Process Regime Changes Across a Regressive to Transgressive Turnaround in a Shelf-Slope Basin, Eocene Central Basin of Spitsbergen

摘要

The sedimentological, architectural, and stratigraphic database from one investigated shelf-margin clinothem complex in the Eocene Central Basin of Spitsbergen suggests that dominating process regimes and facies products may change several times during a sea-level cycle, even though the basin-wide processes are constant.