Volume 28 Issue 3
Jun.  2022
Turn off MathJax
Article Contents
MIN Zhuang, CHEN Zhengle, PAN Jiayong, et al., 2022. Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou. Journal of Geomechanics, 28 (3): 448-463. DOI: 10.12090/j.issn.1006-6616.2021170
Citation: MIN Zhuang, CHEN Zhengle, PAN Jiayong, et al., 2022. Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou. Journal of Geomechanics, 28 (3): 448-463. DOI: 10.12090/j.issn.1006-6616.2021170

Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou

doi: 10.12090/j.issn.1006-6616.2021170
Funds:

the Science and Technology Project of Guizhou Province 2021-408

Geological Survey Projects of the China Geological Survey DD20190161

Geological Survey Projects of the China Geological Survey DD20221660-3

Guizhou Carlin-type Gold Deposit Metallogenic and Prospecting Scientific and Technological Innovation Talent Team Construction Project CXTD2021-007

China Uranium Industry Corporation-East China University of Technology Joint Innovation Fund Project NRE2021-01

Open Fund Project of State Key Laboratory of Nuclear Resources and Environment of East China University of Technology 2020NRE04

More Information
  • Received: 2021-12-21
  • Revised: 2022-05-09
  • The Jiadi gold deposit, located in southwestern Guizhou Province, is a newly discovered large-scale basalt-hosted and fine-grained disseminated gold deposit. This article focuses on the characteristics of ore-forming fluid in order to discuss the ore-forming mechanism by the fluid inclusion analyses from different mineralization stages of the deposit. Based on the field observations and laboratory analyses, the hydrothermal ore-forming processes of the deposit can be divided into three stages: the pyritization forming-stage (1st stage), the smoky-gray quartz forming-stage (2nd stage) and the sulfide forming-stage (3rd stage), among which the smoky-gray quartz forming-stage is the primary stage. The fluid inclusions are mainly composed of NaCl-H2O and CO2-NaCl-H2O type, and CO2-rich inclusions are frequently observed in the first stage minerals, with homogenization temperature (Th) ranging from 211 to 231℃, and salinity (wt) from 2.10 to 7.60 (%NaCl equiv). There are a lot of NaCl-H2O and CO2-NaCl-H2O type of inclusions in the second stage, with the homogenization temperature (Th) changing from 182 to 218℃, and the salinity (wt) from 1.40 to 5.90 (%NaCl equiv). The homogenization temperature (Th) of the third stage is generally lower than 183℃, with the salinity (wt) varying from 0.90 to 5.30 (%NaCl equiv). The results of laser Raman spectroscopy show that the inclusions generally contain CO2, CH4, N2, SO2 and other gas-phase components. As the homogeneous temperature, salinity and density of the ore-forming fluid continue to decrease, the component types in the inclusions tend to reduce. By calculating the ρ, P, pH, Eh, and ƒO2, the ore-forming environment is characterized by low to moderate temperatures, low salinity, low density, near neutrality, relative reducibility and low oxygen fugacity. The change in fluid inclusion assemblage (FIA) indicates that the mineralization occurred as the fluid CO2 content continued to decrease. The fluid mixing in the main ore-forming stage and the regional extensional structure caused strong fluid boiling, and a large number of metal components (pyrite, natural gold, etc.) were rapidly precipitated to form gold ore bodies.

     

