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...
Published in: | Geological Journal |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1983
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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 |