Basin architecture and thermal maturation in the strike‐slip Deer Lake Basin, Carboniferous of Newfoundland
Abstract The Deer Lake Basin is an entirely non‐marine basin associated with the Cabot fault zone. Structural and stratigraphic evidence strongly suggest dextral strike‐slip movements along the fault zone during Tournaisian‐Visean time. Two elongated, end‐on structural blocks (probable positive flow...
Published in: | Basin Research |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1988
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1365-2117.1988.tb00007.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2117.1988.tb00007.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2117.1988.tb00007.x |