  • Full-text Translaiton by iFLYTEK

    The full translation of the current issue may be delayed. If you encounter a 404 page, please try again later.
  • loading
  • CHEN B J, WEN C Q, HUO Y, et al., 2010. Study on fluid inclusion of the Shuiyindong gold deposit, Southwestern Guizhou[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 29(1): 45-51. (in Chinese with English abstract)
    CHEN M H, MAO J W, QU W J, et al., 2007. Re-Os dating of arsenian pyrites from the Lannigou gold deposit, Zhenfeng, Guizhou Province, and its geological significances[J]. Geological Review, 53(3): 371-382. (in Chinese with English abstract)
    DU F, 2017. Characteristics and significance of fluid inclusions from breccia ore of Getang gold deposit in Anlong, Guizhou Province[D]. Chengdu: Chengdu University of Technology. (in Chinese with English abstract)
    FAN H R, XIE Y H, WANG Y L, 1997. Fluid inclusion evidences in the processes and environments of gold deposition[J]. Journal of Precious Metallic Geology, 6(3): 204-213. (in Chinese with English abstract)
    FAN H R, HU F F, YANG J H, et al., 2005. Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong Province[J]. Acta Petrologica Sinica, 21(5): 1317-1328. (in Chinese with English abstract)
    GUO J H, 2002. Mineralizing process of micrograin-type gold deposits in Southeastern Yunnan and Northwestern Guangxi[J]. Mineral Deposits, 21(S1): 121-124. (in Chinese with English abstract)
    HAN X, 2012. The study on geologic-geochemical characteristics and causes discusses of the Lannigou Carlin-type gold deposits in Guizhou[D]. Chengdu: Chengdu University of Technology. (in Chinese with English abstract)
    HE J P, YUAN S F, WANG X Y, et al., 2018. Geochemical Characteristics of the Lianhuashan anticline in the Southwest Guizhou dense area of mineral deposits[J]. Acta Geologica Sichuan, 38(3): 384-387, 397. (in Chinese with English abstract)
    HU C W, MOU Y Z, 2015. Analysis of Geological features ofmineralization and prospecting potential of the Jiadi gold deposit in Panxian, Guizhou Province[J]. Nonferrous Metals Abstract, 30(3): 42-44. (in Chinese with English abstract)
    HU R Z, SU W C, BI X W, et al., 1995. A possible evolution way of ore-Formting hydrothermal fluid for the Carlin-type gold deposits in the Yunnan-Guizhou-Guangxi triangle area[J]. Acta Mineralogica Sinica, 15(2): 144-149. (in Chinese with English abstract)
    HU Y Z, LIU W H, WANG J J, et al., 2017. Basin-scale structure control of Carlin-style gold deposits in central Southwestern Guizhou, China: insights from seismic reflection profiles and gravity data[J]. Ore Geology Reviews, 91: 444-462. doi: 10.1016/j.oregeorev.2017.09.011
    HUA R M, CHEN P R, ZHANG W L, et al., 2005. Three major metallogenic events in Mesozoic in South China[J]. Mineral Deposits, 24(2): 99-107. (in Chinese with English abstract)
    HUANG X Q, CHEN Z L, WANG P A, et al., 2008. Fluid inclusion study of the Shazhou uranium orefield in the Xiangshan deposiţJiangxi[J]. Journal of Geomechanics, 14(2): 176-185. (in Chinese with English abstract)
    LARGE S J E, BAKKER E Y N, WEIS P, et al., 2016. Trace elements in fluid inclusions of sediment-hosted gold deposits indicate a magmatic-hydrothermal origin of the Carlin ore trend[J]. Geology, 44(12): 1015-1018. doi: 10.1130/G38351.1
