Middle carboniferous marine transgression, Bjørnøya, Svalbard: facies sequences from an interplay of sea level changes and tectonics

Abstract The Svalbard Platform, in middle Carboniferous time, was dominated by a series of NNW‐SSE oriented, asymmetric rift basins. The Landnørdingsvika Formation represents the infill of one such basin in the Bjørnøya (Bear Island) area and consists of red beds deposited during a regional rise of...

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Bibliographic Details
Published in:Geological Journal
Main Authors: Gjelberg, J., Steel, R.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1983
Subjects:
Online Access:http://dx.doi.org/10.1002/gj.3350180102
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgj.3350180102
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3350180102