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Abnormal heat flow and the trough’s nature in the Northern Svalbard plate
Abnormal heat flow in the Northern Svalbard plate was investigated. The study discovered the recent activity of western troughs (the Orel trough and Spitsbergen grabenfjords); we cannot state the same for eastern troughs (the Franz Victoria trough and others). Their tectonic origin is quite evident,...
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Published in: | Doklady earth sciences 2009-02, Vol.424 (1), p.29-35 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that cite this one |
Online Access: | Get full text |
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Summary: | Abnormal heat flow in the Northern Svalbard plate was investigated. The study discovered the recent activity of western troughs (the Orel trough and Spitsbergen grabenfjords); we cannot state the same for eastern troughs (the Franz Victoria trough and others). Their tectonic origin is quite evident, but the peak of activity occurred in the late Mesozoic [5, 6], and at present, in addition to the relaxation of the Cretaceous thermal activity, they might serve as channels for sedimentary material transport. |
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ISSN: | 1028-334X 1531-8354 |
DOI: | 10.1134/S1028334X09010073 |