    LEHRMANN D J, PAYNE J L, PEI D H, et al., 2007. Record of the end-Permian extinction and Triassic biotic recovery in the Chongzuo-Pingguo platform, southern Nanpanjiang basin, Guangxi, south China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 252(1-2): 200-217. doi: 10.1016/j.palaeo.2006.11.044
    LI J H, 2021. The study of ore-forming processes of the Jiadi and Damaidi basalt-hosted gold deposits, Southwestern Guizhou Province, China[D]. Guiyang: Guizhou University. (in Chinese with English abstract)
    LIU B, DUAN G X, 1987. The density and isochoric formulae for NaCl-H2O fluid inclusions (salinity≤25 WT%) and their applications[J]. Acta Mineralogica Sinica, 7(4): 345-352. (in Chinese with English abstract)
    LIU B, 2011. Calculation of pH and Eh for aqueous inclusions as simple system[J]. Acta Petrologica Sinica, 27(5): 1533-1542. (in Chinese with English abstract)
    LIU J M, LIU J J, 1997. Basin fluid genetic model of sediment-hosted microdisseminated gold deposits in the gold-triangle area between Guizhou, Guangxi and Yunnan[J]. Acta Mineralogica Sinica, 17(4): 448-456. (in Chinese with English abstract)
    LIU J Z, DENG Y M, LIU C Q, et al., 2006. Metallogenic conditions and model of the superlarge Shuiyindong stratabound gold deposit in Zhenfeng County, Guizhou Province[J]. Geology in China, 33(1): 169-177. (in Chinese with English abstract)
    LIU J Z, XIA Y, DENG Y M, et al., 2009. Researches on the Sbt of Shuiyindong gold deposit and significance for regional prospecting[J]. Gold Science and Technology, 17(3): 1-5. (in Chinese with English abstract)
    LIU X F, NI S Z, SU W C, 1996. Characteristics of isotope geochemistry and plutonic-origin fluid mineralization for Carlin-type gold deposits in the Yunnan-Guizhou-Guangxi[J]. Journal of Mineralogy and Petrology, 16(4): 106-111. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-KWYS199604016.htm
    LIU Y H, 2002. Analysis on the Minerogenetic Geological Condition of the Gold Ore in the Lianhuashan Anticline Western Guizhou[J]. Guizhou Geology, 19(4): 231-234. (in Chinese with English abstract)
    LU H Z, 2008. Role of CO2 fluid in the formation of gold deposits: Fluid inclusion evidences[J]. Geochimica, 37(4): 321-328. (in Chinese with English abstract)
    LU H Z, 2019. Geofluids and across earth sphere structures[J]. Journal of Geomechanics, 25(6): 1003-1012. (in Chinese with English abstract)
    MAO J W, LI Y Q, 2001. Fluid inclusions of the Dongping gold telluride deposit in Hebei Province, China: involvement of mantle fluid in metallogenesis[J]. Mineral Deposits, 20(1): 23-36. (in Chinese with English abstract)
    NIE G J, YU H M, HE S, et al., 2020. Physical simulation analysis of the Cenozoic fault activities and structural deformation mechanism of the Youjiang area[J]. Journal of Geomechanics, 26(3): 316-328. (in Chinese with English abstract)
    NIE L Q, ZHOU T F, WANG F Y, et al., 2019. Study of fluid inclusions and H-O-S isotopic compositions of Donggushan tungsten skarn deposit, Anhui Province, China[J]. Acta Petrologica Sinica, 35(12): 3825-3837. (in Chinese with English abstract) doi: 10.18654/1000-0569/2019.12.16
