南京大学学报(自然科学版) ›› 2012, Vol. 48 ›› Issue (3): 266–277.

• • 上一篇    下一篇

 脉状金矿床的成矿压力与深度:流体包裹体
方法及其影响因素*

 徐九华**,张国瑞,魏浩,林龙华,吴晓贵
  

  • 出版日期:2015-06-12 发布日期:2015-06-12
  • 作者简介: (北京科技大学资源工程系,北京,100083)
  • 基金资助:
     全国危机矿山接替资源找矿专项(20109903),国家自然科学基金项日(40972066)

 Ore-forming pressures and depths of vein gold deposits:
Fluid inclusion studies and their influence factors

 Xu Jiu一hua,Zhang Guo一Rui,Wei Hao ,Lin Long一Hua ,Wu Xiao一Gui 

  

  • Online:2015-06-12 Published:2015-06-12
  • About author: (Department of Resource and Engineering, Beijing University of Technology, Beijing, 100083,China)

摘要:  流体包裹体的捕获压力研究是成矿压力和成矿深度估算的常用方法,其结果受多种因素的影响.在综合考虑脉状金矿的地质特征、所研究包裹体体系的基础上,研究了脉状金矿床富金石英脉的成矿压力.该类金矿床富金阶段的最低形成压力范围较宽,从小秦岭烟灰色含金石英脉阶段的270-290MPa、乌拉山含明金石英脉的250 MPa,到东坪富金石英脉的70 - 160 MPa.流体富CO2是脉状金矿一个重要特征,尤其是造山型金矿及与侵入岩有关的金矿,估算其流体捕获压力时应该利用CO2一H2O体系或CO2 - H2O-NaCI体系的压力计方法.压力与CO2部分均一温度(Tm,co2)有明显的负相关关系,反映了CO2密度与压力的密切关系.CO2丰度高且密度较高的金矿床具有较高的成矿压力.为使获得的数据具有可比性,脉状金矿的成矿压力及深度估算应考虑包裹体类型、寄主矿物所处的构造环境、
断裂性质、断裂/矿脉的产状、岩石类型及密度等主要因素.

Abstract:  Trapping pressures of fluid inclusions are commonly used in the estimation of ore-forming pressures and depths, but the results could be affected by various factors.This paper studies the orrforming pressures of gold- rich quartz veins based on comprehensive geologic characteristics of vein gold deposits and fluid inclusion systems. The minimum orrforming pressures of vein gold deposits have a comparatively wide range, which arc from 270一 290 MPa of smoky quartz vein stage for the Lesser Qinling gold deposits, 250 MPa of visible gold-bearing quartz veins for the Wulashan gold deposit,to 70一160 MPa of gold-rich quartz veins for the Dongping gold deposit. Abundant CO2 in fluids is an important feature for vein gold deposits, especially for orogenic gold deposits and
intrusiorrrclated gold deposits. CO2一H2O or CO2一H2O-NaCI system should be used in estimation of trapping pressures of fluid inclusions.There is a significantly negative correlation between pressures and Tm,co2,reflecting a close relationship between densities and pressures. A gold deposit with high-density and high CO2 content has a high ore-forming pressure. In order to obtain comparatively credible data, some important factors should be considered in the estimation of ore-forming pressure sand depth for vein gold deposits, including fluid inclusion types,ore-forming tectonic environment, fracture properties and their occurrence, as well as features and densities of wallrocks.

