Based on new ('SESAME 01' cruise) and previous seismic reflection data, this paper evidences the effects of the Messinian Salinity Crisis on the sedimentation at the western Sardinian margin. In the lower part of the margin, Messinian detrital deposits are organized into two successive, 300 m thick units. According to their shape, facies and...
-
2005 (v1)Journal articleUploaded on: March 25, 2023
-
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 -
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 -
February 1, 2011 (v1)Book
International audience
Uploaded on: December 3, 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 -
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