Stappen High–Bjørnøya Tectono-Sedimentary Element, Barents Sea-Reference-Cited by-同舟云学术

Stappen High–Bjørnøya Tectono-Sedimentary Element, Barents Sea

Published:2021-03-11 Issue: Volume: Page:M57-2016-24
ISSN:0435-4052
Container-title:Geological Society, London, Memoirs
language:en
Short-container-title:Geological Society, London, Memoirs

Author:

Tsikalas Filippos¹²^ORCID,Blaich Olav Antonio³,Faleide Jan Inge²,Olaussen Snorre⁴

Affiliation:

1. Vår Energi AS, PO Box 101, Forus, NO-4068 Stavanger, Norway

2. Department of Geosciences, University of Oslo, PO Box 1047, Blindern, NO-0316 Oslo, Norway

3. AkerBP ASA, PO Box 65, NO-1324 Lysaker, Norway

4. Department of Arctic Geology, University Centre in Svalbard, PO Box 156, NO-9171 Longyearbyen, Norway

Abstract

AbstractThe Stappen High–Bjørnøya Tectono-Sedimentary Element (TSE) is located in the western Barents Shelf and is one of the prominent tectonic elements in the area. The Stappen High comprises a shallow platform, and Bjørnøya forms its highest point with exposed outcrops. Modern seismic reflection data of improved quality in the southern part of the TSE and vintage seismic data in the northern portion are utilised. Together with updated geological information at Bjørnøya, the study provides insights into the Paleozoic–early Cenozoic evolution of the Stappen High–Bjørnøya TSE. In this context, we discuss structural inheritance and the rift development, and account for confirmed and potential hydrocarbon systems and plays.

Publisher

Geological Society of London

Subject

Geology

Reference104 articles.

1. Andreassen K. , Ødegaard C.M. and Rafaelsen B. 2007. Imprints of former ice streams, imaged and interpreted using industry three-dimensional seismic data from the south-western Barents Sea. Geological Society, London, Special Publications, 277, 151–169, https://doi.org/10.1144/GSL.SP.2007.277.01.09

2. Regional constraints of the Sørkapp Basin: A Carboniferous relic or a Cretaceous depression?

3. Regional tectono-sedimentary development of the highs and basins of the northwestern Barents Shelf;Norwegian Journal of Geology,2016

4. Anell I. , Indrevær K. and Serck C.S. 2019. Influence of structural highs on Triassic deposition on the western Barents Sea. Geological Society, London, Special Publications, 495, https://doi.org/10.1144/SP495-2018-76

5. Cenozoic exhumation on the southwestern Barents Shelf: Estimates and uncertainties constrained from compaction and thermal maturity analyses;Marine and Petroleum Geology,2016

Cited by 11 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Depositional environments and source rock potential of some Upper Palaeozoic (Devonian) coals on Bjørnøya, Western Barents shelf;Marine and Petroleum Geology;2024-05

2. Upper Jurassic to Lower Cretaceous source rocks in the Norwegian Barents Sea, part II: Insights from open- and closed-system pyrolysis experiments;Marine and Petroleum Geology;2021-12

3. Upper Jurassic to Lower Cretaceous source rocks in the Norwegian Barents Sea, part I: Organic geochemical, petrographic, and paleogeographic investigations;Marine and Petroleum Geology;2021-12

4. New insights into the late Mesozoic-Cenozoic tectono-stratigraphic evolution of the northern Lofoten-Vesterålen margin, offshore Norway;Marine and Petroleum Geology;2021-12

5. Interplay between base‐salt relief, progradational sediment loading and salt tectonics in the Nordkapp Basin, Barents Sea – Part II;Basin Research;2021-09-10