Listric Fault Geometry
Listric Fault Geometry is a structural geological model characterized by a concave-upward, curvilinear fault surface that dips steeply at shallow depths and shallows with increasing depth, distinguishing it from planar or other non-curved fault geometries in extensional tectonic settings.
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Displacement Geometry in the Volume Containing a Single Normal Fault
J Barnett · AAPG Bulletin · 1987 · 398 citations
Robert B. Smith, Ronald L. Bruhn · Journal of Geophysical Research Atmospheres · 1984 · 393 citations
David Elliott · Journal of Geophysical Research Atmospheres · 1976 · 361 citations
Geometry and Origin of Fault-Related Folds in Extensional Settings
Roy W. Schlische · AAPG Bulletin · 1995 · 286 citations
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Centre National de la Recherche Scientifique
Paris, France
10 h-index
25 publications
590 citations

Royal Holloway University of London
Egham, United Kingdom
8 h-index
15 publications
949 citations
United States Geological Survey
Reston, United States
4 h-index
9 publications
417 citations

British Geological Survey
Nottingham, United Kingdom
4 h-index
6 publications
175 citations

Geoscience Australia
Canberra, Australia
4 h-index
7 publications
535 citations
University of Colorado Boulder
Boulder, United States
4 h-index
4 publications
508 citations
University of Bergen
Bergen, Norway
4 h-index
5 publications
335 citations
The University of Texas at Austin
Austin, United States
3 h-index
4 publications
102 citations
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23 publications · 1.3K citations
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24 publications · 2.2K citations
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JGR · 18 publications · 1.7K citations
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11 publications · 576 citations
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11 publications · 499 citations
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