How does the water–rock interaction of marly rocks affect its mechanical properties in the Three Gorges reservoir area, China?

Environmental Earth Sciences

Volumn 72, Issue 8, 2014, Pages 2797-2810

  Chai, Bo ^a   Tong, Jun ^b   Jiang, Bo ^a   Yin, Kunlong ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

^b Hunan Institute of Geological Survey   (China)

Author keywords

Landslide; Marly rock; Mechanical properties; Water rock interaction

Indexed keywords

CALCITE; COMPRESSIVE STRENGTH; CREEP; DISSOLUTION; FELDSPAR; ION EXCHANGE; LANDSLIDES; MECHANICAL PROPERTIES; MICROSTRUCTURE; SLOPE PROTECTION;

CREEP DEFORMATIONS; LABORATORY TEST; LINEAR REGRESSION EQUATION; MINERAL COMPOSITION; ROCK INTERACTION; SHALLOW SLOPE FAILURE; THREE GORGES RESERVOIR AREA; UNIAXIAL COMPRESSIVE STRENGTH;

ROCKS;

BOREHOLE; CLAY MINERAL; DEFORMATION; DISSOLUTION; LANDSLIDE; MECHANICAL PROPERTY; MICROSTRUCTURE; POISSON RATIO; SEEPAGE; WATER-ROCK INTERACTION;

CHINA; THREE GORGES RESERVOIR;

EID: 84907689977     PISSN: 18666280     EISSN: 18666299     Source Type: Journal    
DOI: 10.1007/s12665-014-3204-y     Document Type: Article

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