International Journal of Mineral Processing and Extractive Metallurgy

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Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization

Received: 26 February 2020    Accepted: 17 March 2020    Published: 08 April 2020
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Abstract

The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.

DOI 10.11648/j.ijmpem.20200501.12
Published in International Journal of Mineral Processing and Extractive Metallurgy (Volume 5, Issue 1, March 2020)
Page(s) 7-19
Creative Commons

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.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Mafic Intrusion, Zirconu-Pb Dating, Gold Deposit

References
[1] McNeil, A. M., Kerrich, R. Archean lamprophyre dykes and gold mineralization, Matheson, Ontario: the conjunction of LILE-enriched mafic magmas, deep crustal structures, and Au concentration. Canadian Journal of Earth Sciences. 1986, 23: 324-343.
[2] Tu, G. Z. Two Unique Mineralization Areas in Southwest China. Bulletin of Mineralogy Petrology and Geochemistry. 2002, 21: 1-2.
[3] Chen, Y. H., Yao, S. Z., Pan, Y. M. Geochemistry of lamprophyres at the Daping gold deposit, Yunnan Province, China: Constraints on the timing of gold mineralization and evidence for mantle convection in the eastern Tibetan Plateau. Journal of Asian Earth Sciences. 2014, 93: 129-145.
[4] Gan, T., Huang, Z. L. Platinum-group element and Re-Os geochemistry of lamprophyres in the Zhenyuan gold deposit, Yunnan Province, China: Implications for petrogenesis and mantle evolution. Lithos. 2017, 282: 228-239.
[5] Lanjewa, S., Randiv, K. Lamprophyres from the Harohalli dyke swarm in the Halaguru and Mysore areas, Southern India: Implications for backarc basin magmatism. Journal of Asian Earth Sciences. 2018, 157: 329-347.
[6] Groves, D. I., Goldfarb, R. J, Gebre-Mariam, M., Hagemann, S. G., Robert, F. Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews. 1998, 13: 7-27.
[7] Yan, Y. T., Zhang, N., Li, S. R, Li, Y. S. Mineral chemistry and isotope geochemistry of pyrite from the Heilangou gold deposit, Jiaodong Peninsula, Eastern China. Geoscience Frontiers. 2014, 5: 205-213.
[8] Kovalev, K. R., Kuzmina, O. N., Dyachkov, B. A., Vladimirov, A. G., Kalinin, Y. A., Naumov, E. A., Kirillov, M. V., Annikova, I. Y. Disseminated gold–sulfide mineralization at the Zhaima deposit, eastern Kazakhstan. Geology of Ore Deposits. 2016, 58: 116-133.
[9] Wenchao, S., Keyou, Y., Ruizhong, H., Feng, C. Fluid inclusion chronological study of the carlin-type gold deposits in southwestern china: As exemplified by the lannigou gold deposit, guizhou province. Acta mineralogica sinica. 1998, 18: 359-362.
[10] Bao-cheng, P., Chang-song, L., Xian-rong, L., Chao-yong, H., Xin-guo, Z. The characteristic and origin of ore-forming fliud from micro-disseminated gold deposits in youjiang basin. Geology and Prospecting. 2005, 41: 13-17.
[11] Ressel, M. W., Henry, C. D. Igneous geology of the Carlin trend, Nevada: Development of the eocene plutonic complex and significance for Carlin-type gold deposits. Economic Geology. 2006, 101: 347-383.
[12] Chen, M., Zhang, Z., Santosh, M., Dang, Y., Zhang, W. The Carlin-type gold deposits of the “golden triangle” of SW China: Pb and S isotopic constraints for the ore genesis. Journal of Asian Earth Sciences. 2015b, 103: 115-128.
[13] Chen, Y., Chen, B. Geological-geochemical features and genesis of ShuiyindongCarlin gold deposit in southwestern Guizhou Province. Geological survey of china. 2016, 3: 10-14 (in Chinese).
[14] Pi, Q., Hu, R., Peng, K., Wu, J., Wei, C., Huang, Y. Geochronology of the Zhesang gold deposit and maficrock in Funing County of Yunnan Province, with special reference to the dynamic background of Carlin-type gold deposits inthe Dian-Qian-Gui region. Acta Petrologica Sinica. 2016a, 32: 3331-3342.
