Conditions for hydrofracture and the fluid permeability of accretionary wedges
- 1 December 1991
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 107 (3-4) , 550-558
- https://doi.org/10.1016/0012-821x(91)90100-v
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Hydrogeochemistry in the barbados accretionary complex: Leg 110 ODPPalaeogeography, Palaeoclimatology, Palaeoecology, 1989
- Evolution of structures and fabrics in the Barbados Accretionary Prism. Insights from leg 110 of the Ocean Drilling ProgramJournal of Structural Geology, 1988
- Expulsion of fluids from depth along a subduction-zone decollement horizonNature, 1987
- Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocksGSA Bulletin, 1986
- Porosity of sediments in accretionary prisms and some implications for dewatering processesJournal of Geophysical Research, 1985
- Mechanics of fold‐and‐thrust belts and accretionary wedgesJournal of Geophysical Research, 1983
- Controls on low-stress hydro-fracture dilatancy in thrust, wrench and normal fault terrainsNature, 1981
- The role of pore pressure in deformation in geologic processesGeology, 1980
- Mechanics of thin-skinned fold-and-thrust beltsGSA Bulletin, 1978
- Fault rocks and fault mechanismsJournal of the Geological Society, 1977