Geometric analysis and scaling relations of deformation bands in porous sandstone
- 1 December 1997
- journal article
- Published by Elsevier BV in Journal of Structural Geology
- Vol. 19 (12), 1479-1493
- https://doi.org/10.1016/s0191-8141(97)00075-8
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- A modern regression approach to determining fault displacement-length scaling relationshipsJournal of Structural Geology, 1996
- Are fault growth and linkage models consistent with power-law distributions of fault lengths?Journal of Structural Geology, 1996
- Fault growth by segment linkage: an explanation for scatter in maximum displacement and trace length data from the Canyonlands Grabens of SE UtahJournal of Structural Geology, 1995
- Fractal nature and scaling of normal faults in the Española Basin, Rio Grande rift, New Mexico: implications for fault growth and brittle strainJournal of Structural Geology, 1995
- Fault overlap zones within developing normal fault systemsJournal of the Geological Society, 1995
- Microstructure of deformation bands in porous sandstones at Arches National Park, UtahJournal of Structural Geology, 1994
- Analysis of faulting in porous sandstonesJournal of Structural Geology, 1983
- Number and orientation of fault sets in the field and in experimentsGeology, 1982
- Development of faults as zones of deformation bands and as slip surfaces in sandstonePure and Applied Geophysics, 1978
- Small faults formed as deformation bands in sandstonePure and Applied Geophysics, 1978