Rift Reactivation
Rift Reactivation is a tectonic process in which pre-existing rift zones within continental plates, characterized by ancient extensional fault systems and lithospheric weaknesses, experience renewed extensional, transtensional, or inversion deformation due to subsequent far-field stresses, distinguishable from primary rifting by the preferential localization of strain along earlier-formed structural discontinuities.
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2017–2026
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Upper Rhine Graben: Role of preexisting structures during rift evolution
M. E. Schumacher · Tectonics · 2002 · 312 citations
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Centre National de la Recherche Scientifique
Paris, France
8 h-index
18 publications
1.5K citations
The University of Texas at Austin
Austin, United States
7 h-index
10 publications
733 citations

University of Leeds
Leeds, United Kingdom
7 h-index
8 publications
612 citations

Imperial College London
London, United Kingdom
6 h-index
14 publications
1.4K citations

University of Oslo
Oslo, Norway
6 h-index
8 publications
425 citations
University of Bergen
Bergen, Norway
6 h-index
15 publications
1.3K citations
Université de Strasbourg
Strasbourg, France
6 h-index
15 publications
1.4K citations
Northwest University
Xi'an, China
4 h-index
10 publications
315 citations
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19 publications · 2.4K citations
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JGS · 6 publications · 361 citations
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6 publications · 247 citations
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