana Tomić; Dimitrios Sokoutis; Bertrand Meyer; Rodica Macaleţ; Helena Rifelj;handle: 1874/329916
Since the discovery of calcareous nannofossils, dinoflagellate cysts and planktonic foraminifers in deposits from the Dacic Basin, intensive research has been performed in order to evidence which gateway this microplankton used to connect Paratethys and the Mediterranean prior and after the Messinian Salinity Crisis (MSC). Such a gateway is also to be regarded at the origin of successive influxes of Paratethyan organisms (molluscs, ostracods, dinoflagellates) into the Mediterranean Basin ("Lago Mare" events). Observing that the İ stanbul area, usually proposed for this purpose, was inefficient, we examine the succession of marine well-dated pre-MSC and post-MSC deltaic deposits through the Balkans, from northern Greece to southern Romania, that constitutes a reliable candidate for such a marine corridor, the origin of which was caused by the regional tectonic extension. The reconstructed palaeogeography for high sea level episodes that encompassed the MSC clarifies the context of the so-called North Aegean Lake. This marine gateway probably evolved as a powerful river during the peak of the MSC, contributing to the deposition of clastics in the hydrocarbon Prinos Field. A tectonically controlled subsidence to the north and south of the Skopje region caused the closure of such a gateway. International audience
HAL-Rennes 1; HAL-EN... arrow_drop_down NARCIS; Utrecht University RepositoryArticle . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2015add 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.marpetgeo.2015.01.003&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 28 citations 28 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert HAL-Rennes 1; HAL-EN... arrow_drop_down NARCIS; Utrecht University RepositoryArticle . 2015HAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hal-DiderotArticle . 2015add 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.marpetgeo.2015.01.003&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2009 FrancePublisher:Springer Science and Business Media LLC Funded by:FCT | LA 1FCT| LA 1Mary Kovacheva; Annick Chauvin; Neli Jordanova; Philippe Lanos; Vassil Karloukovski;doi: 10.1186/bf03353179
The effect of magnetic anisotropy on the palaeointensity results has been evaluated in different materials. including samples from archaeological Structures of various ages, Such as baked clay from prehistoric domestic ovens or pottery kilns, burnt soil from ancient fires, and bricks and bricks or tiles used in the kiln's construction. The remanence anisotropy was estimated by the thermoremanent (TRM) anisotropy tensor and isothermal remanence (IRM) tensor methods. The small anisotropy effect (less than 5%) observed in the palaeointensity results of baked clay from the relatively thin prehistoric oven's floors estimated previously through IRM anisotropy was confirmed by TRM anisotropy of this material. The new results demonstrate the possibility of using IRM anisotropy evaluation to correct baked clay palaeointensity data instead of the more difficult to determine TRM anisotropy ellipsoid. This is not always the case for the palaeointensity results from bricks and tiles. The anisotropy correction to palaeointensity results seems negligible for materials other than pottery. It would therefore appear that the palaeointensity determination is more sensitive to the degree of remanence anisotropy P and the angle between the natural remanent magnetization (NRM) vector and the laboratory field direction, than to the angle between the NRM and the maximum axis of the remanence anisotropy ellipsoid (K-max). International audience
Earth, Planets and S... arrow_drop_down HAL-Rennes 1; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2009License: CC BY NC NDHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hyper Article en LigneOther literature type . Article . 2009add 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=10.1186/bf03353179&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 42 citations 42 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!more_vert Earth, Planets and S... arrow_drop_down HAL-Rennes 1; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2009License: CC BY NC NDHAL - UPEC / UPEM; HAL-Pasteur; HAL-Inserm; Hyper Article en LigneOther literature type . Article . 2009add 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=10.1186/bf03353179&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu