Fault-block Mountains
Fault-Block Mountains is a type of mountain landform characterized by large-scale uplifted or down-dropped crustal blocks bounded by normal or reverse faults, resulting from tectonic extension or compression that fractures and displaces rigid segments of the Earth's lithosphere.
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174
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2017–2026
5
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Fault-block Mountain
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Tectonic framework and evolution of the Tarim Block in NW China
Chuan‐Lin Zhang, Haibo Zou, Huaikun Li et al. · Gondwana Research · 2012 · 391 citations
She Fa Chen, Christopher J.L. Wilson, Qi Dong Deng et al. · Journal of Geophysical Research Atmospheres · 1994 · 197 citations
Origin of Mountains on Io by Thrust Faulting and Large-Scale Mass Movements
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University of Bergen
Bergen, Norway
3 h-index
5 publications
130 citations
Stanford University
Stanford, United States
3 h-index
6 publications
530 citations

Chinese Academy of Geological Sciences
Beijing, China
2 h-index
6 publications
185 citations
Equinor (Norway)
Stavanger, Norway
2 h-index
4 publications
51 citations

Eastern Connecticut State University
Willimantic, United States
2 h-index
2 publications
65 citations
Ruhr University Bochum
Bochum, Germany
1 h-index
1 publications
15 citations
ETH Zurich
Zurich, Switzerland
1 h-index
4 publications
428 citations
University of Delaware
Newark, United States
1 h-index
1 publications
25 citations
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JG · 7 publications · 146 citations
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3 publications · 107 citations
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3 publications · 48 citations
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3 publications · 59 citations
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3 publications · 65 citations
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