[15] Zhang, J., Su, Q., Liu, X., He, Z., Zhou, Y., Li, Z., Zhao, K. Characteristics of geology and isotopic geochemistryof the Laozhaiwan gold deposit in southeastern Yunnan Province, China. Acta Petrologica Sinica. 2014, 30: 2657-2668.
[16] Jianzhong, F., Dongbo, W., Xueming, W., Yishan, Z., Tiefeng, L. Magmatic Gold Mineralization in the Western Qinling Orogenic Belt: Geology and Metallogenesis of the Baguamiao, Liba and Xiaogouli Gold Deposits. Acta Geologica Sinica ‐ English Edition, 2004, 529-533.
[17] He, H., Wei, L., Zhang, S., Gao, Y., Xu, Y. Helium, Argon, Hydrogen and Oxygen isotopic characters of ore-forming fluid of Baguamiao gold deposit inS haanxi province. Gold. 2007, 30: 3.
[18] Jingwen, M., Yanhe, L., Hongyan, L. Helium isotopic evidence on metalgenisis of mantle fluids in the wangu gold deposit, hun an province. Geological Review. 1997, 43: 646-649 (in Chinese).
[19] Zhilin, W., Teng, D., Guojun, D., Fenghui, Z., Deru, X., Zhilin, W., Ge, L., Genwen, C. Characteristics of Ore-controlling Structures of Wangu Gold Deposit in Northeastern Hunan Province. Geotectonica et Metallogenia. 2016, 40: 281-294.
[20] Jia, D., Hu, R. Analysis of Genesis of Carlin_type Gold Deposits in Yunnan Guizhou Guangxi Triangle Area. Mineral Deposits. 2011, 20: 378-384 (in Chinese).
[21] Yuguo Z, Jishun L, Zuohua, W., Yufei, O., Qizhi, G., Deli, L., Yuanyou, H. The sources of ore-forming substance of Carlin-type gold deposit: A discussion based on the characteristics of regional stratigraphic geochemical evolution in "Gold-Triangle" area of Yunnan, Guizhou, Guangxi Provinces. Earth Science Frontiers. 2009, 16: 199-208.
[22] Bierlein, F. P., Arne, D. C., McKnight, S., Lu, J., Reeves, S., Besanko, J., Marek, J., Cooke, D. Wall-rock petrology and geochemistry in alteration halos associated with mesothermal gold mineralization, central Victoria, Australia. Economic Geology And the Bulletin Of the Society Of Economic Geologists. 2000, 95: 283-311.
[23] Zhai, M. G., Santosh, M. Metallogeny of the North China Craton: Link with secular changes in the evolving Earth. Gondwana Research. 2013, 24: 275-297.
[24] Li, L., Li, S. R., Santosh, M., Li, Q., Gu, Y., Lu, W. J., Zhang, H. F., Shen, J. F., Zhao, G. C. Dyke swarms and their role in the genesis of world-class gold deposits: Insights from the Jiaodong peninsula, China. Journal of Asian Earth Sciences. 2016, 130: 2-22.
[25] Xu, J. P., Jia, J. F., Fang, Y. C. Geological characteristics and prospecting criteria of Zhesang gold deposit in Funing county, Yunnan. Prospecting technology. 2018, 13: 085-087.
[26] Nie, F., Jiang, S., Hou, W., Liu, Y., Xiao, W. Geological features and genesis of gold deposits hosted by low-grade metamorphic rocks in central-western Inner Mongolia. Kuang chuang di zhi=Mineral deposits. 2010, 58-70. (in Chinese).
[27] Zhao, H. X., Frimmel, H. E., Jiang, S. Y., Dai, B. Z. LA-ICP-MS trace element analysis of pyrite from the Xiaoqinling gold district, China: Implications for ore genesis. Ore Geology Reviews. 2011, 43: 142-153.
[28] Zhu, R. X., Fan, H. R., Li, J. W., Meng, Q. R., Li, S. R., Zeng, Q. D. Decratonic gold deposits. Science China-Earth Sciences. 2015, 58: 1523-1537.
[29] Shao, Y. 1: 20 million Funing area regional geological research report. 1978a.
[30] Yncun, W., Xiaobing, Z., Hui, Q. The classification and the representativedeposit of micro disseminated audeposit of guangnan - funing. Yunnan Geology. 2013, 32: 259-263.
[31] Henglin, L., Xijun, L., Jifeng, X., Zhiqiang, K., Yu, S., Wenlong, H., Xuefeng, C., Weinan, W., Qiongdan, L., Ye, Y. Geochemical evolution characteristics and regional tectonic significance of mafic rocks from Youjiang Basin. Journal of Guilin University of Technology. 2015, 35: 1674-9057 (in Chinese).
[32] Wang, Z., Wu, H., Kuang, G. Haracteristics of the late paleozoic oceanic basalts andtheir eruptive environments in west guangxi. Acta petrologica sinica. 1997, 13: 135-140.
[33] Wu, G., Wu, H., Zhong, D., Kuang, G., Ji, J. Volcanic rocks of paleotethyan oceanic island and island-arc bordering yunnan and guangxi, china. Geoscience. 2000, 14: 8.
