Architecture, deformation style and petrophysical properties of growth fault systems: the Late Triassic deltaic succession of southern Edgeøya (East Svalbard)

Author:

Ogata Kei1ORCID,Mulrooney Mark J.23,Braathen Alvar3ORCID,Maher Harmon4,Osmundsen Per Terje5,Anell Ingrid3,Smyrak-Sikora Aleksandra Anna26,Balsamo Fabrizio7

Affiliation:

1. Faculty of Science, Geology and Geochemistry Cluster; VU Amsterdam; Amsterdam the Netherlands

2. Department of Arctic Geology; University Centre in Svalbard; Svalbard Norway

3. Department of Geosciences; University of Oslo; Oslo Norway

4. Department of Geography and Geology; University of Nebraska at Omaha; Omaha NE USA

5. Geological Survey of Norway; Trondheim Norway

6. Department of Earth Science; University of Bergen; Bergen Norway

7. NEXT - Natural and Experimental Tectonics Research Group; Department of Chemistry, Life Sciences and Environmental Sustainability; University of Parma; Parma Italy

Funder

Petromaks Trias North Project

Norges Forskningsråd

Edison Norway

Lundin Norway

RWE Dea Norge

Statoil and Tullow Oil

Publisher

Wiley

Subject

Geology

Reference90 articles.

1. Regional constraints of the Sørkapp Basin: A Carboniferous relic or a Cretaceous depression?;Anell;Marine and Petroleum Geology,2014

2. Evidence of faulting contradicts a quiescent northern Barents Shelf during the Triassic;Anell;First Break,2013

3. Regional tectonosedimentary development of the highs and basins of the northwestern Barents Shelf;Anell;Norwegian Journal of Geology,2016

4. Influence of growth faults on coastal fluvial systems: Examples from the late Miocene to Recent Mississippi River Delta;Armstrong;Sedimentary Geology,2014

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