Heat flow measurements in sediments of the Norwegian Sea (Table 1)
During cruises in the Norwegian Sea in 1969 and 1972 seven heat flow values were measured between Iceland and the Voring Plateau. The six eastern values of this profile show a positive trend east-southeastwards which coincides with a possible transition from oceanic to continental crust suggested by...
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Format: | Dataset |
Language: | English |
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PANGAEA
1974
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.510730 https://doi.org/10.1594/PANGAEA.510730 |