[34] Hou, Q., Fu, B., Kang, Y. Tectonic features of magmatic rocks in the southern part of the Youjiang Basin, Guangxi South China Youth Geoseience Symposium. 2003, pp 33-37 (in Chinese).
[35] Qiu, Y., Zhang, B. On eastern extension of the paleo-Tethys in South China. Regional geology of China. 2000, 19: 175-180.
[36] Cai, J. X., Zhang, K. J. A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic. Tectonophysics. 2009, 467, 35-43.
[37] Zhang, J., Jiang, T. Sedimentary characteristics of triassic back-arc basiv of youjiang and its revolution. Guangxi geology. 1994, 7: 1-14.
[38] Wei, X., Yuping, L., Li, G., Lin, Y., Daohui, P., Zhen, L. Geochemistry and tectonic setting of the babu ophiolite, southeast yunnan. Acta Mineralogica Sinica. 2008, 28: 6-14.
[39] Fang, W., Zhang, H., Jia, R. Dynamics of Triassic Back-Arc Rift Basin and its MetallogenicSequence in Gejiu of Yunnan Province to Napo of Guangxi Zhuang Autonomous Region, China. Geotectonica et Metallogenia. 2011, 35: 15.
[40] Xiaofeng, Q., Zongqi, W., Yingli, Z., Luozhong, P., Guiang, H., Fusheng, Z. Geochemistry of Permian Mafic Igneous Rocks from the Napo-Qinzhou Tectonic Belt in Southwest Guangxi, Southwest China: Implications for Arc-Back Arc Basin Magmatic Evolution. Acta Geologica Sinica - English Edition. 2012, 86: 1182-1199.
[41] Goldfarb, R. J., Santosh, M. The dilemma of the Jiaodong gold deposits: Are they unique? Geoscience Frontiers. 2014, 5: 139-153.
[42] Fan, W., Wang, Y., Peng, T., Miao, L., Guo, F. Ar-Ar and U-Pb geochronology of Late Paleozoic basalts in western Guangxi and their constraints on the eruption era of Emeishan basalt province. Chinese Science Bulletin. 2004, 49: 9 (in Chinese).
[43] Liao, S., Liu, X., Shi, Y., Huang, W., Guo, L. Products of interaction between mantle plume and island arc magma: evidence from mafic intrusion in the diabase type gold deposit in western Guangxi. Acta Mineralogica Sinica. 2013, 33: 111-113 (in Chinese).
[44] Yang, J. H., Cawood, P. A., Du, Y. S., Huang, H., Hu, L. S. Detrital record of Indosinian mountain building in SW China: Provenance of the Middle Triassic turbidites in the Youjiang Basin. Tectonophysics. 2012, 574: 105-117.
[45] Bo, S., Quanren, Y., Zhongjin, X., Huiming, C., Tieqiu, M., Guangyuan, Y. Sedimentary Characteristics and Tectonic Setting of the Middle Triassic Pingxiang Basin, Guangxi. Acta Geologica Sinica. 2013, 97: 453-473.
[46] Zhuhuan, S., Yunbao, Y. Preliminary Study on Finding Deposit of Micro-Grain Type Gold Deposits in Southeast Yunnan. West-China Exploration Engineering. 2007, 133: 65-68.
[47] Hongzhang, D., Cuihua, C., Xuexiang, G., Baohua, L., Shuyi, D., Wenbin, C. Characteristics of Ore-forming Fluids from Zhesang Gold Deposit in Funing County, Yunnan Province. Geoscience. 2014, 28: 893-904 (in Chinese).
[48] Hongzhang, D., Cuihua, C., Jiajun, Y., Chaoxin, H. Elemental Geochemical Characteristics of the Zhesang Gold Deposit in the Yunnan Province and Their Geological Significance. Bulletin of mineralogy, and petrology and geochemistry. 2015, 34: 11.
[49] Shao, Y. 1: 200000 FuNing's mineral map. 1978b.
[50] Li, J., Liang, X., Dong Y., Tu, X., Xu, J. Precise Measurement reconcentration of natural rock sample by MC-ICPMS using iridium to correct for mass fractionation. Geochimica. 2007, 36: 153-160 (in Chinese).
[51] Xie, J., Yang, X., Du, J., Sun, W. Zircon U-Pb geochronology of the Mesozoicintrusive rocks in the Tongling reigon: ImPlicaitons for copper-gold mineralizaiton. Acta Petrologica Sinica. 2008, 24: 1782-1800.
[52] Wenlong, Z., Bo, L., Qing, H., Liu, M. Disscussion on Mineralization Characteristics and Genesis of Cu-Ni Sulfide Deposits of Weidong in Funing mafic intrusion Area. Science Technology and Engineering. 2013, 13: 5908-5914.
[53] Chen, G., Yang, B. Fractal features of spatial distribution of gold deposits in dian-qian-gui region. Contributions to geology and mineral resouces research. 1996, 11: 44-50 (in Chinese).
