Age and origin of high Ba-Sr appinite-granites at the northwestern margin of the Tibet Plateau: implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt
The Buya appinite-granite is a typical high Ba-Sr granite emplaced at the northern West Kunlun orogenic belt along the northwestern margin of the Tibetan Plateau. The granite is dated at ca. 430 Ma using the SHRIMP U-Pb zircon method. It consists of alkaline feldspar granites with coeval appinite en...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2008
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/45509 |