Observations on normal-fault scarp morphology and fault system evolution of the Bishop Tuff in the Volcanic Tableland, Owens Valley, California, U.S.A.
Authors:
- David A. FerrillDFDavid A. Ferrill
- Alan P. MorrisAMAlan P. Morris
- Ronald N. McGinnisRMRonald N. McGinnis
- Kevin J. SmartKSKevin J. Smart
- Morgan J Watson-MorrisMWMorgan J Watson-Morris
- Sarah S. WiggintonSWSarah S. Wigginton
- 28 March 2016
- journal article
- Published by GeoScienceWorld in Lithosphere
- Vol. 8 (3) , 238-253
Abstract
No abstract availableThis publication has 86 references indexed in Scilit:
- A geometric model of fault zone and fault rock thickness variationsJournal of Structural Geology, 2009
- Characterization of strike-slip fault–splay relationships in sandstoneJournal of Structural Geology, 2007
- Damage zone and slip-surface evolution over μm to km scales in high-porosity Navajo sandstone, UtahJournal of Structural Geology, 2001
- Displacement gradient and deformation in normal fault systemsJournal of Structural Geology, 2001
- Influence of rift obliquity on fault-population systematics: results of experimental clay modelsJournal of Structural Geology, 2000
- Normal fault corrugation: implications for growth and seismicity of active normal faultsJournal of Structural Geology, 1999
- Constant-thickness deformation above curved normal faultsJournal of Structural Geology, 1999
- Three-dimensional analyses of slip distributions on normal fault arrays with consequences for fault scalingJournal of Structural Geology, 1996
- Displacement-length scaling and fault linkageJournal of Structural Geology, 1995
- Thickness-displacement relationships for fault zonesJournal of Structural Geology, 1990