Maximum Flooding Surfaces
Maximum Flooding Surface is a stratigraphic surface of marine origin that represents the most landward transgressive extent of a marine shoreline, distinguished from other sequence boundaries by marking the culmination of relative sea-level rise and the transition from retrogradational to progradational stacking patterns within a depositional sequence.
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Maximum Flooding Surface
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Mark A. Partington, Philip Copestake, B. C. MITCHENER et al. · Geological Society London Petroleum Geology Conference series · 1993 · 160 citations
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University of Liverpool
Liverpool, United Kingdom
4 h-index
9 publications
722 citations
BP (United Kingdom)
London, United Kingdom
4 h-index
7 publications
622 citations

University of Alberta
Edmonton, Canada
4 h-index
4 publications
193 citations
The University of Texas at Austin
Austin, United States
4 h-index
6 publications
216 citations
Shell (Netherlands)
The Hague, The Netherlands
3 h-index
3 publications
689 citations

Imperial College London
London, United Kingdom
3 h-index
5 publications
180 citations

University of Edinburgh
Edinburgh, United Kingdom
3 h-index
4 publications
636 citations
China University of Geosciences
Wuhan, China
2 h-index
5 publications
64 citations
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11 publications · 399 citations
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8 publications · 1.5K citations
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Conference · 7 publications · 658 citations
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JSR · 5 publications · 374 citations
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3 publications · 148 citations
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