Ridge subduction and crustal growth in the Central Asian Orogenic Belt: Evidence from Late Carboniferous adakites and high-Mg diorites in the western Junggar region, northern Xinjiang (west China)
The Central Asian Orogenic Belt (CAOB) is a natural laboratory for the study of accretionary tectonics and crustal growth owing to its massive generation of juvenile crust in the Paleozoic. There is a debate, however, on the mechanism of this growth. In the Baogutu area of the western Junggar region...
| Main Authors: | Tang, G., Wang, Q., Wyman, D., Li, Zheng-Xiang, Zhao, Z., Jia, X., Jiang, Z. |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2010
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/28626 |
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