全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
矿床地质  2003 

从流体包裹体研究探讨金属矿床成矿条件

Keywords: 地球化学,成矿流体分类,流体包裹体,成矿条件,金属矿床,综述

Full-Text   Cite this paper   Add to My Lib

Abstract:

根据作者多年来对流体包裹体的研究成果,参考了国内外的研究结论,提出了一个新的成矿流体分类方案,并评述了我国若干典型金属矿床的研究状况,由此探讨了金属矿床的形成机制。

References

[1]  [1]Chang Y F, Liu X P and Wu Y C. 1991. The copper-iron belt of the lower and middle reaches of the Changjiang river [M]. Beijing: Geol. Pub. House. 179p (in Chinese with English abstract).
[2]  [2]Chen Y C, Ye Q T, Feng J, et al. 1996. Ore-forming conditions and metallogenic prognosis of the Ashele copper-zinc metallogenic belt, Xinjiang, China [M]. Beijing: Geol. Pub. House. 330p (in Chinses with English abstract).
[3]  [3]Hedenquist J W and Henley R W. 1985. The importance of CO2 on freezing point measurements of fluid inclusions: evidence from active geothermal systems and implication for epithermal ore deposition [J]. Econ Geol., 80(5): 1379~1406.
[4]  [5]Liu B. 1982. Studies of solid and fluid inclusions on the copper deposits in Baiyinchang [J]. Acta Geologica Sinica, 58(2): 165~173 (in Chinese with English abstract).
[5]  [6]Lu H Z, Shi J X, Yu C M, et al. 1974. Determination of the temperature of ore formation and digenesis of a deposit from southern China [J]. Geochimica, (3):145~156 (in Chinese with English abstract).& Tech. Press. 210p(in Chinese).
[6]  [7]Lu H Z. 1997. Ore-forming fluid [M]. Beijing: Beijing Sci.
[7]  [8]Ma H W. 1990. Petrology and mineralization of granites in Yulong porphyry copper belt, Tibet [M]. Wuhan: China Univ. Geosci. Press. 158p (in Chinese with English abstract).
[8]  [9]Ma X J. 1988. A study on the geochemistry of inclusions of the Dajishan tungsten ore deposit [A]. In: Li Y Q, et al. ed . Application of fluid inclusions in ore deposit and petrology[C]. Beijing: Beijing Sci. & Tech. Press. 64~112 (in Chinese with English abstract).
[9]  [10]Mao J W, Li H Y and Pei R F. 1995. Nd-Sr isotopic and petrogenetic studies of the Qianlishan granite stock, Hunan Province [J]. Mineral Deposits, 14(3): 236~242 (in Chinese with English abstract).
[10]  [11]Roedder E. 1984. Reviews in mineralogy, Vol. 12: Fluid inclusion[M]. Michigan: BookCrafters, Inc. Chelsea. 644p.
[11]  [12]Rui Z Y, Huang C K, Qi G M, et al. 1984. Porphyry copper (molybdenum)deposits of China [M]. Beijing: Geol. Pub. House. 350p(in Chinese).
[12]  [13]Rui Z Y, Li N, Wang L S. 1991. The Guanmenshan lead-zinc deposit:its basin brine ore-forming process and lead isotopic targeting [M] . Beijing: Geol. Pub. House. 208p(in Chinese with English summary).
[13]  [14]Rui Z Y, Li Y Q. 1995. Study of fluid inclusion in minerals[M]. Beijing: Geol. Pub. House. 213~241( in Chinese with English summary).
[14]  [15]Rui Z Y, Liu Y L, Wang L S, et al. 2002. The porphyry copper belt and its tectonic framework of Eastern Tianshan in Xingjiang[J]. Acta Geologica Sinica, 76(1): 83~94 (in Chinese with English abstract).
[15]  [16]Rui Z Y, Zhang H T, Wang L S, et al. 1995. The multiple metallogenic model of the porphyry-epithermal copper-gold deposits in Eastern Jilin and Heilongjiang [J]. Mineral Deposits, 14(2): 174~184(in Chinese with English abstract).