[54] JianQiang, Z. Ore characteristics and modes of occurrence of gold in the Zhesang gold deposit, Yunnan. Geology and Mineral Resources of South China. 2014, 30: 383-388.
[55] Nengxue, S., Xujun, L., Shupeng, Z. The metallogenetic enrichment rule of weilin au deposit, funing. Yunnan Geology. 2011, 30: 134-137.
[56] Guo, J. Mineralizing Process of Micrograin-type Gold Deposits in Southeastern Yunnan and Northwestern Guangxi. Mineral Deposits. 2004, 21: 4.
[57] Liu, J., Ye, J., Liu, J., Xuexiang, G. Relationship Between Sediments_hosted Micro_disseminated GoldDeposits and Basin Evolution: Case Study in Youjiang Basin, South China. Mineral Deposits. 2001, 20: 11.
[58] Zhou, M. F., Zhao, J. H., Qi, L., Su, W., Hu, R. Zircon U-Pb geochronology and elemental and Sr–Nd isotope geochemistry of Permian mafic rocks in the Funing area, SW China. Contributions to Mineralogy and Petrology. 2005, 151: 1-19.
[59] Pi, Q. H., Hu, R. Z., Xiong, B., Li, Q. L., Zhong, R. C. In situ SIMS U-Pb dating of hydrothermal rutile: reliable age for the Zhesang Carlin-type gold deposit in the golden triangle region, SW China. Mineralium Deposita. 2017, 52: 1179-1190.
[60] Chen, C., He, B., Gu, X. Relationship between evolution of the youjiang sedimentary basin and metallogenesis of micro-disseminated gold deposits. Geology and prospecting. 2004, 40: 21-25 (in Chinese).
[61] WenDou, D., NengPing, S., WenChao, S., JiaLi, C. Study on the ore-forming fluid geochemistry of the Anna gold deposit in southeastern Yunnan Province, China. Acta Petrologica Sinica. 2016, 32: 10.
[62] Mingcong, W., ZhuXia, L., Yanlin, M., Peihua, S. Geological Features and Genesis of the Laozhaiwan Gold Deposit in Southeastern Yunnan Province. Geology and Exploration. 2011, 47: 261-267.
[63] Zhao, D., Chen, C., Gu, X., Li, B., Dai, H. Geochemical characteristics of trace and rare earth elements in the Laozhaiwan gold deposit, Yunnan. Mineral Deposits. 2012, 31: 463-464.
[64] Cuihua, C., Dekun, Z., Xuexiang, G., Hongzhang, D. Discussion on Ore-forming Material Sources of the Laozhaiwan Gold Deposit, Yunnan. Bulletin of mineralogy, and petrology and geochemistry. 2014, 33: 23-30 (in Chinese).
[65] Hu, R., Fu, S., Huang, Y., Zhou, M. F., Fu, S., Zhao, C., Wang, Y., Bi, X., Xiao, J. The giant South China Mesozoic low-temperature metallogenic domain: Reviews and a new geodynamic model. Journal of Asian Earth Sciences. 2017b, 137: 9-34.
[66] Hu, R. Z., Chen, W. T., X, D. R., Zhou, M. F. Reviews and new metallogenic models of mineral deposits in South China: An introduction. Journal of Asian Earth Sciences. 2017a, 137: 1-8.
[67] Zhu, J., Zhong, H., Xie, G., Zhao, C., Xu, L., Lu, G. Origin and geological implication of the inherited zirconfrom felsic dykes, Youjiang basin, China. Acta Petrologica Sinica. 2016, 32: 3269-3280.
[68] Qi, Y., Hu, R., Zhang, H., Ren, G., Wu, L., Zhu, J., Wang, X., Meng, C., Jin, X. Zircon U-Pb Geochronology and Geochemical Characteristics of The Mafic Intrusions in Northwestern Guizhou Province, and Their Significances to the Lead-Zinc Mineralization. Acta geologica sinica. 2016, 90: 933-949.
[69] Hu, R., Fu, S., Xiao, J. Major scientific problems on low-temperature metallogenesis in South China. Acta Petrologica Sinica. 2016, 32: 3239-3251 (in Chinese).
[70] Peng, J., Hu, R. Metallogenic epoch and metallogenic tectonicenvironment of antimony deposits, south china. Geology-geochemistry. 2001, 29: 104-108.
[71] Chen, M., Mao, J., Li, C., Zhang, Z., Dang, Y. Re–Os isochron ages for arsenopyrite from Carlin-like gold deposits in the Yunnan-Guizhou-Guangxi “golden triangle”, southwestern China. Ore Geology Reviews. 2015a, 64: 316-327.
[72] Chen, M., Mao, J., Li, C., Zhang, Z., Dang, Y. Genetic types of phyllosilicate (micas) and its 39Ar-40Ar dating in Lannigou gold deposit, Guizhou Province, China. Acta Mineral Sin. 2009, 29: 353–362 (in Chinese with English abstract).
Author Information
  • Earth Sciences Institute, Guilin University of Technology, Guilin, China; Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

