New sequence stratigraphic framework on a ‘passive’ margin: implications for the post-break-up depositional environment and onset of glaciomarine conditions in NE Greenland

Abstract

Detailed sequence stratigraphic frameworks have been produced for most of the Cenozoic deposits around the North Atlantic and Greenland Sea. However, the sequence stratigraphic evolution of the NE Greenland shelf, a significant part of the Atlantic Ocean margin, has so far never been interpreted. This study provides, for the first time, a detailed sequence stratigraphic interpretation of the NE Greenland shelf since the late Eocene. The tectonic evolution, eustatic sea-level change and the impact of glaciations are integrated into a consistent geological history. Based on the identification of pronounced unconformities and their correlative conformities, ten stratigraphic sequences are identified. The onset of deposition is defined by a pronounced erosional event, where late Paleocene tectonic activity caused mass wasting of the uplifted footwall of the Danmarkshavn Ridge along a c. 200 km section of the ridge. A second pronounced unconformity developed across the margin during the mid-Miocene, which caused forced regressive submarine fans to prograde across the margin. The following tectonic quiet period is overlain by glaciomarine deposits, with evidence of ice deformation reaching the present day shelf break. Unknown super-regional plate tectonic forces are suggested as a driver of sequence formation based on correlation with the Canadian Arctic.