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Tianshan orogenic belt, Chinai
| Regional Level Types | |
|---|---|
| Tianshan orogenic belt | Fold Belt |
| China | Country |
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The South Tianshan, a continuous tectonic belt marking the southwestern margin of the Altaids, stretches about 2500 km from western China to Central Asia. The belt is separated from the Paleozoic Yili-Central Tianshan arc by the Atbashi-Inylchek-South Nalati Fault to the north and from the Tarim Craton by the North Tarim Fault to the south. Tectonically, the South Tianshan is a fossil accretionary complex formed by the northward subduction of the Paleo-South Tianshan Ocean. It records the final suturing process between the Yili-Central Tianshan arc and the northern Tarim Craton, which is thought to have taken place in the late Paleozoic, or alternatively in the early Mesozoic.
Commodity List
This is a list of exploitable or exploited mineral commodities recorded from this region.Rock Types Recorded
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Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramList of minerals for each chemical element
Localities in this Region
- Tianshan orogenic belt
Other Regions, Features and Areas that Intersect
Asia
- Tian ShanGroup of Mountain Ranges
China
- Tianshan orogenic belt
- Boluokenu fold-beltFold Belt
Eurasian Plate
- Aktau MicrocontinentAccretionary Complex
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