Isotopic evidence for a Precambrian metamorphic event within the Charcot Land window, East
V tj Rb-Sr, U-Pb and K-Ar analyses on rocks and minerals from a tectonic window below a Caledonian thrust f sheet in the westernmost part of the Scoresby Sund region (70°-72°N) give evidence for a Precambrian age of formation. The Charcdt Land supracrustal sequence rests on a basement that is probab...
Main Authors: | , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1980
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.8540 http://2dgf.dk/xpdf/bull29-03-151-160.pdf |