A new record of the Cenomanian–Turonian transgression preserved in the Ikorfat Fault zone, Nuussuaq Basin, West Greenland
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The Ikorfat Fault zone in northern Nuussuaq, Central West Greenland, has preserved a hitherto unknown succession of Upper Cretaceous marine mudstones referred to the Itilli Formation, which have been removed by erosion on the footwall block and buried deeply below sea-level on the hanging-wall block. Outcrops in the fault zone provide new data on sedimentology, palynology, stable carbon isotopes and organic geochemistry in the lower part of the Itilli Formation. A new, detailed geological map of the study area is based on digital photogrammetry. Marine organic walled dinoflagellate cysts (dinocysts) demonstrate a late Cenomanian–Turonian age, coeval with the Oceanic Anoxic Event 2 (OAE2) and link the Nuussuaq Basin with the Baffin Bay and Sverdrup Basins. The Ikorfat Fault zone is part of the eastern boundary fault of the Nuussuaq Basin. Lower Campanian listric faults truncate the footwall block. Subsidence along steep normal faults continued during deposition of the volcanic Vaigat Formation of Danian to Selandian age. The downthrow of the hanging-wall block was around 2.5 km.
| Original language | English |
|---|---|
| Article number | 105481 |
| Journal | Cretaceous Research |
| Volume | 145 |
| Number of pages | 37 |
| ISSN | 0195-6671 |
| DOIs | |
| Publication status | Published - 2023 |
Bibliographical note
Funding Information:
The field work and the study of the samples had not been possible without funding from the Ministry of Mineral Resources in Nuuk, Greenland . Jan Schulz Adolfssen and Thomas Bang Holm participated in the field work and contributed to the discussion of the observations. At GEUS important technical assistance was provided by Jette Halskov, Annette Ryge, Charlotte Olsen, and Carsten Guvad. The constructive comments from the referees are greatly appreciated. The authors direct their warm thanks to the persons and institutions mentioned. The manuscript is published with permission of the Geological Survey of Denmark and Greenland.
Funding Information:
The field work and the study of the samples had not been possible without funding from the Ministry of Mineral Resources in Nuuk, Greenland. Jan Schulz Adolfssen and Thomas Bang Holm participated in the field work and contributed to the discussion of the observations. At GEUS important technical assistance was provided by Jette Halskov, Annette Ryge, Charlotte Olsen, and Carsten Guvad. The constructive comments from the referees are greatly appreciated. The authors direct their warm thanks to the persons and institutions mentioned. The manuscript is published with permission of the Geological Survey of Denmark and Greenland.
Publisher Copyright:
© 2023 Elsevier Ltd
- Biostratigraphy, Ikorfat Fault zone, Itilli Formation, Late Cenomanian–early Turonian transgression, Nuussuaq Basin, OAE2, Palynology, Sedimentology, Structural geology, West Greenland
Research areas
ID: 355624199