Mesozoic-Cenozoic regional stress field evolution in Svalbard
Cooling fracture orientations in diabase sills associated with the Cretaceous High Arctic Large Igneous Province and syn‐sedimentary Triassic faults help constrain a model for Svalbard's (NE Barents Shelf) Mesozoic stress field evolution. Fracture data from Edgeøya and adjacent islands in SE Sv...
Published in: | Tectonics |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/10852/83184 http://urn.nb.no/URN:NBN:no-85939 https://doi.org/10.1029/2018TC005461 |