According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type.
Published in | Earth Sciences (Volume 8, Issue 4) |
DOI | 10.11648/j.earth.20190804.11 |
Page(s) | 217-227 |
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
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Copyright © The Author(s), 2019. Published by Science Publishing Group |
Wenquanbingzhan Study Area, Metallogenic Condition, Geochemical Analysis, Factor Metering, Medium Acid Volcanic Rocks, Metallogenic Structure
[1] | Han Shengfu, Yang Shengde, Pan Tong, et al. Qinghai Provincial Department of land and resources, the third round metallogenic prospective zoning and prospecting target prediction in Qinghai Province [R]. 2005: 303-307. |
[2] | Song Yucai, Hou Zengqian, Yang Tiannan, and other "Sanjiang" sedimentary rock hosting base metal deposits: development characteristics and metallogenic model [D]. Beijing: Chinese Academy of Geological Sciences. 2012. |
[3] | Song Yucai, Hou Zengqian, Li Zheng, et al. Tuotuohe Chaqu Pacha Pb (-Zn) deposit: product of basin fluid activity in the context of continental collision [J]. Journal of Minerals, 2009, 29 (s1): 186-87. |
[4] | Song Yucai, Hou Zengqian, Yang Tiannan, et al. Basic characteristics and genetic types of the base metal deposits in the Himalaya period of Sanjiang [J]. Journal of Petrology and Mineralogy. 2011, 30 (3): 355-380. |
[5] | Sun Chongren, editor in chief, Qinghai geology and Mineral Resources Bureau. Qinghai lithostratigraphic [M]. 1997. |
[6] | Li Yong, Li Yalin, Duan Zhiming, et al. [R] Report on Regional Geological Survey of 1: 250000 Wenquanbingzhan [R]. Institute of Geological Survey, Chengdu University of Technology, 2005. |
[7] | Xu Guang, Liu Yujun, Chen Fawei, et al. 1: 200000 Mzhangcuoqin, Wenquanbingzhan map of geochemical instructions map [R]. Qinghai geological survey, 2004. |
[8] | Zheng Xiangguang, Lei Qunying, Mao Yifeng, et al. 1: 200000 Mzhangcuoqin, Wenquanbingzhan map of geochemical instructions map [R]. No. 2 Comprehensive geophysical survey team, Shaanxi Bureau of Geology and Mineral Resources. |
[9] | Xiang Yunchuan, Rentianxiang, Mu Xuzan, et al. Technical requirements for the application of geochemical data [M]. Beijing: Geological Publishing House, 2010: 41-42. |
[10] | Yang Xiaofeng, Liu Changyuan, Zhang Tairan, et al. Geochemical prospecting methods [M]. Beijing: Geological Publishing House, 2007: 129-135. |
[11] | Ruan Tianjian, Zhu Youguang. Geochemical prospecting [M]. Beijing: Geological Publishing House, 1985: 127-130. |
[12] | Zhao Lunshan, Zhang Benren. Geochemistry [M]. Beijing: Geological Publishing House, 1988: 229-242. |
[13] | Ye Qingtong, Hu Yunzhong, Yang Yueqing, et al. [M] Regional geochemical background and gold-silver-lead-zinc mineralization in the "Three Rivers" region. Beijing: Geological Publishing House, 1992. |
[14] | Ye Tianzhu, Lu Zhicheng, Pang Zhenshan, et al. Theory and method of prospecting and prediction in exploration area [M]. Beijing: Geological Publishing House, 2014: 358-376. |
[15] | Pan Tong, Luo Cairang, Yi Youchang, et al. Metallogenic regularity and metallogenic prognosis of metal minerals in Qinghai Province [M]. Beijing: Geological Publishing House, 2006: 176-203. |
[16] | Hou Zengqian, Wang Erqi, Mo Yixue, et al. Collision orogenesis and mineralization of the Qinghai-Tibet Plateau [M]. Beijing: Geological Publishing House, 2008. |
[17] | Mo Yixue, Lu Fengxiang, Shen Shangyue, et al. [M] Volcanism and Metallogenesis of the "Three Rivers" Tethys. Beijing: Geological Publishing House, 1993. |
[18] | Deng Jun, Hou Zengqian, Mo Yixue, et al. "Sanjiang" Tethys complex orogeny and mineralization [J]. deposit geology [J]. Deposit Geology, 2010, 29 (1): 37-42. |
[19] | Hou Zengqian, Song Yucai, Li Zheng, et al. New types of Pb-Zn-Ag deposits in the collision orogenic belt of the Qinghai-Tibet Plateau: basic metallogenic characteristics and structural ore-controlling model [J]. Deposit geology, 2008, 27 (2): 123-144. |
[20] | Zhang Hongrui, Yang Tiannan, Hou Zengqian, et al. Structural deformation and lead-zinc mineralization in the cha tepacha mining area, northern Sanjiang [J]. 2011, 30 (3): 467-474. |
[21] | Zheng Xiangguang, Lei Qunying, Li Jing, et al. Geochemical conditions of Yanshiping area in northern Sanjiang [J]. Geophysical and geochemical prospecting, 2016, 40 (5): 861-868. |
APA Style
Zheng Xiang Guang, Lu Lin, Mao Yi Feng, Wang Chen, Meng Jun Feng. (2019). Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sciences, 8(4), 217-227. https://doi.org/10.11648/j.earth.20190804.11
ACS Style
Zheng Xiang Guang; Lu Lin; Mao Yi Feng; Wang Chen; Meng Jun Feng. Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sci. 2019, 8(4), 217-227. doi: 10.11648/j.earth.20190804.11
AMA Style
Zheng Xiang Guang, Lu Lin, Mao Yi Feng, Wang Chen, Meng Jun Feng. Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sci. 2019;8(4):217-227. doi: 10.11648/j.earth.20190804.11
@article{10.11648/j.earth.20190804.11, author = {Zheng Xiang Guang and Lu Lin and Mao Yi Feng and Wang Chen and Meng Jun Feng}, title = {Basic Geological and Geochemical Analysis in Wenquanbingzhan Area}, journal = {Earth Sciences}, volume = {8}, number = {4}, pages = {217-227}, doi = {10.11648/j.earth.20190804.11}, url = {https://doi.org/10.11648/j.earth.20190804.11}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20190804.11}, abstract = {According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type.}, year = {2019} }
TY - JOUR T1 - Basic Geological and Geochemical Analysis in Wenquanbingzhan Area AU - Zheng Xiang Guang AU - Lu Lin AU - Mao Yi Feng AU - Wang Chen AU - Meng Jun Feng Y1 - 2019/07/18 PY - 2019 N1 - https://doi.org/10.11648/j.earth.20190804.11 DO - 10.11648/j.earth.20190804.11 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 217 EP - 227 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20190804.11 AB - According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type. VL - 8 IS - 4 ER -