Chemical changes and fluid-rock interaction in faults of crystalline thrust sheets, northwestern Wyoming, U.S.A.
- 1 April 1995
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 17 (4) , 533-547
- https://doi.org/10.1016/0191-8141(94)00068-b
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- Element mobility associated with meta-shear zones within the Ben Hope amphibolite suite, ScotlandPublished by Elsevier ,2003
- Trace element mobility in the mylonite zone within the ophiolite aureole, St. Anthony Complex, NewfoundlandPublished by Elsevier ,2002
- Internal structure and weakening mechanisms of the San Andreas FaultJournal of Geophysical Research, 1993
- Deformation mechanisms and kinematics of a crystalline-cored thrust sheet: The EA thrust system, WyomingPublished by Geological Society of America ,1993
- Structural and fluid-chemical properties of seismogenic normal faultsTectonophysics, 1990
- Healing of microcracks in quartz: Implications for fluid flowGeology, 1990
- Paleogeographic and paleotectonic setting of Laramide sedimentary basins in the central Rocky Mountain regionGSA Bulletin, 1988
- Deformation mechanisms in granitic rocks at shallow crustal levelsJournal of Structural Geology, 1988
- Implications for mechanical properties of brittle faults from observations of the Punchbowl fault zone, CaliforniaPure and Applied Geophysics, 1986
- The role of pore water circulation during the deformation of foreland fold and thrust beltsJournal of Geophysical Research, 1984