Parallel Folding
Parallel Folding is a kinematic model of deformation in structural geology where layered rock units fold such that the thickness perpendicular to the bedding remains constant, distinguishing it from other folding mechanisms by preserving layer-parallel shortening without internal strain variation across the fold limbs.
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2.2K
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137
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73
Institutions
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2017–2026
5
Variants
Concentric Folding
Parents
47
The Geometry and Mechanics of Formation of "Similar" Type Folds
John G. Ramsay · The Journal of Geology · 1962 · 251 citations
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University of Bath
Bath, United Kingdom
4 h-index
11 publications
212 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
3 publications
151 citations
Harvard University
Cambridge, United States
3 h-index
6 publications
679 citations

Imperial College London
London, United Kingdom
2 h-index
2 publications
30 citations
University of Wisconsin–Madison
Madison, United States
2 h-index
3 publications
76 citations

Indian Institute of Technology Roorkee
Roorkee, India
2 h-index
4 publications
72 citations
Stanford University
Stanford, United States
2 h-index
3 publications
202 citations

Université de Montpellier
Montpellier, France
2 h-index
2 publications
131 citations
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8 publications · 329 citations
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JMB · 4 publications · 189 citations
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3 publications · 179 citations
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3 publications · 118 citations
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2 publications · 47 citations
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