Abstract
Sedimentary basins with a marine connection show significant stratigraphic variations that result from eustatic sea-level fluctuation. Other key factors that control stratigraphy include the availability of sediment and the role of tectonically induced subsidence and uplift. Tectonic activity is important in most sedimentary basins as it is a causal mechanism for the production of certain regionaland local-scale sequence boundaries, generating accommodation space, altering base levels and controlling source areas. This collection of academic and industrial studies addresses the relative roles of tectonics, eustasy and sediment supply in generating stratigraphy. This volume will be of interest to petroleum geologists and researchers in sequence stratigraphy.
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