    PENG Y W, GU X X, ZHANG Y M, et al., 2014. Source and evolution of ore-forming fluid of the Huijiabao gold field, Southwestern Guizhou: evidences from fluid inclusions and stable isotopes[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 33(5): 666-680. (in Chinese with English abstract)
    QIU L F, WU D, WU Y, et al., 2019. Characteristics of ore-forming fluids and sources of polymetallic ore-forming materials in deep segment of uranium deposits in Niutoushan area, Xiangshan[J]. Mineral Deposits, 38(2): 291-302. (in Chinese with English abstract)
    SU W C, XIA B, ZHANG H T, et al., 2008. Visible gold in arsenian pyrite at the Shuiyindong Carlin-type gold deposit, Guizhou, China: implications for the environment and processes of ore formation[J]. Ore Geology Reviews, 33(3-4): 667-679. doi: 10.1016/j.oregeorev.2007.10.002
    SU W C, ZHANG H T, HU R Z, et al., 2012. Mineralogy and geochemistry of gold-bearing arsenian pyrite from the Shuiyindong Carlin-type gold deposit, Guizhou, China: implications for gold depositional processes[J]. Mineralium Deposita, 47(6): 653-662. doi: 10.1007/s00126-011-0328-9
    TIAN C, ZHANG W G, HE H J, et al., 2021. Mineralogical characteristics of gold-bearing pyrite and gold occurrence regularity of the Jiadi gold deposit in southwestern Guizhou Province[J]. Geology in China, 48(4): 1255-1266. (in Chinese with English abstract)
    WANG D F, LIU J Z, XIONG C J, et al., 2014. A Preliminary Study on Ore Characteristics of the Jiadi Gold Deposit in Panxian, Guizhou[J]. Journal of Guizhou University (Natural Sciences), 31(6): 55-60. (in Chinese with English abstract)
    WANG D F, 2015. A preliminary study on the geological and geochemical characteristics of the Jiadi gold deposit in Panxian, Guizhou[D]. Guiyang: Guizhou University. (in Chinese with English abstract)
    WU F Y, GE W C, SUN D Y, et al., 2003. Discussions on the lithospheric thinning in eastern China[J]. Earth Science Frontiers, 10(3): 51-60. (in Chinese with English abstract)
    WU X H, CHENG P L, XIAO C G, et al., 2013. Metallogenic geologic characteristics of Damaidi gold deposit in basalt distribution area of Western Guizhou[J]. Guizhou Geology, 30(4): 283-288. (in Chinese with English abstract)
    XIA Y, 2005. Characteristics and model for Shuiyindong gold deposit in Southwestern Guizhou, China[D]. Guiyang: Institute of Geochemistry, Chinese Academy of Sciences. (in Chinese with English abstract)
    YAN D P, ZHOU M F, SONG H L, et al., 2002, Where was south China locatedin the reconstruction of Rodinia?[D]. Eart h Science Frontiers, 9(4): 249-256. (in Chinese with English abstract)
    YAO J, 2018. Studies on ore-forming material source and ore genesis of Laozhaiwan fine-disseminated gold deposit, in Yunnan[D]. Chengdu: Chengdu University of Technology. (in Chinese with English abstract)
    ZENG G P, 2018. Study on the structurally controlling on the micro-disseminated gold deposits in the western of the Southwest Guizhou gold ore concentration area[D]. Wuhan: China University of Geosciences (Wuhan). (in Chinese with English abstract)
    ZENG S G, WANG S H, WU X H, 2014. Metallogenic Mode Disscussion of Microscopic Disseminated Type Gold Deposit in Lianhuashan Area[J]. Guizhou Geology, 31(3): 161-169. (in Chinese with English abstract)
    ZHANG L, DU D Q, ZHANG H B, et al., 2012. Study on structural ore control of Huijiapu gold mine field in Southwestern Guizhou: tectonic significance of the "Two-stairs" model[J]. Gold, 33(9): 13-18. (in Chinese with English abstract)