[16]  [17]Rui Z Y, Li Y Q, Wang L S, et al. 2002. Preliminary discussion on ore-forming fluid and enrichment system of metallic minerals[J]. Mineral Deposits, 21(1): 83~90(in Chinese with English abstract).
[17]  [18]Sangster D F. 1972. Precambrian volcanogenic massive deposits in canada: a review[J]. Geol. Surv. Can., 72~22: 44.
[18]  [19]Sato T. 1972. Behaviours of ore-forming solution in sea water[J]. Min. Geol., 22: 31~42.
[19]  [20]Sheng J F, Li Y D and Bel L L, et al. 1995. A study of fluid inclusions and metallogenesis of the Xihuashan tungsten deposit[J]. Bull. the Institute of Mineral Deposits, CAGS, (2): 42~61(in Chinese with Enlish abstract).
[20]  更多...
[21]  [21]Sverjensky D A. 1984. Oil field brines as ore-forming solutions [J]. Econ. Geol., 79: 23~37.
[22]  [22]Turner F J and Verhoogen J. 1960. Igneous and metamorphic petrology[M]. 2nd edition. New York: McGraw-Hill Book Co. 387~388.
[23]  [23]Von Damm K L. 1990. Seafloor hydrothermal activity: Black smoker chemistry and chimneys [J]. Ann. Rev. Earth Planet Sci., 173~204.
[24]  [24]Wang H N, Zhang J R, Dai A H, et al. 1989. Geochemistry of the Hetai gold deposit in the altered mylonite zone[J]. Mineral Deposits, 8(2): 61~71.
[25]  [25]Wang X Z, Cheng J P, Liang H Y, et al. 1995. Three-stage metallogenic model for gold deposits of metamorphosed fine-clastic rock type[J]. Mineral Deposits, 14(4): 322~328(in Chinese with English abstract).
[26]  [26]Wu Y L, Mei Y W, Liu P C, et al. 1985. Geology of the Xihuashan tungsten ore field [M]. Beijing: Geol. Pub. House. 317p (in Chinese with English abstract)..
[27]  [27]Xia L Q, Xia Z C, Xu X Y. 1996. The fluid inclusions, magmatic inclusions and glasses in mantle peridotite xenoliths[A]. In: Du L T, et al. ed. Geochemistry of mantle fluids and asthenosphere (asthenoliths)[C ]. 230~271( in Chinese with English abstract).
[28]  [28]Xia L Q. 1980. On the origin of alpine-type chromite deposits in North Western China[J]. Bull. the Xi\'an Institute fo Geology and Mineral Resources, CAGS, Series X. 1(2): 25~39(in Chinese)
[29]  [29]Xie Y H, Zhao R, Li R M, et al. 1988. Physical-chemical conditions and material sources for minerallzation of the Yinyan porphyry tin deposit [J]. Mineral Deposits, 7(3): 42~49(in Chinese with English abstract).
[30]  [30]Xu M J, Fu D M, Yin Y M, et al. 1993. The Gacun silver-polymetallic deposit in Sichuan Province [M]. Chengdu: Chengdu Sci. & Tech. Press. 164p(in Chinese ).
[31]  [31]Xue C J. 2000. Studies on the Tevtiary metallogenic series in Lanping basin, Yunnan[D]. Tutor: Chen Y C. Beijing: CAGS.
[32]  [32]Yang Y Q, Ni Y X, Guo Y Q, et al . 1987. Rock-forming and ore-forming characteristics of the Xikeng granitic pegmatites in Fujian Province[J]. Mineral Deposits, 6(3): 10~21.
[33]  [33]Yin H H, Fan W M and Lin G. 1990. Deep processes and mantle crust compound mineralization in the evolution of the Lanpin-Simao Mesozoic-Cenozoic Diwa basin in Western Yunnan, China[J]. Geotectonic et Metallogenic, 14(2): 113~124(in Chinese with English abstract).
[34]  [34]Zeng Q F and Yang B L. 1995. Preliminary study on the forming temperature of hydrothermal tungsten deposit from the Nanling range, South China[J]. Scientia Geologica Sinica, (2): 166~180(in Chinese with English abstract).
