Migration of Mn-rich fluids through normal faults and fine-grained terrigenous sediments during early development of the Neogene Vallès-Penedès half-graben (NE Spain)

Author:

TRAVÉ A.,ROCA E.,PLAYÀ E.,PARCERISA D.,GÓMEZ-GRAS D.,MARTÍN-MARTÍN J. D.

Publisher

Wiley

Subject

General Earth and Planetary Sciences

Reference82 articles.

1. Sinopsis estratigráfica del Neógeno de la fosa del Vallès-Penedès;Agustí;Paleontologia i Evolució,1985

2. Effect of faulting on fluid flow in porous sandstone: petrophysical properties;Antonellini;American Association of Petroleum Geologists Bulletin,1994

3. Effect of faulting on fluid flow in porous sandstone: geometry and spatial distribution;Antonellini;American Association of Petroleum Geologists Bulletin,1995

4. The structural evolution of the northern Viking Graben and its bearing upon extensional modes of basin formation;Badley;Journal of Geological Society of London Bulletin,1988

5. Redox conditions of calcite cementation interpreted from Mn and Fe contents of authigenic calcites;Barnaby;Geological Society of America Bulletin,1989

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