Drag Folds is a structural geological feature, specifically a type of minor fold in layered rock, that forms due to differential movement along a fault plane and serves as a kinematic indicator of shear sense by displaying asymmetrical geometry oriented in the direction of slip.
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43
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2017–2026
3
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Publications
34
Geometry and Origin of Fault-Related Folds in Extensional Settings
Roy W. Schlische · AAPG Bulletin · 1995 · 286 citations
Hans Ramberg · Geological Magazine · 1963 · 107 citations
Structural Petrology of Planes of Liquid Inclusions
O. F. Tuttle · The Journal of Geology · 1949 · 104 citations · Full text
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Authors
78
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1–5 of 78
Institutions
43
Imperial College London
London, United Kingdom
1 h-index
1 publications
32 citations
Universidade Federal do Pará
Belém, Brazil
1 h-index
5 publications
85 citations
Universitat Autònoma de Barcelona
Cerdanyola del Vallès, Spain
1 h-index
3 publications
99 citations
Geological Survey Department
Nicosia, Cyprus
1 h-index
1 publications
15 citations
Geological Survey of Canada
Ottawa, Canada
1 h-index
5 publications
110 citations
Universidade Federal de Ouro Preto
Ouro Preto, Brazil
1 h-index
1 publications
23 citations
Sorbonne Université
Paris, France
1 h-index
2 publications
30 citations
University of Milano-Bicocca
Milan, Italy
1 h-index
1 publications
19 citations
1–8 of 43
Venues
- Canadian Journal of Earth Sciences
5 publications · 128 citations
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- AAPG Bulletin
4 publications · 450 citations
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- Journal of Structural Geology
3 publications · 85 citations
3
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- Island Arc
2 publications · 43 citations
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- Geological Magazine
2 publications · 122 citations
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