Diagenesis and fluid-fracture evolution in an intracontinental basin: The Penedès half-graben,western Mediterranean / Diagènesi i evolució de la relació fluid-fractura en una conca intracontinental: la conca del Penedès, oest de la Mediterrània

The Penedes half-graben represents a natural field laboratory for the study of the link between tectonics and palaeofluids because it exposes numerous outcrops that allow a global and complete diagenetic study of the basin from Mesozoic to present times. The Penedes half-graben is located in the ce...

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Bibliographic Details
Main Author: Baqués Almirall, Vinyet
Other Authors: Travé i Herrero, Anna
Format: Doctoral Thesis
Language:English
Published: Universitat de Barcelona 2012
Subjects:
55
Online Access:http://hdl.handle.net/10803/112701