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地质学报  2003 

紫金山地区的斑岩-浅成热液成矿系统

, PP. 253-261

Keywords: 绢云母-冰长石型,酸性硫酸盐型,浅成热液矿床,斑岩矿床,紫金山地区,福建

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Abstract:

紫金山地区绢云母-冰长石型浅成热液矿床、酸性硫酸盐型浅成热液矿床和斑岩矿床是以花岗闪长斑岩侵入体为中心的斑岩-浅成热液成矿系统的产物。其中,斑岩矿床与发育于花岗闪长斑岩顶部的高盐度岩浆流体有关;酸性硫酸盐型浅成热液矿床是近岩浆源的、从改造斑岩矿床后形成的含岩浆挥发份的热水中淀积形成的;而绢云母-冰长石型浅成热液矿床则是被侵入体侧向加热、侧向流动的中性―弱酸性热水淀积产物(相当于远成热液矿床)。

References

[1]  陈好寿.1996.紫金山铜金矿床成矿年代及同位素找矿评价研究.大地构造与成矿学,20(4):348-360.
[2]  冯建忠,王京兵.1999.与火山-斑岩有关的金银矿控矿因素.地质论评,45(增刊):154-159.
[3]  华仁民,陆建军,陈培荣,李晓峰,刘晓东,张文兰.2002.中国东部晚中生代斑岩浅成热液金(铜)体系及其成矿流体.自然科学进展,12(3):240~244.
[4]  刘晓东,黄铁心.1998.福建碧田金矿床冰长石特征及其意义.华东地质学院学报,21(4):308~314.
[5]  王培宗.1993.福建省地壳-上地幔结构及深部构造背景研究.福建地质,12(2):79~158.
[6]  张德全,李大新,赵一鸣,陈景和,李子林,张克尧.1991.紫金山矿床:我国大陆首例石英-明矾石型浅成低温热液矿床.地质论评,37(6):481-491.
[7]  张德全,李大新,赵一鸣,王文桂,顾光先.1996.五子骑龙矿床--被改造的斑岩铜矿上部带.矿床地质,15(2):109~122.
[8]  张德全,佘宏全,阎升好,徐文艺.2001b.福建紫金山地区中生代构造环境转换的岩浆岩地球化学证据.地质论评,47(6):608~616.
[9]  Fan Hongrui, Xie Yihan, Wang Yinglan, Yang Xueming and Yang Xiaoyong. 1999. Ore-forming fluid system of epithermal goldcopper-silver deposits related with volcanism and subvolcanism.Geological Review, 45 (supp.): 133 ~ 145 (in Chinese with English abstract).
[10]  Fitzmayer J R, Petersen E U. 1996. The KoriKollo Au-Ag deposit: a transitional magmatic epithermal precious metal system within the La Hoya District, Bolivia. Abstracts with Progress, Geological Society of America, 28(7): 334.
[11]  Huang Tiexin, Liu Xiaodong, Zhang Jincheng. 1996. The Bitian gold deposit-A quartz-adularia type epithermal precious metal deposit. Geology and Geochemistry, 6, 1~6 (in Chinese ).
[12]  Liu Xlaodong, Huang Tiexin. 1998. The characteristics and implication of adularia from Bitan gold depositin Fujian Province.Journal of East China Geological Institute, 21 (4):308~ 314 (in Chinese with English abstract).
[13]  Love D A, Clark A H, Hodgson C J, et al. 1998. The timing of adularia-sericite-type mineralization and alunite-kaolinite-type alteration, Mount Skukum epithermal deposit, Yukon Territory,Canada: Ar-Ar and U-Pb geochronology. Economic Geology, 93(4): 437~462.
[14]  Wang Peizong. 1993. Crust-upper mantle structure and deep structural setting of Fujian Province. Geology of Fujian, 12 (2):79~158 (in Chinese with English abstract).
[15]  Zhang Dequan, Li Daxin, Zhao Yiming, Chen Jinghe, Li Zilin, Zhang Keyao. 1992. Alteration and Mineralization zoning of the Zijinshan copper-gold deposit. Beijing: Geological Publishing House, 1~77 (in Chinese with English abstract).
[16]  hang Dequan, Li Daxin, Zhao Yiming, Wang Wengui, Gu Guangxian. 1996. The Wuziqilong deposit--the reformed upper part of a porphyry copper deposit. Mineral Deposits, 15(2): 109~122 (in Chinese with English abstract).
