Inferred fluid flow through fault damage zones based on the observation of stalactites in carbonate caves
- 13 May 2009
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 32 (9), 1305-1316
- https://doi.org/10.1016/j.jsg.2009.04.017
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Fault zone architecture and permeability features in siliceous sedimentary rocks: Insights from the Rapolano geothermal area (Northern Apennines, Italy)Journal of Structural Geology, 2008
- Permeability scaling properties of fault damage zones in siliclastic rocksJournal of Structural Geology, 2004
- The evolution of faults formed by shearing across joint zones in sandstoneJournal of Structural Geology, 2004
- Fault damage zonesJournal of Structural Geology, 2004
- Initiation of brittle faults in the upper crust: a review of field observationsJournal of Structural Geology, 2003
- The damage zone-fault core transition in carbonate rocks: implications for fault growth, structure and permeabilityJournal of Structural Geology, 2003
- A conceptual model for the origin of fault damage zone structures in high-porosity sandstoneJournal of Structural Geology, 2002
- Damage zone and slip-surface evolution over μm to km scales in high-porosity Navajo sandstone, UtahJournal of Structural Geology, 2001
- Damage zone geometry around fault tipsJournal of Structural Geology, 1995
- Earthquake faulting as a structural processJournal of Structural Geology, 1989