Darrell W. Sims
Southwest Research Institute
21 Papers
83 Citations
Darrell W. Sims is an academic researcher from Southwest Research Institute. The author has contributed to research in topics: Fault (geology) & Groundwater recharge. The author has an hindex of 11, co-authored 21 publications.
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Papers
Distribution, morphology, and origins of Martian pit crater chains
TL;DR: In this paper, the authors performed a detailed quantitative analysis of pit crater morphology using MOC narrow angle images, Thermal Emission Imaging System (THEMIS) visual images, and Mars Orbiter Laser Altimeter (MOLA) data.
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Role of a ductile decollement in the development of pull-apart basins : experimental results and natural examples
TL;DR: In this article, the authors show that pull-apart basins are dramatically different when overburden rides over a ductile horizon, and that thickness of the ductiles horizon exerts control on basin development.
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Structural framework of the Edwards Aquifer recharge zone in south-central Texas
David A. Ferrill,Darrell W. Sims,Deborah J. Waiting,Alan P. Morris,Nathan M. Franklin,Alvin L. Schultz +5 more
TL;DR: In this paper, the authors investigate the geologic structure of the Edwards Aquifer to assess the large-scale aquifer architecture, analyze fault offset and stratigraphic juxtaposition relationships, evaluate fault-zone deformation and dissolution and fault-system architecture, and investigate fault-block deformation.
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Crossing conjugate normal faults
TL;DR: In this paper, the authors use two-dimensional geometric modeling to show that simultaneous slip on crossing conjugate normal faults requires loss, gain, or localized redistribution of cross-sectional area, while alternating sequential slip on the crossing faults can produce crossing fault patterns without area modification in cross section.
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Development of Synthetic Layer Dip Adjacent to Normal Faults
David A. Ferrill,Alan P. Morris,Darrell W. Sims,Deborah J. Waiting,Shutaro Hasegawa +4 more
- 01 Jan 2005
TL;DR: In this article, the authors demonstrate that synthetic dip panels adjacent to normal faults should be expected at some scale in all normal fault systems, and five fault-related mechanisms for the development of synthetic dip are antilistric fault bend, distributed shear, shear in relay zone of vertically and/or laterally segmented faults, and fault block impingement and lateral contraction.
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