[1]Roedder E. Fluid inclusions. Reviews in Miner-alogy,1984,12:1~644
[2]Shepherd T J,Pankin A H,Aldcrton D H M. A practical guide to fluid inclusion studies. New York;Chapman and Hall,198,1一235.
[3]Liu B, Shcn K.Thcrmodynamics of fluid Inclu- sions. Beijing; Geological Publishing House,1999, 1-290.(刘斌,沈崖.流体包裹体热
力学.北京:地质出版社,1999, 1 -290).
[4]Lv G X. R escarch and measure to the depth of mineralization for Linglong gold deposit in Shandong Province. Chinese Science Bulletin,
1995,0(15);1399-1402.(吕占贤. ili东省玲珑金矿田成矿深度的研究与测算.科学通报,1995,40(15):1399一1402).
[5]Sun F Y,Jin W,Li B L,et al. Considerations on the mineralizing depth of hydrothermal lode gold deposits Journal of Changchun University of Science and Technology, 2000,30(Supplemen- tary) ; 27-29.(孙丰月,金巍,李碧乐等.关于脉状热液金矿床成矿深度的思考.长春科技大学学报,2000,30(增刊);27-29).
[6]Chen B L Calculation of metallogenic depth of lode gold deposit from mineralizations structure- dynamics. Chinese Journal of Gecology, 2001,36
(3):380-384.陈柏林.从成矿构造动力学探讨脉状金矿床成矿深度.地质科学,2001 , 36(3):380一384).
[7]Hu Z G,Qian Z Z,A new idea of geological tec- tonics in the Xiaoqinling region. Geological Re- view, 1994 ,40(4) :289-295.(胡正国,钱壮志.
小秦岭地质构造新认识.地质论评,1994 , 40(4):289一295).
[8]Chen Y J,Fu S G. The metallogeny of gold de posits in west Henan. Beijing; Earthquake Press, 1992 , 1 -234.陈衍景,富士谷.豫西金矿
成矿规律.北京:地震出版杜,1992,1-234).
[9]Fan H R,Xie Y H,Zhao R,et al. Fluid inclu- sions evidence of multiple causes in quartz veins with gold for Xiaoqinling gold deposits. Chinese
Science Bulletin, 2000,45(5):537一542.(范宏瑞,谢奕汉,赵瑞等.小秦岭含金石英脉复式成因的流体包裹体证据.科学通报,2000,45(5):537一542).
[10]Fan H R,Xie Y H,Zhai M G, et al. A three stage fluid flow model for Xiaoqinling lode gold metallogenesis in Henan and Shanxi Provinces,
Central China. Acta Petrologica Sinica, 2003,19 (2) ;260-266.(范宏瑞,谢奕汉,翟明国等.豫陕小秦岭脉状金矿床三期流体运移成矿作用.
岩石学报,2003, 19(2) ;260-266).
[11]Jiang N,Xu J H,Song M X. Fluid inclusion characteristics of mesothermal gold deposits in the Xiaoqinling district,Shaanxi and Henan
provinces,People’s Republic of China. Minerali- um Deposita, 1999,34:150一162.
[12]Li S R,Li Q Z,Li W L,et al. Geochemical fea- turcs of fluid inclusions of Dongchuang Pb一Zn deposit in Xiaoqinling. Gold Geology, 1997,3
(4):21-28.(李绍儒,李强之,李文良等.小秦岭东闯铅、金矿床流体包裹体地球化学特征.黄金地质,1997,3(4):21-28).
[13]Xu J H,Ni W , Zhao Y S. A study on wall rock alteration at Dongchuang gold deposit in Xiao- qinling M T.area, west Henan. Contributions to
Geology and Mineral Resources Research,1990,18-32.(徐九华,倪文,赵彦生.豫西小秦岭东闯金矿床围岩蚀变研究.地质找矿论丛,1990,18一32).
[14]Xu J H,Xie Y L, Jiang N, et al. Mineralogical fluid inclusion, and stable isotope study of We nyu一Dongchuang gold deposits in the Xiaoqin
ling MT. Area,west Henan,China. Exploration and Minim Geology, 1998,7(4):321一332.
[15]Thiery R,Vidal J,Dubcssy J. Phase equilibria modeling applied to fluid inclusions; Liquid- vapour equilibria and calculation of the molar
CO2一CH4一N2 system. Geochimca et Cosmo- chimica Acta,l994,58:1073一1082.
[16]Collins P L F. Gas hydrates in CO2-bearing fluid inclusions and the use of freezing data for esti mation of salinity. Economic Geology, 1979,74:1435-1444
[17]Diamond L W. Review of the systcmatics CO2一H2O fluid inclusions.Lithos. 2001,55 69一99.
[18]Brown P F,Lamb,W M. P一V一T properties of fluids in the system Cl:New graphical prcsen- tations and implications for fluid inclusion stud-
ies.Geochimica et Cosmochimica Acta, 1989,53: 1209一1221.
[19]Wu Z H,Wu Z H,Wan J L,et al.Genczoic up- lift and dcnudation history of Huashan mountains; evidence from fission track thermo-
chronology of Huashan granite. Geological Sci- ence and Technology information, 2003,22(3): 27-32.(吴中海,吴珍汉,万景林等.华山新生
