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...

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Bibliographic Details
Published in:Polar Research
Main Authors: Ohta, Y., Krasil'šikov, A. A., Lepvrier, C., Teben'kov, A. M.
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1995
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/1954
https://doi.org/10.3402/polar.v14i3.6670