Geological investigations at the southern tip of the Americas :the development of the Patagonian Orocline and uplift of the Cordillera Darwin metamorphic complex, southernmost Chile
The Patagonian Orocline is the 90° bend in the southernmost Andes between 50°S and 56°S. New paleomagnetic data indicate that the orocline is, at least in part, the product of tectonic rotation. Field work in the Beagle Channel region of southernmost Chile provides evidence for widespread left-later...
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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The University of Texas at Austin
1993
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| Online Access: | https://dx.doi.org/10.26153/tsw/19 https://repositories.lib.utexas.edu/handle/2152/72864 |