    ZHANG R Q, ZHOU Y, WANG X W, et al., 2009. Structural features and tectonic evolution of the Wei-Zi-Luo fault zone in Southwestern Guizhou Province[J]. Journal of Geomechanics, 15(2): 178-189. (in Chinese with English abstract)
    ZHANG T, CHEN Z L, HUANG H Y, et al., 2020. Geochemical characteristics of gold-bearing minerals and its geological significance in the Ashawayi gold deposit in the southwestern Tianshan Orogen[J]. Journal of Geomechanics, 26(3): 443-458. (in Chinese with English abstract)
    ZHAO F Y, XIAO C G, ZHANG B Q, et al., 2018. REE and isotopic features of the Jiadi gold deposit in Panxian county, Guizhou Province and its ore-forming material source[J]. Geology and Exploration, 54(3): 465-478. (in Chinese with English abstract)
    ZHENG L L, 2017. Mineralization mechanism and ore-forming process of the Nibao gold deposit in Southwestern Guizhou, China[D]. Guiyang: Guizhou University. (in Chinese with English abstract)
    ZHU L M, JIN J F, HE M Y, et al., 1997. An initial study of the mineralization of plutonic fluid of the fine disseminated gold deposit in Southwest Guizhou Province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 16(3): 173-177. (in Chinese with English abstract)
    ZHUO Y Z, HU R Z, XIAO J F, et al., 2019. Trace elements and C-O isotopes of calcite from Carlin-type gold deposits in the Youjiang Basin, SW China: constraints on ore-forming fluid compositions and sources[J]. Ore Geology Reviews, 113: 103067. doi: 10.1016/j.oregeorev.2019.103067
    陈本金, 温春齐, 霍艳, 等, 2010. 黔西南水银洞金矿床流体包裹体研究[J]. 矿物岩石地球化学通报, 29(1): 45-51. doi: 10.3969/j.issn.1007-2802.2010.01.007
    陈懋弘, 毛景文, 屈文俊, 等, 2007. 贵州贞丰烂泥沟卡林型金矿床含砷黄铁矿Re-Os同位素测年及地质意义[J]. 地质论评, 53(3): 371-382. doi: 10.3321/j.issn:0371-5736.2007.03.010
    杜放, 2017. 贵州安龙戈塘金矿角砾状矿石流体包裹体特征研究及意义[D]. 成都: 成都理工大学.
    范宏瑞, 谢奕汉, 王英兰, 1997. 流体包裹体与金矿床的成矿及勘探评价[J]. 贵金属地质, 6(3): 204-213. https://www.cnki.com.cn/Article/CJFDTOTAL-GJSD703.006.htm
    范宏瑞, 胡芳芳, 杨进辉, 等, 2005. 胶东中生代构造体制转折过程中流体演化和金的大规模成矿[J]. 岩石学报, 21(5): 1317-1328. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200505000.htm
    国家辉, 2002. 滇东南桂西北微细粒型金矿成矿作用探讨[J]. 矿床地质, 21(S1): 121-124. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ2002S1038.htm
    韩雪, 2012. 贵州烂泥沟卡林型金矿床地质地球化学特征及成因探讨[D]. 成都: 成都理工大学.
    何金坪, 苑顺发, 汪小勇, 等, 2018. 黔西南矿集区莲花山背斜区地球化学特征[J]. 四川地质学报, 38(3): 384-387, 397. doi: 10.3969/j.issn.1006-0995.2018.03.007
    胡瑞忠, 苏文超, 毕献武, 等, 1995. 滇黔桂三角区微细浸染型金矿床成矿热液一种可能的演化途径: 年代学证据[J]. 矿物学报, 15(2): 144-149. doi: 10.3321/j.issn:1000-4734.1995.02.005
    胡承伟, 牟永忠, 2015. 贵州省盘县架底金矿床成矿地质特征及找矿潜力分析[J]. 有色金属文摘, 30(3): 42-44. https://www.cnki.com.cn/Article/CJFDTOTAL-YSJW201503023.htm
    华仁民, 陈培荣, 张文兰, 等, 2005. 论华南地区中生代3次大规模成矿作用[J]. 矿床地质, 24(2): 99-107. doi: 10.3969/j.issn.0258-7106.2005.02.002
    黄锡强, 陈正乐, 王平安, 等, 2008. 江西相山铀矿田沙洲矿床流体包裹体研究[J]. 地质力学学报, 14(2): 176-185. doi: 10.3969/j.issn.1006-6616.2008.02.009
    李俊海, 2021. 贵州西南部架底和大麦地玄武岩中金矿床成矿过程研究[D]. 贵阳: 贵州大学.
    刘斌, 段光贤, 1987. NaCl—H2O溶液包裹体的密度式和等容式及其应用[J]. 矿物学报, 7(4): 345-352. doi: 10.3321/j.issn:1000-4734.1987.04.010
    刘斌, 2011. 简单体系水溶液包裹体pH和Eh的计算[J]. 岩石学报, 27(5): 1533-1542. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201105026.htm
