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| Hardenbol, J; Vail, Pr; Ferrer, J; Montadert, L; Blanchet, R. |
| Interaction between basement subsidence, eustatic sea-level changes, and varying sediment supply shapes the sediment accumulations along passive continental margins. Detailed analysis of the sediments with seismic stratigraphy and well data permits quantification of the subsidence history and reconstruction of paleoenvironments and sea-level changes through time. Geohistory analysis provides a quantitative analysis of basin subsidence using geologic time-depth diagrams to visualize the total basin subsidence. Long-term eustatic changes are a significant component of the thermo-tectonic subsidence curve. These changes can be quantified by measuring dpearture from an established set of calculated subsidence curves. Short-term, rapid changes of sea level can... |
| Tipo: Text |
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| Ano: 1981 |
URL: http://archimer.ifremer.fr/doc/00245/35652/34161.pdf |
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