Locality type: | Deposit |
Classification |
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Species: | Calcite |
Formula: | CaCO3 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Calcite data |
Locality Data: | Click here to view Diantan Sn-Fe deposit, Diantan, Tengchong Sn belt, Tengchong County, Baoshan, Yunnan, China |
Data Identifiers |
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Mindat Occurrence Record ID: | 755255 |
Long-form Identifier: | 1:3:755255:7 |
GUID (UUID V4): | 1b32425e-8ade-476c-9a7c-956efb75b009 |
Nearest other occurrences of Calcite |
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31.4km (19.5 miles) | ⓘLiancheng Cu deposit, Lanping County, Nujiang, Yunnan, China |
32.8km (20.4 miles) | ⓘDatongchang Sn-Pb-Zn deposit (Dadongchang Sn-Pb-Zn deposit), Tengchong Sn belt, Tengchong County, Baoshan, Yunnan, China |
63.1km (39.2 miles) | ⓘCaoziwa Pb–Zn deposit, Tengchong County, Baoshan, Yunnan, China |
72.0km (44.8 miles) | ⓘTiechang Sn deposit (Yunlong Sn deposit), Lancang river valley (Lancangjiang valley; Mekong valley), Yunlong County, Dali, Yunnan, China |
75.1km (46.6 miles) | ⓘHetaoping Pb-Zn deposit, Longyang District, Baoshan, Yunnan, China |
79.8km (49.6 miles) | ⓘJinchanghe Mine, Longyang District, Baoshan, Yunnan, China |
98.6km (61.3 miles) | ⓘTuganzhai iREE deposit, Lianghe County, Dehong, Yunnan, China |
References |
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Reference Search (possible matching items) |
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| Deng, Jun, Wang, Qingfei, Li, Gongjian, Li, Chusi, Wang, Changming (2014) Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region, SW China. Gondwana Research, 26 (2) 419-437 doi:10.1016/j.gr.2013.08.002 | Journal (article/letter/editorial) | important mineral deposits in the Sanjiang region, SW China☆ Jun Deng a,⁎, Qingfei Wang a,b, Gongjian Li a,...and Mineral Resources, China University of Geosciences, Beijing 100083, China Department of Geological...Metallogeny Yunnan a b s t r a c t The Sanjiang region in SE Tibet Plateau and NW Yunnan is known to...ophiolites (473–439 Ma) in the Changning–Menglian belt indicate the existence of a Proto-Tethys ocean in...the early-Paleozoic, one occurred in the Baoshan and Tengchong blocks at 502–455 Ma and the other occurred |
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