A new model for the growth of normal faults developed above pre-existing structures
Author:
Affiliation:
1. Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET), School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
2. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
Abstract
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/geology/article-pdf/49/5/587/5273575/587.pdf
Reference33 articles.
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2. Fault populations, strain distribution and basement fault reactivation in the East Pennines Coalfield, UK;Bailey;Journal of Structural Geology,2005
3. The kinematics of reactivation of normal faults using high resolution throw mapping;Baudon;Journal of Structural Geology,2008
4. Rifting of the plate boundary in north Iceland 1975–1978;Björnsson;Journal of Geophysical Research,1979
5. Evidence for spreading-rate dependence in the displacement-length ratios of abyssal hill faults at mid-ocean ridges;Bohnenstiehl;Geology,2000
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