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- W2065660462 abstract "A priori , the recorded relative sea-level changes during the Cretaceous must be the combined effect of tectono-eustasy, geoidal-eustasy and various crustal level changes. To this we must add the human factor of differences and errors in interpretations. A posteriori , it is claimed that geoidal-eustasy dominated during the Hauterivian, Barremian, Turonian, Santonian and Maastrichtian, that tectono-eustasy dominated during the Albian, Cenomanian, Campanian and at the Maastrichtian/Danian boundary, and that local influences of sea-floor spreading are identified from the Albian/Cenomanian boundary onwards. To this we must add the local differential crustal movements modulating the global and regional ocean level changes. Geoidal-eustasy is mainly expressed as a latitudinal differentiation of the sea-level with out-of-phase changes between the hemispheres or the both high latitude regions. Furthermore, sedimentological records seem to record short-period geoidal-eustatic cycles." @default.
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- W2065660462 date "1980-12-01" @default.
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- W2065660462 title "Relative sea-level, tectono-eustasy, geoidal-eustasy and geodynamics during the Cretaceous" @default.
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- W2065660462 doi "https://doi.org/10.1016/0195-6671(80)90042-7" @default.
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