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    Pi Qiaohui, Wei Chaowen, Yu Huidong, Lu Di. (2020). Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. International Journal of Mineral Processing and Extractive Metallurgy, 5(1), 7-19. https://doi.org/10.11648/j.ijmpem.20200501.12

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    Pi Qiaohui; Wei Chaowen; Yu Huidong; Lu Di. Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. Int. J. Miner. Process. Extr. Metall. 2020, 5(1), 7-19. doi: 10.11648/j.ijmpem.20200501.12

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    AMA Style

    Pi Qiaohui, Wei Chaowen, Yu Huidong, Lu Di. Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. Int J Miner Process Extr Metall. 2020;5(1):7-19. doi: 10.11648/j.ijmpem.20200501.12

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  • @article{10.11648/j.ijmpem.20200501.12,
      author = {Pi Qiaohui and Wei Chaowen and Yu Huidong and Lu Di},
      title = {Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization},
      journal = {International Journal of Mineral Processing and Extractive Metallurgy},
      volume = {5},
      number = {1},
      pages = {7-19},
      doi = {10.11648/j.ijmpem.20200501.12},
      url = {https://doi.org/10.11648/j.ijmpem.20200501.12},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.ijmpem.20200501.12},
      abstract = {The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.},
     year = {2020}
    }
    

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  • TY  - JOUR
    T1  - Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization
    AU  - Pi Qiaohui
    AU  - Wei Chaowen
    AU  - Yu Huidong
    AU  - Lu Di
    Y1  - 2020/04/08
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    N1  - https://doi.org/10.11648/j.ijmpem.20200501.12
    DO  - 10.11648/j.ijmpem.20200501.12
    T2  - International Journal of Mineral Processing and Extractive Metallurgy
    JF  - International Journal of Mineral Processing and Extractive Metallurgy
    JO  - International Journal of Mineral Processing and Extractive Metallurgy
    SP  - 7
    EP  - 19
    PB  - Science Publishing Group
    SN  - 2575-1859
    UR  - https://doi.org/10.11648/j.ijmpem.20200501.12
    AB  - The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.
    VL  - 5
    IS  - 1
    ER  - 

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