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Central-Southern Khingan belt, Northeast China metallogenic province, Central Asian Orogenic Belt, Eurasian Platei
| Regional Level Types | |
|---|---|
| Central-Southern Khingan belt | Mineral Belt |
| Northeast China metallogenic province | Mineral Province |
| Central Asian Orogenic Belt | Orogenic Belt |
| Eurasian Plate | Tectonic Plate |
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Type:
This belt is in the central-southern segment of the Great Xingan Range, Northeast China, eastern CAOB. Its tectonic evolution was controlled by multi-stage processes: closure of the Paleo-Asian Ocean (Late Permian-Triassic), subduction of the Mongol-Okhotsk (Early Cretaceous) and the Paleo-Pacific oceanic plate (Early Jurassic-Early Cretaceous), forming a continental margin magmatic arc and compression-extension transition setting. Mineralization is genetically associated with hypabyssal intrusions emplaced during the Triassic, Early Jurassic, and mainly Early Cretaceous.
List of minerals for each chemical element
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References
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