Northern continuation of Caledonian high-pressure metamorphic rocks in central-western Spitsbergen
Caledonian low-temperature, high-pressure metamorphic rocks, as first recognised at Motalafjella, central western Spitsbergen, include characteristic brown dolostone and serpentinite. Similar rocks are scattered in the strandflats, along the eastern marginal fault of the Tertiary Forlandsundet Grabe...
Published in: | Polar Research |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Norwegian Polar Institute
1995
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Subjects: | |
Online Access: | https://polarresearch.net/index.php/polar/article/view/1954 https://doi.org/10.3402/polar.v14i3.6670 |