Normal-fault development during two phases of non-coaxial extension: An experimental study
- 30 November 2010
- journal article
- Published by Elsevier BV in Journal of Structural Geology
- Vol. 32 (11), 1656-1667
- https://doi.org/10.1016/j.jsg.2009.07.007
Abstract
No abstract availableThis publication has 29 references indexed in Scilit:
- Fault superimposition and linkage resulting from stress changes during rifting: Examples from 3D seismic data, Phitsanulok Basin, ThailandJournal of Structural Geology, 2007
- Evaluating sand and clay models: do rheological differences matter?Journal of Structural Geology, 2005
- Activation of rift oblique and rift parallel pre-existing fabrics during extension and their effect on deformation style: examples from the rifts of ThailandJournal of Structural Geology, 2004
- Influence of viscous layers on the growth of normal faults: insights from experimental and numerical modelsJournal of Structural Geology, 2003
- Influence of rift obliquity on fault-population systematics: results of experimental clay modelsJournal of Structural Geology, 2000
- Joints at high angles to normal fault strike: an explanation using 3-D numerical models of fault-perturbed stress fieldsJournal of Structural Geology, 2000
- Characterization of stress perturbations near major fault zones: insights from 2-D distinct-element numerical modelling and field studies (Jura mountains)Journal of Structural Geology, 1997
- Release fault: A variety of cross fault in linked extensional fault systems, in the Sergipe-Alagoas Basin, NE BrazilJournal of Structural Geology, 1995
- RHEOLOGICAL AND TECTONIC MODELING OF SALT PROVINCESTectonophysics, 1993
- Deformation produced by oblique riftingTectonophysics, 1986