Fault zone architecture and deformation processes within evaporitic rocks in the upper crust

Author:

De Paola N.,Collettini C.1,Faulkner D. R.2,Trippetta F.1

Affiliation:

1. Gruppo di Geologia Strutturale e Geofisica, Dipartimento di Scienze della Terra; Università di Perugia; Perugia; Italy

2. Rock Deformation Laboratory, Earth and Ocean Sciences Department; Liverpool University; Liverpool; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference92 articles.

1. Architecture and deformation mechanism of a basin-bounding normal fault in Mesozoic platform carbonates, central Italy;Agosta;J. Struct. Geol.,2006

2. Fluid conduits in carbonate-hosted seismogenic normal faults of central Italy;Agosta;J. Geophys. Res.,2003

3. Geol. Soc. Spec. Publ.;Austin,2005

4. Geol. Soc. Spec. Pub.;Austin,2005

5. Balanced sections and seismic reflection profiles across the Central Apennines;Bally;Mem. Soc. Geol. Ital.,1986

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