Bituminous shales of the Ravnefjeld Formation
were deposited in the subsiding East Greenland basin dur-ing the Upper Permian. The shales are exposed from Jameson Land in the south (71°N; Fig. 1) to Clavering Ø in the north (74°20′N) and have attracted consider-able attention due to their high potential as hydrocar-
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.611.1923 http://www.geus.dk/publications/review-greenland-97/gsb180p81-87.pdf |
| Summary: | were deposited in the subsiding East Greenland basin dur-ing the Upper Permian. The shales are exposed from Jameson Land in the south (71°N; Fig. 1) to Clavering Ø in the north (74°20′N) and have attracted consider-able attention due to their high potential as hydrocar- |
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