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Topaz from
Dachang Sn-polymetallic ore field, Nandan County, Hechi, Guangxi, China


Locality type:Ore Field
Classification
Species:Topaz
Formula:Al2(SiO4)(F,OH)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Topaz data
Locality Data:Click here to view Dachang Sn-polymetallic ore field, Nandan County, Hechi, Guangxi, China
Data Identifiers
Mindat Occurrence Record ID:738718
Long-form Identifier:1:3:738718:0
GUID (UUID V4):19671de1-f32f-4b3e-aa11-7b6d2a944ca6
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Genesis of tin-dominant polymetallic deposits in the Dachang district, South China: Insights from cassiterite...oregeorev.2018.03.023 OREGEO 2539 To appear in: Ore Geology Reviews Received Date: Revised Date: Accepted...Genesis of tin-dominant polymetallic deposits in the Dachang district, South China: Insights from cassiterite...cassiterite U–Pb ages and trace element compositions, Ore Geology Reviews (2018), doi: https://doi.org/10.1016/j... Genesis of tin-dominant polymetallic deposits in the Dachang district, South China: Insights from cassiterite
Journal (article/letter/editorial)
tourmaline from the Dachang Sn-polymetallic ore deposit, Guangxi Province, P.R. China Shao-Yong Jiang b...Academy of Geological Science, Beijing, 100037, China c Department of Earth Sciences, UniÕersity of Bristol...Abstract The Dachang Sn-polymetallic ore deposit ŽGuangxi, China. is one of the largest Sn deposits in...massive and vein orebodies. Various models for the ore genesis of the deposit have been proposed, and the...the major debate focuses on whether the stratiform Sn–Pb–Zn orebodies are syn-sedimentary in origin or
Journal (article/letter/editorial)
overgrown by K-feldspar, muscovite, quartz and topaz megacrysts. The PT E increasing number and size...of magmatic plagioclase and crystallization of topaz megacrysts resulting from infiltration of Na- rich...to the un-altered milky white granites. LILE and Sn do not show clear variation trends throughout the...(e.g. co-occurrence of topaz, Li–Fe mica and albite, high F, Li, CE Rb, Ga, Sn and Nb contents; and low...(1976) suggested late Proterozoic ages based on the field relations, whereas El Gaby et PT E al. (1988,
 
Mineral and/or Locality  
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