Structural and petrophysical evolution of extensional fault zones in low-porosity, poorly lithified sandstones of the Barreiras Formation, NE Brazil

Journal of Structural Geology

Volumn 32, Issue 11, 2010, Pages 1806-1826

  Balsamo, F ^a   Storti, F ^a   Salvini, F ^a   Silva, A T ^b   Lima, C C ^b  

^a ROMA TRE UNIVERSITY   (Italy)

^b CENPES   (Brazil)

Author keywords

Cataclasis; Dilatancy; Fault zone permeability; Fractal distribution; Grain size reduction; Porosity

Indexed keywords

CATACLASIS; DILATANCY; FAULT-ZONE PERMEABILITY; FRACTAL DISTRIBUTION; GRAIN-SIZE REDUCTION;

DEFORMATION; FRACTALS; FRACTURE; GRAIN SIZE AND SHAPE; QUARTZ; SANDSTONE; SIZE DETERMINATION; STRUCTURAL GEOLOGY; TEXTURES;

POROSITY;

DILATANCY; EXTENSIONAL TECTONICS; FAULT DISPLACEMENT; FAULT ZONE; FRACTAL ANALYSIS; FRACTURE; GRAIN SIZE; POROSITY; ROCK MICROSTRUCTURE; SANDSTONE; STRUCTURAL GEOLOGY; TECTONIC EVOLUTION;

BRAZIL;

EID: 78649797665     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2009.10.010     Document Type: Article

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