no abstract
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May 1, 2018 (v1)Book sectionUploaded on: December 4, 2022
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May 1, 2018 (v1)Book section
no abstract
Uploaded on: December 4, 2022 -
November 14, 2011 (v1)Conference paper
Le projet METYSS (Messinian Event in the Tyrrhenian from Seismic Study) concerne le bassin tyrrhénien occidental le long de la côte est-sarde et s'intègre dans le cadre d'une étude comparative des marqueurs sismiques de la Crise de Salinité Messinienne (CSM) à l'échelle du bassin méditerranéen. La mer tyrrhénienne est un bassin arrière-arc...
Uploaded on: December 3, 2022 -
May 1, 2018 (v1)Book section
no abstract
Uploaded on: December 4, 2022 -
April 1, 2018 (v1)Journal article
In the last fifty years, the Messinian Salinity Crisis (MSC) has been widely investigated in the Mediterranean Sea, but a major basin remains fewly explored in terms of MSC thematic: the Western Tyrrhenian Basin. The rifting of this back-arc basin is considered to occur between the Middle-Miocene and the Early-Pliocene, thus including the MSC,...
Uploaded on: December 4, 2022 -
November 14, 2011 (v1)Conference paper
The Tyrrhenian Sea is usually interpreted to be a Neogene back-arc basin that opened by continental rifting and oceanic spreading caused by the eastward migration of the Apennine subduction system from Tortonian to Pliocene times. Rifting of the Tyrrhenian Sea started first along the Eastern Sardinian margin during the Tortonian-Messinian...
Uploaded on: December 3, 2022 -
March 5, 2014 (v1)Journal article
The Tyrrhenian Sea is usually interpreted to be a Neogene back-arc basin that opened by continental rifting and oceanic spreading caused by the eastward migration of the Apennine subduction system during Miocene and Pliocene times. Rifting of the southern Tyrrhenian Sea started first along the Eastern Sardinian margin during the middle to late...
Uploaded on: December 3, 2022 -
February 1, 2011 (v1)Book
International audience
Uploaded on: December 3, 2022 -
2011 (v1)Journal article
The Messinian salinity crisis (MSC) is characterized by gigantic erosion that remodels the margins while a thick, essentially evaporitic and detrital, sedimentary sequence forms in the deep basins. Based on recent (MAURESC, 2003) and earlier (MESEA 1, 1990; MAGIRAA, 1996; GEOBREST, 2002) seismic reflection data, this work brings to light the...
Uploaded on: December 3, 2022 -
November 7, 2007 (v1)Conference paper
International audience
Uploaded on: December 4, 2022 -
April 23, 2023 (v1)Publication
The Eastern Sardinian margin consists in a hyper-extended rifted margin, located in the western Tyrrhenian Sea, a recent back-arc basin (late Neogene). This area was affected by strong aerial erosion during the Messinian Salinity Crisis (MSC, 5.96 - 5.33 My) associated with the drop of sea level (> 1500 m) which occurred throughout the whole...
Uploaded on: November 25, 2023 -
October 30, 2023 (v1)Conference paper
La marge orientale de la Sardaigne est une marge continentale passive hyper-étirée, située en Mer Tyrrhénienne occidentale, en contexte d'arrière arc récent (fin Néogène - Quaternaire). Cette région a été affectée par une forte érosion aérienne pendant la Crise de Salinité Messinienne (CSM ; 5,96 - 5,33 Ma) associée à une baisse importante du...
Uploaded on: November 25, 2023 -
2021 (v1)Journal articleNew Magnetic compilation and interpretation of the Bay of Biscay and surrounding continental shelves
International audience
Uploaded on: December 3, 2022 -
November 1, 2021 (v1)Conference paper
Le bassin Ligure, à la jonction entre la mer Méditerranée occidentale et la chaîne Alpine, résulte d'une extension arrière-arc liée au retrait de la plaque plongeante Ionienne depuis l'Oligocène jusqu'au Miocène. Cette phase d'extension prenant place dans le contexte de la collision Eurasie-Afrique a créé des structures complexes dans une...
Uploaded on: December 3, 2022 -
December 13, 2021 (v1)Conference paper
The north Ligurian margin is a stretched continental margin located at the junction of the Western Mediterranean Sea and the Alpine belt. The back-arc Ligurian basin opened from late Oligocene to early Miocene, as a result of the Apulian slab rollback. It has then evolved next to the active Alpine orogen, in a regional compressional setting...
Uploaded on: December 3, 2022 -
April 19, 2021 (v1)Conference paper
The north Ligurian margin is a stretched continental margin located at the junction of the Western Mediterranean Sea and the Alpine belt. This region underwent several phases of contrasting deformation styles. The Ligurian basin opened from late Oligocene to early Miocene times, as a result of a back-arc extension induced by the rollback of the...
Uploaded on: December 3, 2022 -
March 1, 2011 (v1)Journal article
The Messinian salinity crisis (MSC) is characterized by gigantic erosion that remodels the margins while a thick, essentially evaporitic and detrital, sedimentary sequence forms in the deep basins. Based on recent (MAURESC, 2003) and earlier (MESEA 1, 1990; MAGIRAA, 1996; GEOBREST, 2002) seismic reflection data, this work brings to light the...
Uploaded on: December 3, 2022 -
April 12, 2023 (v1)Journal article
Phylogenetic studies of present-day terrestrial organisms suggest that faunal dispersals between South America and the Greater Antilles may have occurred during the Cenozoic through the Lesser Antilles. However, because of the lack of geological data to unravel the areas that may have emerged along the Lesser Antilles trench, the migration...
Uploaded on: April 23, 2023 -
April 3, 2011 (v1)Journal article
We focus on the northern Ligurian margin, at the geological junction of the subalpine domain and the Ligurian oceanic basin, in order (1) to identify the location of the southern limit of the Alpine compressive domain during the Cenozoic, and (2) to study the influence of a compressive environment on the tectonic and sedimentary evolution of a...
Uploaded on: December 3, 2022 -
2016 (v1)Journal article
The seaward extension of onshore formations and structures were previously almost unknown in Provence. The interpretation of 2D high-resolution marine seismic profiles together with the integration of sea-bottom rock samples provides new insights into the stratigraphic, structural and paleogeographic framework of pre-Messinian Salinity Crisis...
Uploaded on: February 28, 2023 -
March 21, 2011 (v1)Conference paper
The Bouillante geothermal field, located on the west coast of Guadeloupe (Lesser Antilles), was explored in the 1970s, developed in the 1980s, brought into production in 1986, and expanded in 2005 to currently produce up to 15 MWe. In addition to its electricity-producing role, the Bouillante field is an outstanding research laboratory for...
Uploaded on: December 3, 2022