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Pyrite from
Xifanping Cu-Au deposit, Yanyuan County, Liangshan Yi, Sichuan, China


Locality type:Deposit
Classification
Species:Pyrite
Formula:FeS2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Pyrite data
Locality Data:Click here to view Xifanping Cu-Au deposit, Yanyuan County, Liangshan Yi, Sichuan, China
Data Identifiers
Mindat Occurrence Record ID:469188
Long-form Identifier:1:3:469188:4
GUID (UUID V4):fc84e7da-d84e-4d23-bb8f-465440fa51fe
Nearest other occurrences of Pyrite
17.2km (10.7 miles) Mofancun Cu deposit, Yanyuan County, Liangshan Yi, Sichuan, China
76.7km (47.7 miles) Nanyang, Huaping County, Lijiang, Yunnan, China
80.2km (49.8 miles) Lengshuiqing Mine, Yanbian County, Panzhihua, Sichuan, China
84.0km (52.2 miles) Dalucao REE deposit, Dechang County, Liangshan Yi, Sichuan, China
98.0km (60.9 miles) Baima V-Ti-Fe deposit, Miyi County, Panzhihua, Sichuan, China
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Yongfeng Gao . Andao Du . Deming Fu Himalayan Cu–Mo–Au mineralization in the eastern Indo–Asian collision...data on three porphyry Cu–Mo–Au deposits (Yulong, Machangqing, and Xifanping). These deposits are associated...Indo–Asian collision zone. Three distinct episodes of Cu–Mo–Au mineralization are recognized. At Yulong, Re–Os...the pre- and intra-ore porphyries, suggest that Cu–Mo–Au mineralization formed during the late stage (∼40...Baiwanzhuang Road, Beijing, 100037, People’’s Republic of China e-mail: houzengqian@126.com Tel.: +81-883-64366
Book (volume)
ordered on-line from: w w w .p o rterg e o .co m .au /b o o k sh o p SUPER PORPHYRY COPPER AND GOLD DEPOSITS:.................................285 The Porphyry Au-Cu Deposits and Related Shoshonitic M agmatism of the.................. 287 , G rasbec^ Porphyry Cu-Au Deposit Papua» In d o n esia:1 .Magmatic History John................ 313 , , G rasbcrg Porphyry Cu-Au Deposit Papua Indonesia: 2. Pervasive Hydrotherm al...Reservoir T rapped Below the Tam pakan Copper-Gold Deposit by Mio-Pliocene Crustal Compression in the Southern
 
Mineral and/or Locality  
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