Changes in bedrock channel morphology driven by displacement rate increase during normal fault interaction and linkage
Author:
Affiliation:
1. Department of Earth and Environmental Sciences; Tulane University; New Orleans LA USA
Funder
American Chemical Society Petroleum Research Fund
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/bre.12072/fullpdf
Reference46 articles.
1. Channel width response to differential uplift;Amos;J. Geophys. Res.,2007
2. Modeling fluvial incision and transient landscape evolution: influence of dynamic channel adjustment;Attal;J. Geophys. Res.,2008
3. Fault growth by segment linkage: an explanation for scatter in maximum displacement and trace length data from the Canyonlands grabens of SE Utah;Cartwright;J. Struct. Geol.,1995
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