代降升一剥蚀历史的裂变径迹热年代学分析. 地质科技情报,2003,22(3);27-32).
[20]Zheng F S, Xu G Q, Feng Z, et al.Geological characteristics and prospective value of green- stone type gold deposits of central part of Inner
Mongolia autonomous area. Acta Geologica Sini- ca,2005,79(2);232-248.(郑翻身,徐国权,冯贞等.内蒙占中部地区绿岩型金矿地质特征及
成矿远景预测.地质学报,2005,79(2);232-248).
[21]Xu X C. Evolution of metamorphism and its dy- namics in Wulashan region, inner Mongolia. Journal of Changchun University of Earth Sci-
ence,l991,21(1);25-32.(徐学纯.内蒙占乌拉山地区变质作用演化及其动力学研究.长春地质学院学报,1991,21(1);25-32).
[22]Zhang Y,Xu L J,Sun G T.Study on the gold metallogeny and ore一control ling conditions in Wulashan Gold deposit,Inner Mongolia. Word
Geology,l997,3(19):29一33.(张渊,徐丽杰,孙戈天.内蒙乌拉山金矿控矿条件及成矿作用.世界地质,1997,3(19):2 9-33).
[23]Miao L C, Qiu Y M, Guan K,et al. Shrimp chronological study of the granitoids and miner- alization in the Hadamengou gold deposit, inner
Mongolia. Mineral Deposits,2000,2(19):182一190.苗来成,Qiu Y M,关康等.哈达门沟金矿床成岩成矿时代的定点定年研究.矿床地质,2000,2(19):182一190).
[24]Nie F J,Jiang S H,Liu Y,et al. Re-discussion on the time limitation of gold mineralization oc curring within the Hadamengou deposit,south一
central Inner Mongolia autonomous region. Acta Petrologica Sinica,2005,21(6):1719一1728.(聂凤军,江思宏,刘妍等.再论内蒙占哈达门沟
金矿床的成矿时限问题.岩石学报,2005 , 21 (6):1719一1928).
[25]Yao Z W,Zhao Z H,Zhou L D,et al. An investi- gation into the petrogenesis of the Shuiquangou syenite complex, Northwest of Hebei Province.
Acta Pctrologica Sinica, 1996,12(4):562一572. (包志伟,赵振华,周玲棣.冀西北水泉沟正长岩杂岩体的成因.岩石学报,1996, 12 0 ) ; 562一 5 72).
[26]Fan H R,Xie Y H,Zhai M G. Study of ore- forming fluids in the Dongping gold deposit,North Western Hebci. Science in China(Serics D),2001,31(7):537一544.(范宏瑞,谢奕汉,翟明国.冀西北东坪金矿成矿流体研究.中国科学(D辑),3001,31 (7):5637一544)
[27]Mao J W,Li Y Q. Fluid inclusions of the Dong- ping gold telluride deposit in Hebci Province,China; involvement of mantle fluid in metallo-
genesis. Mineral Deposits,2001 ,20(1):23一36. (毛景文,李荫清.河北省东坪蹄化物金矿床流体包裹体研究:地慢流体与成矿关系.矿床地质,2001,20(1):23一36).
[28]Frantz J D, Popp R K,Hoering T C.The com- positional limits of fluid immicibility in the sys- tem determined with the use of synthetic fluid
inclusions in conjunction with mass spcctrome- try. Chemical Geology, 1992,69:235一244.
[29]Xu J H,Ding R F, Xie Y L,et al. Pure CO2 flu- ids in the Sarekoubu gold deposit at southern margin of Altai Mountains in Xinjiang, West
China. Chinese Science Bulletin, 2005,50(4): 333一340.
[30]Portter. Pressure corrections for fluid一inclu- lion homogenization temperatures based on the volumetric properties of the system NaCI一
H2O.US Geological Survey Journal of Re search,1977,5:603一607.
[31]Dong J,Wang X D, Hao G J,et al. Statistical characteristcs of regional rock density data from Hebei Province. Geophysical & Geochemical
Exploration, 2001,25(5):321一327.(董杰,王晓东,郝国江等.河北省区域岩石密度的统计结果及空间分布特征.物探与化探,2001,25 (5):321一327).
[32]Sibson R H. Crustal stress, faulting and fluid flow. Geological Society Special Publication, 1994,78:69一84.
[33]Lv Y S, Zhu X T,Cai Y T,et al. Fluid inclu- sion planes for the Huoshaogang granite in the Yongping copper deposit,Jiangxi,eastern Chi-
na. Journal of Nanjing University(Natural Sci- ences),2012,48(3):316一327.(吕赞珊,朱筱婷,蔡逸涛等.江西永平铜矿火烧岗岩体中流
体包裹体面研究.南京大学学报(自然科学),2012,48(3):316一327).
[34]Shen K,Zhang Z M,Santosh M, et al. Origin and geological significance of high-density CO2 fluid inclusions in Charnockites from the Gang-
dese batholith, Lhasa terrane, southern Tibet. Journal of Nanjing University(Natural Sci- ences), 2012, X8(3): 278-294.(沈昆,张泽
明,Santosh M等.西藏拉萨地体冈底斯岩基紫苏花岗岩中的高密度CO:包裹体成因及其地质意义.南京大学学报(自然科学),2012, 48 (3):278一294).


No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!