Grain size and permeability evolution of soft-sediment extensional sub-seismic and seismic fault zones in high-porosity sediments from the Crotone basin, southern Apennines, Italy

Marine and Petroleum Geology

Volumn 27, Issue 4, 2010, Pages 822-837

  Balsamo, F ^a   Storti, F ^a  

^a ROMA TRE UNIVERSITY   (Italy)

Author keywords

Deformation band; Faulting; Grain size reduction; Permeability

Indexed keywords

APENNINES; CATACLASTIC DEFORMATION; DAMAGE ZONES; DEFORMATION BAND; DEGREES OF COMPLEXITY; DISPLACEMENT VALUE; EXTENSIONAL FAULTS; FAULT CORE; FAULT DAMAGE ZONE; FAULT DISPLACEMENT; FAULT ZONE; GRAIN SIZE; GRAIN-SIZE REDUCTION; PERMEABILITY EVOLUTION; PERMEABILITY REDUCTION; ROCK PERMEABILITY; SEISMIC FAULTS; SLIP SURFACES;

DEFORMATION; GRAIN SIZE AND SHAPE; GRINDING (COMMINUTION); LENSES; OPTICAL INSTRUMENTS; SEDIMENTOLOGY; SEISMOLOGY; SIZE DETERMINATION;

CAPILLARITY;

COMMINUTION; DEFORMATION MECHANISM; DISPLACEMENT; EXTENSIONAL TECTONICS; FAULT ZONE; FAULTING; FOLIATION; FOOTWALL; GRAIN SIZE; MICROSTRUCTURE; PERMEABILITY; POROSITY; SEDIMENT; SEISMIC ZONE; STRIATION;

CALABRIA; CROTONE BASIN; ITALY;

EID: 77950518208     PISSN: 02648172     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marpetgeo.2009.10.016     Document Type: Article

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