Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Malachite from
Nanmu Cu-(Mo) deposit, Qüxü Co. (Qushui Co.), Lhasa, Tibet, China


Locality type:Deposit
Classification
Species:Malachite
Formula:Cu2(CO3)(OH)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Malachite data
Locality Data:Click here to view Nanmu Cu-(Mo) deposit, Qüxü Co. (Qushui Co.), Lhasa, Tibet, China
Data Identifiers
Mindat Occurrence Record ID:476244
Long-form Identifier:1:3:476244:7
GUID (UUID V4):0
Nearest other occurrences of Malachite
35.5km (22.1 miles) ⓘXingaguo Zn-Pb-Cu-Ag deposit, Lhünzhub Co. (Linzhou Co.), Lhasa, Tibet, China
46.8km (29.1 miles) ⓘLakang'e Cu deposit, Dagzê Co. (Dazi Co.), Lhasa, Tibet, China
48.9km (30.4 miles) ⓘKelu Cu-Au deposit (Keru Cu-Au deposit), Zhanang Co., Shannan Prefecture (Lhokha Prefecture; Lhoka Prefecture), Tibet, China
50.1km (31.1 miles) ⓘLuobadui Pb-Zn-polymetallic deposit, Lhünzhub Co. (Linzhou Co.), Lhasa, Tibet, China
52.1km (32.4 miles) ⓘQiangdui Cu-Mo deposit, Dagzê Co. (Dazi Co.), Lhasa, Tibet, China
67.2km (41.8 miles) ⓘQulong Cu-(Mo) deposit, Maizhokunggar Co. (Mozhugongka Co.), Lhasa, Tibet, China
69.5km (43.2 miles) ⓘLangmujiaguo Cu deposit, Maizhokunggar Co. (Mozhugongka Co.), Lhasa, Tibet, China
86.6km (53.8 miles) ⓘTinggong Cu-Mo deposit (Tingguan Cu-Mo deposit), Nyêmo Co. (Nimu Co.), Lhasa, Tibet, China
87.8km (54.5 miles) ⓘNuri Cu-Mo-W deposit, Nêdong Co. (Naidong Co.; Zedang Co.), Shannan Prefecture (Lhokha Prefecture; Lhoka Prefecture), Tibet, China
89.3km (55.5 miles) ⓘChongjiang Cu-(Mo-Au) deposit, Nyêmo Co. (Nimu Co.), Lhasa, Tibet, China
References
Xiaoming, Qu; Hou, Zengqian; Zaw, Khin; Youguo, Li (2007) Characteristics and genesis of Gangdese porphyry copper deposits in the southern Tibetan Plateau: Preliminary geochemical and geochronological results. Ore Geology Reviews, 31 (1). doi:10.1016/j.oregeorev.2005.03.012
 
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