SHRIMP U-Pb zircon ages of granitoids in the Wulashan gold deposit, Inner Mongolia, China: Timing of mineralization and tectonic implications.
The Wulashan gold deposit, situated along the northwestern margin of the North China craton (NCC), is hosted by ductile-brittle faults within Archean metamorphic volcano-sedimentary rocks of the Wulashan Group. This deposit is characterized by gold-bearing quartz-K feldspar and quartz veins. Both gr...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
Bellwether Publishing
2003
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| Online Access: | http://hdl.handle.net/20.500.11937/28329 |