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 -
May 1, 2018 (v1)Book section
no abstract
Uploaded on: December 4, 2022 -
September 2015 (v1)Journal article
The current interpretation of the Messinian Salinity Crisis (MSC) involves the deposition of peripheral or marginal evaporites in onshore basins as well as the erosion of the margin and the deposition of thick evaporites in deep basins. The so-called intermediate basins are formed in domains between the onland outcrops and the deep basins. The...
Uploaded on: February 28, 2023 -
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 -
May 1, 2018 (v1)Book section
no abstract
Uploaded on: December 4, 2022 -
May 1, 2018 (v1)Book section
no abstract
Uploaded on: December 4, 2022 -
October 2021 (v1)Conference paper
International audience
Uploaded on: February 22, 2023 -
October 2021 (v1)Conference paper
International audience
Uploaded on: February 22, 2023