Jianzhao Yin
College of Earth Sciences, Jilin University, Changchun, Jilin, 130061, China; Wuhan Institute of Technology, Wuhan, Hubei, 430074, China
Shoupu Xiang
Silvercorp Metals Inc., Chaoyang District, Beijing, 100027, China
Haoyu Yin
Guinea Westfield Mining Company-Sarlu, Jinzhong, Shanxi, 031300, China
Hongyun Shi
Orient Resources Ltd., Richmond, BC, V7E 1M8, Canada
Yuhong Chao
Ganzhongnan Institute of Geology and Mineral Exploration, Nanchang, Jiangxi, 330002, China
Through a detailed study of the abundances and spatial-temporal distribution patterns of Te, Bi, As, Se, Cu, Pb, Zn, Au, and Ag in the rock types of different geological epochs in the Dashuigou independent tellurium deposit, and in combination with other research findings of previous researchers in this area, the authors conclude as follows: Abundances of the main ore-forming elements Te, Bi, As, Se, Au, and Ag are not high in the regional geological background, generally lower or close to their respective crustal Clark values, but almost all altered country rocks contain high levels of ore-forming elements. This indicates that the deposit’s ore-forming elements do not come from the country rocks. This also indicates that the geological thermal events that cause alteration and mineralization originate from depths and may be related to mantle plumes. Considering the distribution pattern of these ore-forming elements in the ore bodies’ hanging wall and footwall, the metallogenic mechanism may be as follows: Mineralization is not achieved through lateral secretion in the horizontal or near horizontal direction, but rather through the upward movement and emplacement of deep ore-forming elements driven by geological processes such as mantle plumes. In addition, the migration of deep ore-forming elements is not achieved through dispersed infiltration between overlying rock particles, but through non widespread concentrated penetrating channels. This type of channel is likely to be the expansion structures where faults from different directions intersect, or where linear faults intersect with circular structures.
[1] Yin, J.Z., 1996. Shi jie shou li du li di kuang chuang de cheng kuang ji li ji cheng kuang mo shi (Chinese) [The first and only independent tellurium deposit in the world]. Chongqing Publishing House: Chongqing. pp. 190.
[2] Chen, Y.C., Mao, J.W., Luo, Y.N., et al., 1996. Si chuan da shui gou di (jin) kuang chuang di zhi he di qiu hua xue (Chinese) [Geology and geochemistry of the Dashuigou tellurium (gold) deposit in Western Sichuan, China]. Atomic Energy Press: Beijing. pp. 146.
[3] Luo, Y.N., Fu, D.M., Zhou, S.D., et al., 1994. Si chuan shi mian xian da shui gou di kuang chuang di zhi yu cheng yin (Chinese) [Genesis of the Dashuigou tellurium deposit in Sichuan Province of China]. Bulletin of Sichuan Geology. 14(2), 101-110.
[4] Luo, Y.N., Cao, Z.M., Wen, C.Q., 1996. Da shui gou du li di kuang di zhi (Chinese) [Geology of the Dashuigou independent tellurium deposit]. Southwest Communication University Publishing House: Chengdu. pp. 30-45.
[5] Yin, J.Z., 1996. The metallogenetic model and mineralizing mechanism of Dashuigou independent tellurium deposit in Shimian County, Sichuan; the first and the only independent tellurium deposit in the world. Acta Geoscientia Sinica.17, 93-97.
[6] Yin, J.Z., Shi, H.Y., 2019. Nano effect mineral ization of rare elements-taking the Dashuigou tellurium deposit, Tibet Plateau, Southwest China as the example. Academia Journal of Scien tific Research. 7(11), 635-642.
[7] Wang, R.C., Lu, J.J., Chen, X.M., 2000. Si chuan shi mian da shui gou di kuang chuang cheng yin tan tao (Chinese) [Genesis of the Dashuigou tellurium deposit in Sichuan Province, China]. Bulletin of Mineralogy, Petrology and Geochemistry. 4, 348-349.
[8] Yin, J., Xiang, S., Chao, Y., et al., 2023. Petrochemical eigenvalues and diagrams for the iden tification of metamorphic rocks’ protolith, taking the host rocks of Dashuigou tellurium deposit in China as an example. Acta Geochimica. 42(1), 103-124. DOI: https://doi.org/10.1007/s11631-022-00583-6
[9] Yin, J., Shi, H., 2021. Fluid inclusions and me tallogenic conditions of the Dashuigou tellurium deposit, Tibet Plateau, southwest China. Geology, Earth & Marine Sciences. 3(3), 1-15. DOI: https://doi.org/10.31038/GEMS.2021331
[10] Yin, J., Shi, H., 2020. Mineralogy and stable isotopes of tetradymite from the Dashuigou tellurium deposit, Tibet Plateau, southwest China. Scientific Reports. 10(1), 4634. DOI: https://doi.org/10.1038/s41598-020-61581-3
[11] Geological Bureau of Sichuan Province, 1974. Zhong hua ren min gong he guo qu yu di zhi diao cha bao gao. 1: 200,000, Shi mian fu, Kuang chan (Chinese) [Regional geological survey report of the People’s Republic of China. 1: 200,000, Shimian Sheet, Minerals]. Geological Bureau of Sichuan Province: Chengdu.
[12] Ding, T.P., Jiang, S.Y., Wan, D.F., et al., 1995. Gui tong wei su di qiu hua xue (Chinese) [Silicon isotope geochemistry]. Geological Publishing House: Beijing. pp. 122.
