| Zhao, K.-D., Jiang, S.-Y., Ni, P., Ling, H.-F., Jiang, Y.-H. (2007) Sulfur, lead and helium isotopic compositions of sulfide minerals from the Dachang Sn-polymetallic ore district in South China: implication for ore genesis. Mineralogy and Petrology, 89 (3) 251-273 doi:10.1007/s00710-006-0148-2 | Journal (article/letter/editorial) | minerals from the Dachang Sn-polymetallic ore district in South China: implication for ore genesis K.-D...Nanjing University, Nanjing, Jiangsu Province, P.R. China Received September 1, 2005; accepted March 26, 2006...The Dachang Sn-polymetallic ore district is one of the largest tin producing districts in China. Its...exhalative-hydrothermal origin. The Dachang ore district comprises several types of ore deposits, including the Lamo...isotopic compositions of sulfide minerals in the Dachang ore district reveal a difference between massive | | Guo, Jia, Zhang, Rongqing, Sun, Weidong, Ling, Mingxing, Hu, Yongbin, Wu, Kai, Luo, Ming, Zhang, Lichuan (2018) Genesis of tin-dominant polymetallic deposits in the Dachang district, South China: Insights from cassiterite U–Pb ages and trace element compositions. Ore Geology Reviews, 95. 863-879 doi:10.1016/j.oregeorev.2018.03.023 | 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 | | Huang, Wenting, Liang, Huaying, Zhang, Jian, Wu, Jing, Chen, Xilian, Ren, Long (2019) Genesis of the Dachang Sn-polymetallic and Baoshan Cu ore deposits, and formation of a Cretaceous Sn-Cu ore belt from southwest China to western Myanmar. Ore Geology Reviews, 112. 103030 doi:10.1016/j.oregeorev.2019.103030 | Journal (article/letter/editorial) | the Dachang Sn-polymetallic and Baoshan Cu ore deposits, and formation of a Cretaceous Sn-Cu ore belt...belt from southwest China to western Myanmar Wenting Huang, Huaying Liang, Jian Zhang, Jing Wu, Xilian Chen...oregeorev.2019.103030 OREGEO 103030 To appear in: Ore Geology Reviews Received Date: Revised Date: Accepted...the Dachang Snpolymetallic and Baoshan Cu ore deposits, and formation of a Cretaceous Sn-Cu ore belt...belt from southwest China to western Myanmar, Ore Geology Reviews (2019), doi: https://doi.org/10.1016/j | | Jiang, Shao-Yong, Han, Fa, Shen, Jian-Zhong, Palmer, Martin R. (1999) Chemical and Rb–Sr, Sm–Nd isotopic systematics of tourmaline from the Dachang Sn-polymetallic ore deposit, Guangxi Province, P.R. China. Chemical Geology, 157 (1) 49-67 doi:10.1016/s0009-2541(98)00200-9 | 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) | to the un-altered milky white granites. LILE and Sn do not show clear variation trends throughout the... Li–Fe mica and albite, high F, Li, CE Rb, Ga, Sn and Nb contents; and low Mg, Ti, Zr, Ba, Sr and Eu...(1976) suggested late Proterozoic ages based on the field relations, whereas El Gaby et PT E al. (1988,...zircon, magnetite that locally intergrown with ilmenite, sphene, apatite, fluorite and cassiterite, whereas...red granites fall wholly within alkali granite field on the R1-R2 discrimination diagram (Fig. 4c). |
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