Quaternary Basin Development is a geodynamic process denoting the formation and evolution of sedimentary basins during the Quaternary period, distinguished by its response to neotectonic activity, climatic influences, and eustatic sea-level changes.
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21.7K
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1.3K
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506
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2017–2026
39
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Publications
384
1–5 of 384
Authors
1.3K
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5
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- MB
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3
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1–5 of 1.3K
Institutions
506
Centre National de la Recherche Scientifique
Paris, France
10 h-index
30 publications
1.3K citations
Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
9 h-index
37 publications
1.4K citations
University of Florence
Florence, Italy
9 h-index
23 publications
1.6K citations
Utrecht University
Utrecht, The Netherlands
9 h-index
25 publications
2.4K citations
Geological Survey of Canada
Ottawa, Canada
7 h-index
15 publications
1.5K citations
British Geological Survey
Nottingham, United Kingdom
7 h-index
14 publications
494 citations
China University of Geosciences (Beijing)
Beijing, China
7 h-index
12 publications
547 citations
Dokuz Eylül University
Izmir, Türkiye
7 h-index
13 publications
852 citations
1–8 of 506
Venues
- Tectonophysics
20 publications · 1K citations
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- Quaternary International
19 publications · 897 citations
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- Geomorphology
18 publications · 734 citations
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- Geological Society of America Bulletin
15 publications · 2.7K citations
15
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- Marine and Petroleum Geology
15 publications · 1.2K citations
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