Chapter 2 Sedimentary successions of the Arctic Region (58–64° to 90°N) that may be prospective for hydrocarbons

Author:

Grantz Arthur1,Scott Robert A.2,Drachev Sergey S.34,Moore Thomas E.5,Valin Zenon C.5

Affiliation:

1. Consulting Geologist, c/o US Geological Survey, 345 Middlefield Road (M.S. 969), Menlo Park, CA 94025, USA

2. CASP, University of Cambridge, 181a Huntingdon Road, Cambridge CB3 ODH, UK

3. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

4. Present address: ExxonMobil International Ltd, ExxonMobil House, MP44 Ermyn Way, Leatherhead, Surrey KT22 8UX, UK

5. US Geological Survey, 345 Middlefield Road (M.S. 969), Menlo Park, CA 94025, USA

Abstract

AbstractA total of 143 sedimentary successions that contain, or may be prospective for, hydrocarbons were identified in the Arctic Region north of 58–64°N and mapped in four quadrants at a scale of 1:11 000 000. Eighteen of these successions (12.6%) occur in the Arctic Ocean Basin, 25 (17.5%) in the passive and sheared continental margins of the Arctic Basin and 100 (70.0%) on the Circum-Arctic continents of which one (<1%) lies in the active margin of the Pacific Rim. Each succession was assigned to one of 13 tectono-stratigraphic and morphologic classes and coloured accordingly on the map. The thickness of each succession and that of any underlying sedimentary section down to economic basement, where known, are shown on the map by isopachs. Major structural or tectonic features associated with the creation of the successions, or with the enhancement or degradation of their hydrocarbon potential, are also shown. Forty-four (30.8%) of the successions are known to contain hydrocarbon accumulations, 64 (44.8%) are sufficiently thick to have generated hydrocarbons and 35 (24.5%) may be too thin to be prospective.

Publisher

Geological Society of London

Subject

Geology

Reference30 articles.

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2. Bird K. J. Burrus R. C. Pawlewicz M. (1999) Thermal maturity (Chapter VR) in ANWR Assessment Team: Oil and Gas Resource Potential of the Arctic National Wildlife Refuge 1002 Area, Alaska 98-34, US Geological Survey, Reston, VA, Open File Reports.

3. New aerogeophysical study of the Eurasia Basin and Lomonosov Ridge: Implications for basin development

4. Busby C. J. Ingersoll R. V. , eds (1995) Tectonics of Sedimentary Basins (Blackwell Science, Cambridge, MA).

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