    刘建明, 刘家军, 1997. 滇黔桂金三角区微细浸染型金矿床的盆地流体成因模式[J]. 矿物学报, 17(4): 448-456. doi: 10.3321/j.issn:1000-4734.1997.04.012
    刘建中, 邓一明, 刘川勤, 等, 2006. 贵州省贞丰县水银洞层控特大型金矿成矿条件与成矿模式[J]. 中国地质, 33(1): 169-177. doi: 10.3969/j.issn.1000-3657.2006.01.019
    刘建中, 夏勇, 邓一明, 等, 2009. 贵州水银洞Sbt研究及区域找矿意义探讨[J]. 黄金科学技术, 17(3): 1-5. doi: 10.3969/j.issn.1005-2518.2009.03.001
    刘显凡, 倪师军, 苏文超, 1996. 滇黔桂微细浸染型金矿同位素地球化学特征与深源流体成矿[J]. 矿物岩石, 16(4): 106-111. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS199604016.htm
    刘远辉, 2002. 贵州莲花山背斜金的成矿地质条件分析[J]. 贵州地质, 19(4): 231-234. doi: 10.3969/j.issn.1000-5943.2002.04.004
    卢焕章, 2008. CO2流体与金矿化: 流体包裹体的证据[J]. 地球化学, 37(4): 321-328. doi: 10.3321/j.issn:0379-1726.2008.04.006
    卢焕章, 2019. 地球中的流体和穿越层圈构造[J]. 地质力学学报, 25(6): 1003-1012. doi: 10.12090/j.issn.1006-6616.2019.25.06.083
    毛景文, 李荫清, 2001. 河北省东坪碲化物金矿床流体包裹体研究: 地幔流体与成矿关系[J]. 矿床地质, 20(1): 23-36. doi: 10.3969/j.issn.0258-7106.2001.01.004
    聂冠军, 于红梅, 何声, 等, 2020. 右江地区新生代断裂活动及构造变形机制的物理模拟分析[J]. 地质力学学报, 26(3): 316-328. doi: 10.12090/j.issn.1006-6616.2020.26.03.029
    聂利青, 周涛发, 汪方跃, 等, 2019. 安徽庐枞矿集区东顾山钨矿床成矿流体来源与演化: 来自H、O、S同位素和流体包裹体的证据[J]. 岩石学报, 35(12): 3825-3837. doi: 10.18654/1000-0569/2019.12.16
    彭义伟, 顾雪祥, 章永梅, 等, 2014. 黔西南灰家堡金矿田成矿流体来源及演化: 流体包裹体和稳定同位素证据[J]. 矿物岩石地球化学通报, 33(5): 666-680. doi: 10.3969/j.issn.1007-2802.2014.05.013
    邱林飞, 吴迪, 吴玉, 等, 2019. 相山牛头山地区铀矿床深部多金属成矿流体特征与成矿物质来源探讨[J]. 矿床地质, 38(2): 291-302. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201902005.htm
    田冲, 张文高, 何虎军, 等, 2021. 黔西南架底金矿床载金黄铁矿的矿物学特征及金的赋存规律研究[J]. 中国地质, 48(4): 1255-1266. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202104022.htm
    王大福, 刘建中, 熊灿娟, 等, 2014. 贵州盘县架底金矿矿石特征初步研究[J]. 贵州大学学报(自然科学版), 31(6): 55-60. doi: 10.3969/j.issn.1000-5269.2014.06.014
    王大福, 2015. 贵州盘县架底金矿地质地球化学特征初步研究[D]. 贵阳: 贵州大学.
    吴福元, 葛文春, 孙德有, 等, 2003. 中国东部岩石圈减薄研究中的几个问题[J]. 地学前缘, 10(3): 51-60. doi: 10.3321/j.issn:1005-2321.2003.03.004
    吴小红, 程鹏林, 肖成刚, 等, 2013. 贵州西部玄武岩分布区大麦地金矿成矿地质特征[J]. 贵州地质, 30(4): 283-288. doi: 10.3969/j.issn.1000-5943.2013.04.008
    夏勇, 2005. 贵州贞丰县水银洞金矿床成矿特征和金的超常富集机制研究[D]. 贵阳: 中国科学院研究生院(地球化学研究所).
    颜丹平, 周美夫, 宋鸿林, 等, 2002. 华南在Rodinia古陆中位置的讨论: 扬子地块西缘变质-岩浆杂岩证据及其与Seychelles地块的对比[J]. 地学前缘, 9(4): 249-256. doi: 10.3321/j.issn:1005-2321.2002.04.004
    姚娟, 2008. 云南老寨湾金矿床成矿物质来源分析及矿床成因探讨[D]. 成都: 成都理工大学.
    曾国平, 2018. 黔西南矿集区西段微细浸染型金矿构造控矿作用研究[D]. 武汉: 中国地质大学(武汉).
    张蕾, 杜定全, 张晗彬, 等, 2012. 黔西南灰家堡金矿田的构造控矿模式研究: "两层楼"模式的构造意义[J]. 黄金, 33(9): 13-18. https://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ201209003.htm
    张荣强, 周雁, 汪新伟, 等, 2009. 贵州西南部威-紫-罗断裂带构造特征及演化[J]. 地质力学学报, 15(2): 178-189. doi: 10.3969/j.issn.1006-6616.2009.02.007
    曾昭光, 王石华, 吴小红, 2014. 莲花山地区微细粒浸染型金矿成矿模式探讨: 以架底金矿为例[J]. 贵州地质, 31(3): 161-169. doi: 10.3969/j.issn.1000-5943.2014.03.001
    张涛, 陈正乐, 黄宏业, 等, 2020. 西南天山阿沙哇义金矿载金矿物地球化学特征及地质意义[J]. 地质力学学报, 26(3): 443-458. doi: 10.12090/j.issn.1006-6616.2020.26.03.038
    赵富远, 肖成刚, 张兵强, 等, 2018. 贵州盘县架底金矿稀土元素和同位素特征及成矿物质来源探讨[J]. 地质与勘探, 54(3): 465-478. doi: 10.3969/j.issn.0495-5331.2018.03.003
    郑禄林, 2017. 贵州西南部泥堡金矿床成矿作用与成矿过程[D]. 贵阳: 贵州大学.
    朱赖民, 金景福, 何明友, 等, 1997. 初论黔西南微细浸染型金矿床深源流体成矿[J]. 矿物岩石地球化学通报, 16(3): 173-177. https://www.cnki.com.cn/Article/CJFDTOTAL-KYDH703.008.htm
  • 加载中

Catalog

    Figures(8)  / Tables(3)

    Article Metrics

    Article views (704) PDF downloads(69) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return