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...

Full description

Bibliographic Details
Published in:Tectonics
Main Authors: Maher, Harmon, Senger, Kim, Braathen, Alvar, Mulrooney, Mark Joseph, Smyrak-Sikora, Aleksandra, Osmundsen, Per Terje, Ogata, Kei
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/10852/83184
http://urn.nb.no/URN:NBN:no-85939
https://doi.org/10.1029/2018TC005461