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Specularite from
Taochong Fe deposit, Fanchang County, Wuhu, Anhui, China


Locality type:Deposit
Classification
Species:Hematite var: Specularite
Formula:Fe2O3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Specularite data
Locality Data:Click here to view Taochong Fe deposit, Fanchang County, Wuhu, Anhui, China
Data Identifiers
Mindat Occurrence Record ID:779882
Long-form Identifier:1:3:779882:5
GUID (UUID V4):0
Nearest other occurrences of Specularite
9.2km (5.7 miles) ⓘChanglongshan Fe deposit, Fanchang County, Wuhu, Anhui, China
14.6km (9.0 miles) ⓘSuishan deposit, Fanchang County, Wuhu, Anhui, China
19.2km (12.0 miles) ⓘXiaoyangchong deposit, Fanchang County, Wuhu, Anhui, China
20.2km (12.6 miles) ⓘYaojialing Zn-Au deposit, Nanling County, Wuhu, Anhui, China
22.7km (14.1 miles) ⓘDongguashan Mine, Shizishan ore field, Tongling, Anhui, China
55.0km (34.2 miles) ⓘGushan Mine, Zhonggu Fe ore field (Zhongshan-Gushan Fe ore field; Zhonggushan Fe ore field), Dangtu County, Ma'anshan, Anhui, China
58.0km (36.1 miles) ⓘBaixiangshan Mine, Zhonggu Fe ore field (Zhongshan-Gushan Fe ore field; Zhonggushan Fe ore field), Dangtu County, Ma'anshan, Anhui, China
58.6km (36.4 miles) ⓘLongqiao Fe-Cu deposit, Lujiang Co., Hefei, Anhui, China
59.5km (37.0 miles) ⓘTaipingshan Mine (Taiping Mine), Ningwu Mining District, Jiangning District, Nanjing, Jiangsu, China
61.6km (38.3 miles) ⓘJingbian Cu-Au deposit, Lujiang Co., Hefei, Anhui, China
References
Cao, Yi; Du, Yangsong; Gao, Fuping; Hu, Lifang; Xin, Fengpei; Pang, Zhenshan (2012) Origin and evolution of hydrothermal fluids in the Taochong iron deposit, Middle–Lower Yangtze Valley, Eastern China: Evidence from microthermometric and stable isotope analyses of fluid inclusions. Ore Geology Reviews, 48. 225-238 doi:10.1016/j.oregeorev.2012.03.009
Zhang, Songsong, Xiaoyong Yang, and Lei Liu. (2023) "Evolution, Magmatic Source and Metallogenesis of A-Type Granites in the Fanchang Volcanic Basin, Middle and Lower Yangtze Metallogenic Belt: A Review" Minerals 13, no. 4: 571. https://doi.org/10.3390/min13040571
 
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