Riedel Shears is a structural geological phenomenon categorized as a type of shear fracture system, distinguished by the development of en echelon synthetic and antithetic secondary faults that form in response to localized brittle deformation along strike-slip fault zones.
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2017–2026
17
Variants
Riedel Shear Structures
Parents
Publications
69
Experimental models of strike-slip tectonics
P. Richard, Michael A. Naylor, Anton Koopman · Petroleum Geoscience · 1995 · 168 citations
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Authors
198
- AL
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h-index
- NCNicolas Chamot‐Rooke
Laboratoire de Géologie de l’École Normale Supérieure, France
2 publications · 48 citations
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- JM
2
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- MK
2
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- RC
2
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1–5 of 198
Institutions
94
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
3 h-index
7 publications
255 citations
ETH Zurich
Zurich, Switzerland
3 h-index
10 publications
362 citations
Chengdu University of Technology
Chengdu, China
2 h-index
7 publications
179 citations
Rice University
Houston, United States
2 h-index
4 publications
100 citations
GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
2 h-index
2 publications
50 citations
University of Southampton
Southampton, United Kingdom
2 h-index
8 publications
192 citations
China Earthquake Administration
Beijing, China
2 h-index
7 publications
155 citations
National Central University
Taoyuan City, Taiwan
2 h-index
5 publications
110 citations
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Venues
- Journal of Geophysical Research Atmospheres
JGR · 7 publications · 701 citations
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- Geological Society London Special Publications
6 publications · 150 citations
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- Journal of the Geological Society
JGS · 5 publications · 248 citations
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- Journal of Structural Geology
5 publications · 368 citations
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- Tectonophysics
5 publications · 206 citations
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