[17]  Zhang Dequan, She Hongquan, Yan Shenghao, Xu Wenyi. 2001b.Geochemistry of Mesozoic magmatites in the Zijinshan region and implication on regional tectonic inversion. Geological Review, 47(6): 608~616 (in Chinese with English abstract).
[18]  范宏瑞,谢奕汉,王英兰,杨学明,杨晓勇.1999.与火山潜火山作用有关的浅成热液金(铜银)矿床流体成矿系统.地质论评,45(增刊):133~145.
[19]  高天钧,黄仁生.1998.福建上杭紫金山矿田铜银金矿床类型及对比.火山地质与矿产,19(4):283-294.
[20]  黄铁心,刘晓东,张金成.1996.碧田金矿--石英-冰长石型浅成低温热液贵金属矿床.地质地球化学,(6):1~6.
[21]  那建国.1998.福建碧田银多金属矿区地质成矿特征初探.华南铀矿地质,15:20~31.
[22]  张德全,李大新,赵一鸣,陈景和,李子林,张克尧.1992.紫金山铜金矿床蚀变及矿化分带.北京:地质出版社,1~77.
[23]  张德全,李大新,丰成友,董英君.2001a.紫金山地区中生代岩浆系统的时空结构及其地质意义.地球学报,22(5):403~408.
[24]  Chen Haoshou. 1996. The research on the mineralization chronology and isotopic exploration assessment for Zijinshan copper-gold deposit. Geotectonica et Metallogenia, 20 (4): 348 ~ 360 (in Chinese with English abstract).
[25]  Feng Jianzhong, Wang Jingbin. 1999. Ore-cotroling factors for AuAg deposits related to volcanic rocks and porphyries. Geological Review, 45 (supp.): 154 ~ 159 (in Chinese with English abstract).
[26]  Gao Tianjun, Huang Rensheng. 1998. Comparison of typical characters of Zijinshan copper gold silver deposit, Shanghang, Fujian Province. Volcanology & Mineral Resouces, 19(4): 283~294 (in Chinese with English abstract).
[27]  Heald P, Foley N K, Hayba D O. 1987. Comparative anatomy of volcanic-hosted epithermal deposits: Acid-sulfate and adularlasericite types. Economic Geology, 82(1): 1~ 26.
[28]  Hua Renmin, Lu Jianjun, Chen Peirong, Li Xiaofeng, Liu Xiaodong,Zhang Wenlan. 2002. The late Mesozoic porphyry-epithermal Au-Cu system in East China and their ore-forming fluids.Progress in Natural Sciences, 12(3):240~244.
[29]  La Jlanguo. 1998. Geological and ore-forming characteristics of the Bitian silver-polymetallic deposit, Fujian Province. Uranium Deposits in South China, 15:20~31 (in Chinese).
[30]  So C S, Zhang D Q, Yun S T, Li D X. 1998. Alterationmineralization zoning and fluid inclusions of the high sulfidation epithermal Cu-Au mineralization at Zijinshan, Fujian Province,China. Economic Geology, 93(7): 961~980.
[31]  Zhang Dequan, Li Daxin, Zhao Yiming, Chen Jinghe, Li Ziling,Zhang Keyao. 1991. The Zijinshan deposit: The first example of quartz-alunite type epithermal deposit in the continent of China.Geological Review, 37 (6):481~491 (in Chinese with English abstract).
[32]  ZhangDQ, LiDX, ZhaoYM, ChenJH, ZhangKY. 1994. The Zijinshan deposit: The first example of quartz-alunite type epithermal deposit in the continent of China. Resource Geology,44(1): 93~99.
[33]  Zhand Dequan, Li Daxing, Feng Chengyou, Dong Yingjun. 2001a.The temporal and spacial framework of the Mesozoic magmatic system in the Zijinshan region and its geological significance. Acta Geoscientla Sinica, 22 (5): 403~408 (in Chinese with English abstract).

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