Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6441629 | Marine Geology | 2014 | 17 Pages |
Abstract
Our results suggest the presence offshore of at least two generations of diachronous MSC deposits. The observation of salt on a continental high and the widespread MSC deposits on the margins of the Central Mallorca Depression call into question the location of halite preferentially in the deep abyssal basins and the significance of the deep basin MSC units that onlap onto the Margin Erosional Surface (MES), as observed all around the passive margins of the Northwest-Mediterranean Basin. The dual terminology used for peripheral/deep MSC evaporites cannot be applied to any of the MSC units found in the study area.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Agnès Maillard, Olivier Driussi, Johanna Lofi, Anne Briais, Franck Chanier, Christian Hübscher, Virginie Gaullier,