Passive Margin Magmatism is a geological phenomenon characterized by volcanic and igneous activity occurring during and after the rifting phase of continental breakup at passive margins, distinguished from other tectonic magmatic settings by its association with decompression melting of the mantle beneath extensionally thinned lithosphere in the absence of active plate convergence.
90
Publications
6.7K
Citations
341
Authors
181
Institutions
Publications per year
2017–2026
28
Parents
Publications
90
1–5 of 90
Authors
341
- LG
5
h-index
- JP
3
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- KM
2
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- NH
2
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- HW
2
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1–5 of 341
Institutions
181
Centre National de la Recherche Scientifique
Paris, France
11 h-index
23 publications
1.1K citations
Sorbonne Université
Paris, France
5 h-index
9 publications
441 citations
ETH Zurich
Zurich, Switzerland
5 h-index
12 publications
982 citations
Rice University
Houston, United States
4 h-index
6 publications
586 citations
Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
9 publications
1.2K citations
Université de Bretagne Occidentale
Brest, France
4 h-index
6 publications
406 citations
Total (France)
Paris, France
4 h-index
7 publications
501 citations
Institut des Sciences de la Terre de Paris
Paris, France
4 h-index
9 publications
313 citations
1–8 of 181
Venues
- Terra Nova
7 publications · 170 citations
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- Geology
6 publications · 1.2K citations
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- Geological Society London Special Publications
5 publications · 268 citations
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- Tectonophysics
5 publications · 603 citations
5
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- Geological Society of America Bulletin
4 publications · 477 citations
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1–5