Splay Faulting
Splay Faulting is a structural geologic process characterized by the formation of secondary thrust faults branching from a main subduction megathrust, which accommodate differential strain partitioning along the plate boundary.
92
Publications
4.7K
Citations
354
Authors
195
Institutions
Publications per year
2017–2026
30
Parents
92
Splay Fault Branching Along the Nankai Subduction Zone
Jin‐Oh Park, Shuichi Kodaira, Phil R. Cummins et al. · Science · 2002 · 607 citations
Origin and evolution of a splay fault in the Nankai accretionary wedge
Michael Strasser, Gregory F. Moore, Gaku Kimura et al. · Nature Geoscience · 2009 · 213 citations
1–5 of 92
354
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Japan Agency for Marine-Earth Science and Technology, Japan
3 publications · 823 citations
3
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3
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1–5 of 354
195
United States Geological Survey
Reston, United States
12 h-index
21 publications
656 citations
California Institute of Technology
Pasadena, United States
7 h-index
13 publications
898 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
13 publications
667 citations
GNS Science
Lower Hutt, New Zealand
6 h-index
15 publications
320 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
6 h-index
17 publications
4.5K citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
5 h-index
8 publications
475 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
4 h-index
7 publications
422 citations
Boise State University
Boise, United States
4 h-index
8 publications
209 citations
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9 publications · 579 citations
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6 publications · 309 citations
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5 publications · 310 citations
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4 publications · 186 citations
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NZJG · 4 publications · 71 citations
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