Major advances in quantitative basin analysis have been made during the past decade. Lithospheric processes are not only crucial as a cause of long-term subsidence but are also of fundamental importance as a cause for short-term deviations from long-term patterns of thermal subsidence. Regional and global tectonics contribute significantly to the record of sea-level changes. Both rifting and compression can give rise to phases of rapid subsidence that were hitherto commonly attributed to renewed phases of crustal stretching. These findings allow a critical appraisal of some concepts in basin formation and basin evolution that are vital in modern analysis of tectonic subsidence and basin correlation. -Authors
CITATION STYLE
Cloetingh, S., & Kooi, H. (1989). Tectonic subsidence and sea-level changes: a reappraisal. Correlation in Hydrocarbon Exploration. Proc. Conference, Bergen, 1988, 3–11. https://doi.org/10.1007/978-94-009-1149-9_1
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