Collision-related granitoid magmatism and crustal structure of the Hunza Karakoram, North Pakistan
The Cretaceous to Miocene Karakoram Axial Batholith runs E-W across the middle Hunza Valley in north Pakistan and separates a dominantly sedimentary terrain to the north from a regional metamorphic terrain to the south. A strong phase of deformation and metamorphism associated with the c. 65-50 Ma c...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
1993
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