Comparing Tibet-Himalayan and Caledonian crustal architecture, evolution and mountain building processes
The Himalaya-Tibet and Caledonide orogens are comparable in scale and are similar in various aspects. Regional suture zones are recognizable in both, although their identification is more problematic in the deeply eroded Caledonide orogen. Crustal-scale thrust belts, regional Barrovian metamorphism...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2010
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