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...

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Bibliographic Details
Published in:Basin Research
Main Authors: Hyde, RICHARD S., Miller, HUGH G., Hiscott, RICHARD N., Wright, JAMES A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1988
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