Linking Sedimentary Textures to Neoproterozoic Climate Dynamics
The Bråvika Member in Northeastern Svalbard is a Cryogenian-aged (630 to 720 Ma), northward-thickening and coarsening-upward wedge of sandstones and dolomites that sits at the boundary between two vastly different climate states: the overlying Wilsonbreen Formation, representing the Marinoan...
Other Authors: | , , , , |
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Format: | Other/Unknown Material |
Language: | unknown |
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2019
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Online Access: | https://repository.wellesley.edu/islandora/object/ir%3A863/datastream/TN/view/Linking%20Sedimentary%20Textures%20to%20Neoproterozoic%20Climate%20Dynamics.jpg |