Locality type: | Deposit |
Classification |
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Species: | Chalcopyrite |
Formula: | CuFeS2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Chalcopyrite data |
Locality Data: | Click here to view Jiaduoling Fe deposit, Jomdo Co. (Jiangda Co.), Qamdo Prefecture (Changdu Prefecture), Tibet, China |
Data Identifiers |
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Mindat Occurrence Record ID: | 869064 |
Long-form Identifier: | 1:3:869064:7 |
GUID (UUID V4): | 3258c53c-2a72-441d-9ec7-2dd8fec28d36 |
Nearest other occurrences of Chalcopyrite |
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16.9km (10.5 miles) | ⓘDingqinnong Cu-Ag-Pb-Zn deposit, Jomdo Co. (Jiangda Co.), Qamdo Prefecture (Changdu Prefecture), Tibet, China |
73.7km (45.8 miles) | ⓘYulong Cu-(Mo) deposit, Jomdo Co. (Jiangda Co.), Qamdo Prefecture (Changdu Prefecture), Tibet, China |
79.3km (49.3 miles) | ⓘBaomai porphyry Cu-Mo deposit, Karuo District, Qamdo Prefecture (Changdu Prefecture), Tibet, China |
83.5km (51.9 miles) | ⓘMangzong Cu-(Mo) deposit (Mangzhong Cu-(Mo) deposit), Karuo District, Qamdo Prefecture (Changdu Prefecture), Tibet, China |
88.0km (54.7 miles) | ⓘZhanaga Cu-(Mo) deposit (Zhalaga Cu-(Mo) deposit), Karuo District, Qamdo Prefecture (Changdu Prefecture), Tibet, China |
90.7km (56.3 miles) | ⓘDuoxiasongduo Cu-(Mo) deposit, Karuo District, Qamdo Prefecture (Changdu Prefecture), Tibet, China |
96.5km (59.9 miles) | ⓘHengxingcuo Cu-(Mo) deposit, Karuo District, Qamdo Prefecture (Changdu Prefecture), Tibet, 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...Yunnan a b s t r a c t The Sanjiang region in SE Tibet Plateau and NW Yunnan is known to have formed by...terrane stretching N1500 km from Yunnan to eastern Tibet. From the waning stage of subduction to postsubduction...granitoids and associated skarn-type Pb–Zn and Sn–Fe deposits in the Baoshan and Tengchong blocks were |
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