Evidence of Hydrocarbon-Rich Fluid Interaction with Clays: Clay Mineralogy and Boron Isotope Data from Gulf of Cádiz Mud Volcano Sediments

Clay dehydration at great depth generates fluids and overpressures in organic-rich sediments that can release isotopically light boron from mature organic matter, producing <sup>10</sup>B-rich fluids. The B can be incorporated into the tetrahedral sites of authigenic illite during the il...

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Bibliographic Details
Main Authors: Rubén Martos-Villa, M. Pilar Mata, Lynda B. Williams, Fernando Nieto, Xabier Arroyo Rey, C. Ignacio Sainz-Díaz
Format: Article
Language:English
Published: MDPI AG 2020-07-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/8/651