[13] Cao, Z.M., Luo, Y.N., 1994. Zhong guo si chuan mo zhuang di kuang cheng yin ji cheng kuang xu lie. Zhong guo kuang wu, yan shi ji di qiu hua xue yan jiu jin zhan (Chinese) [Mineral sequence and ore genesis of the Sichuan telluride lode deposit in China. New research progresses of the mineralogy, petrology and geochemistry in China]. Lanzhou University Publishing House: Lanzhou. pp. 476-478.
[14] Cao, Z.M., Wen, C.Q., Li, B.H., et al., 1995. Shou li du li di kuang chuang cheng yin tan tao (Chinese) [Genesis of the Dashuigou tellurium deposit in Sichuan Province of China]. Science China (B). 25(6), 647-654.
[15] Yin, J.Z., Shi, H.Y., 2020. Mineralogy of tsumoite based on samples from the Dashuigou tellurium deposit, Tibet plateau, China. Geological Society of America Abstracts with Programs. 52(6). DOI: https://doi.org/10.1130/abs/2020AM-349615
[16] Yin, J.Z., Zhou, J.X., Yang, B.C., et al., 1994. Zhong guo si chuan da shui gou du li di kuang de di zhi te zheng (Chinese) [Geological characteristics of the Dashuigou tellurium deposit in Sichuan Province, China]. Earth Science Frontiers. 1(4), 241-243.
[17] Yin, J.Z., Chen, Y.C., Zhou, J.X., et al., 1995. Shi jie shou li du li di kuang chuang fu kuang wei yan de yuan yan hui fu (Chinese) [Original rock of the host rock of the Dashuigou independent tellurium deposit in Sichuan Province, China]. Bulletin of Mineralogy, Petrology and Geochemistry. 2, 114-115.
[18] Yin, J.Z., Chen, Y.C., Zhou, J.X., et al., 1996. Shi jie shou li du li di kuang chuang fu kuang wei yan de di zhi di qiu hua xue yan jiu (Chinese) [Geology and geochemistry of host rocks of the Dashuigou independent tellurium deposit in Sichuan Province, China]. Journal of Changchun University of Earth Sciences. 26(3), 322-326.
[19] Yin, J.Z., Chen, Y.C., Zhou, J.X., et al., 1996. Si chuan shi mian da shui gou du li di kuang chuang shi bian yan de di zhi di qiu hua xue yan jiu (Chinese) [Geology and geochemistry of altered rocks of the Dashuigou independent tellurium deposit in Sichuan Province, China]. Journal of Xi’an College of Geology. 18(4), 19-25.
[20] Chen, Y.C., Yin, J.Z., Zhou, J.X., 1994. The first and only independent tellurium ore deposit in Dashuigou, Shimian County, Sichuan Province, China. Scientia Geologica Sinica. 3(1), 109-113.
[21] Chen, Y.C., Yin, J.Z., Zhou, J.X., et al., 1994. Sichuan shi mian xian da shui gou du li di kuang chuang di zhi te zheng (Chinese) [Geology of the Dashuigou independent tellurium deposit of Sichuan Province]. Acta Geoscientia Sinica. 29(2), 165-167.
[22] Yin, J.Z., Zhou, J.X., Yang, B.C., 1994. Rock-forming minerals and ore-forming minerals of the Dashuigou tellurium ore deposit unique in the world—A preliminary study. Scientia Geologica Sinica. 3(2), 197-210.
[23] Yin, J.Z., Chen, Y.C., Zhou, J.X., 1994. Zhong guo si chuan da shui gou du li di kuang de kuang wu xue yan jiu (Chinese) [Mineralogical research of the Dashuigou independent tellurium deposit in Sichuan Province, China]. Bulletin of Mineralogy, Petrology and Geochemistry. 3, 153-155.
[24] Yin, J., He, D., Yin, Y., et al., 2022. On ore from the Dashuigou tellurium deposit, Tibet Plateau, Southwest China. European Journal of Applied Sciences. 10(6), 458-472. DOI: https://doi.org/10.14738/aivp.106.13599
[25] Yin, J.Z., Chen, Y.C., Zhou, J.X., et al., 1995. K-Ar isotope evidence for age of the first and only independent tellurium deposit. Science Bulletin. 40(22), 1933-1934.
[26] Shen, F.Q., 1985. Trace elements geochemistry of igneous rocks assemblage in Panxi rift. Scientific Sinica. (9), 844-855.
[27] Zhang, Q.S., 1984. Zhong guo zao qian han wu ji di zhi ji cheng kuang zuo yong (Chinese) [Geology and metallogeny of the early Precambrian in China]. Jilin People Press: Changchun. pp.536.
[28] Li, T., 1976. Di qiu zhong hua xue yuan su feng du (Chinese) [Abundance of chemical elements in the Earth]. Geochemistry. 3, 167-174.
[29] Liu, Y.J., Cao, L.M., Li, Z.L., et al., 1984. Yuan su di qiu hua xue (Chinese) [Element geochemistry]. Science Press: Beijing. pp. 510.
[30] Yin, J., Xiang, S., Yang, K., et al., 2023. Review of tellurium resources in the world and in China. Advances in Social Sciences and Management. 1(1), 41-51
Copyright © 2023 JianZhao Yin, Shoupu Xiang, Haoyu Yin, Hongyun Shi, Yuhong Chao
This is an open access article under the Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) License.
