The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region, U.S.A.
Top Cited Papers
- 3 April 2003
- journal article
- research article
- Published by Elsevier
- Vol. 11 (1-2) , 65-94
- https://doi.org/10.1016/0191-8141(89)90036-9
Abstract
No abstract availableThis publication has 34 references indexed in Scilit:
- Crystal growth in cataclasites: Diagnostic microstructures and implicationsPublished by Elsevier ,2003
- Modes of extensional tectonicsPublished by Elsevier ,2003
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- Shear zone origin of quartzite mylonite and mylonitic pegmatite in the Coyote Mountains metamorphic core complex, ArizonaJournal of Structural Geology, 1987
- Role of tectonic denudation in warping and uplift of low-angle normal faultsGeology, 1984
- Continental fault structure and the shallow earthquake sourceJournal of the Geological Society, 1983
- Normal faulting, block tilting, and décollement in a stretched crustTectonics, 1983
- The Snake Range Décollement: An exhumed Mid‐Tertiary ductile‐brittle transitionTectonics, 1983
- Limits of stresses in continental crusts and their relation to the depth‐frequency distribution of shallow earthquakesTectonics, 1982
- An assessment of dynamically recrystallized grainsize as a palaeopiezometer in quartz-bearing mylonite zonesTectonophysics, 1981