[35]  [35]Zhang W H and Chen Z Y. 1993. Geology of fluid inclusions[M]. Wuhan: Press of China Univ. Geosci. 246p(in Chinese).
[36]  [36]Zhao Y M, Lin W W, Bi C S, et al. 1990. Skarn deposits of China[M]. Beijing: Geol. Pub. House. 154p(in Chinese with English abstract).
[37]  [37]Zhao Y M. 2002. Some new important advances in study of skarn deposits[J]. Mineral Deposits, 21(2): 113~120(in Chinese with English abstract).
[38]  [38]Zou T R, Zhang X H, Jia F Y, et al. 1986. The Origin of No.3 pegmatite in Altayshan, Xinjiang[J]. Mineral Deposits, 5(4): 34~48.
[39]  [39]常印佛, 刘湘培, 吴言昌. 1991. 长江中下游铜铁成矿带[M]. 北京: 地质出版社. 379页.
[40]  [40]陈毓川, 叶庆同, 冯京, 等. 1996. 阿舍勒铜锌成矿带成矿条件和成矿预测[M]. 北京: 地质出版社. 330页.
[41]  [41]李荫清, 芮宗瑶, 程莱仙. 1981. 玉龙斑岩铜(钼)矿床的流体包裹体及成矿作用研究[J]. 地质学报, 55(3): 216~231.
[42]  [42]刘斌. 1982. 白银厂铜矿床石英中固体和流体包裹体的研究[J]. 地质学报, 56(2): 165~173.
[43]  [43]卢焕章, 施继锡, 喻茨玫. 1974. 华南某矿区成岩成矿温度的研究[J]. 地球化学, (3): 145~156.
[44]  [44]卢焕章. 1997. 成矿流体[M]. 北京: 北京科学技术出版社. 210.
[45]  [45]马鸿文. 1990. 西藏玉龙斑岩铜矿带花岗岩类与成矿[M]. 武汉: 中国地质大学出版社. 158页.
[46]  [46]马秀娟. 1988. 大吉山钨矿包裹体地球化学研究[A]. 见: 李荫清, 等主编. 流体包裹体在矿床学和岩石学中的应用[C]. 北京: 北京科学技术出版社. 64~112.
[47]  [47]毛景文, 李红艳, 裴荣富. 1995. 湖南千里山花岗岩的Nd-Sr同位素及岩石成因研究[J]. 矿床地质, 14(3): 233~242.
[48]  [48]芮宗瑶, 黄崇轲, 齐国明, 等. 1984. 中国斑岩铜(钼)矿床[M]. 北京: 地质出版社. 350页.
[49]  [49]芮宗瑶, 李宁, 王龙生. 1991. 关门山铅锌矿床: 盆地热卤水成矿及铅同位素打靶[M]. 北京: 地质出版社. 208页.
[50]  [50]芮宗瑶, 张洪涛, 王龙生, 等. 1995a. 吉黑东部斑岩型-浅成热液型铜金矿床多重成矿模型[J]. 矿床地质, 14(2): 174~184.
[51]  [51]芮宗瑶, 李荫清. 1995b. 矿物中包裹体研究[A]. 见: 唐仁鲤, 罗怀松, 等编. 西玉龙斑岩铜(钼)矿带地质[C]. 北京: 地质出版社. 213~241.
[52]  芮宗瑶, 刘玉琳, 王龙生, 等. 2002. 新疆东天山斑岩铜矿带及其大地构造格局[J]. 地质学报, 76(1): 83-94.
[53]  [53]芮宗瑶, 李荫清, 王龙生, 等. 2002. 初论成矿流体及金属矿物富集系统[J]. 矿床地质,21(1): 83~90.
[54]  [54]盛继福, 李亿斗, 勒贝尔, 等. 1985. 西华山钨矿流体包裹体及其成矿作用研究[J]. 中国地质科学院矿床地质研究所所刊, (2): 42~61.
[55]  [55]王鹤年, 张景华, 戴爱华, 等. 1989. 广东河台糜棱岩带蚀变岩型金矿床的地球化学研究[J]. 矿床地质, 8(2): 61~71.
[56]  [56]王秀璋, 程景平, 梁华英, 等. 1995. 变质细碎屑岩型金矿床的三阶段成矿模式[J]. 矿床地质, 14(4): 322~328.
[57]  [57]吴永乐, 梅勇文, 刘鹏程, 等. 1985. 西华山钨钼地质[M]. 北京: 地质出版社. 317.
[58]  [58]夏林圻, 夏祖春, 徐学义. 1996. 地幔橄榄岩捕虏体中的流体包裹体、岩浆包裹体和玻璃[A]. 见: 杜乐天, 等主编. 幔汁流体与软流层(体)地球化学[C]. 北京: 地质出版社. 230~271.
[59]  [59]夏林圻. 1980. 论我国西北地区阿尔卑斯型铬铁矿的成因[J]. 中国地质科学院西安地质矿产研究所分刊, 1(2): 25~39.
[60]  [60]谢奕汉, 赵瑞, 李若梅, 等. 1988. 银岩斑岩锡矿成矿物理化学条件及成矿物质来源[J]. 矿床地质, 7(3): 42~49.
[61]  [61]徐明基, 付德明, 尹裕民, 等. 1993. 四川呷村银多金属矿床[M]. 成都: 成都科学技术出版社. 164.
[62]  [62]薛春纪. 2000. 云南兰坪盆地第三纪成矿系列研究[D][博士后出站报告]. 导师: 陈毓川. 北京: 中国地质科学院.
[63]  [63]杨岳清, 倪云祥, 郭永泉, 等. 1987. 福建西坑花岗伟晶岩成岩成矿特征[J]. 矿床地质, 6(3): 10~21.
[64]  [64]尹汉辉, 范蔚茗, 林舸. 1990. 云南兰坪-思茅盆地演化的深部因素及幔-壳复合成矿作用[J]. 大地构造与成矿学, 14(2): 113~124.
[65]  [65]曾庆丰, 杨柏林. 1975. 南岭热液型钨矿(主要矿区)成矿温度及分析[J]. 地质科学, (2): 116~180.
[66]  [66]张文淮, 陈紫英. 1993. 流体包裹体地质学[M]. 武汉: 中国地质大学出版社. 246.
[67]  [67]赵一鸣, 林文蔚, 毕承思, 等. 1990. 中国夕卡岩矿床[M]. 北京: 地质出版社. 354.
[68]  [4]Hutehinson R W. 1973. Volcanogenic sulfide deposits and their metallogenic significance [J]. Econ. Geol., 68: 1223~1246.
[69]  [68]赵一鸣. 2002. 夕卡岩矿床研究的某些重要新进展[J]. 矿床地质, 21(2):113~120.
[70]  [69]邹天人, 张相宸, 贾富义, 等. 1986. 论阿尔泰3号伟晶岩脉的成因[J]. 矿床地质, 5(4): 34~48.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133