矽卡岩型白钨矿矿床研究进展

Abstract
Figure/Table
References
Related Citation (15)

Download: PDF (11820 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Skarn-type scheelite deposit is widespread and has the greatest economic value, occupies an important place among all tungsten deposits in the world, and accounts for half of the total tungten reserves in the world In China, skarn-type scheelite makes up at least 60％ of the total tungsten reserves. Therefore, study of skarn-type scheelite deposit is of great economic and strategic importance. In previous studies, some researchers have done a lot of works on skarn-type scheelite deposit and obtained a series of achievements. In this paper, on the basis of previous data, the spatial and temporal distribution, the geological and metallogenic characteristics, the ore-forming fluid and source, the metallogenic mechanism and comparison of typical deposits in domestic and abroad are discussed, and an overview of the current state in study of the skarn-type scheelite deposit is presented.

Key words： skarn-type scheelite deposit spatial and temporal distribution geological characteristics ore-forming fluid metallogenic material research progress

Received: 29 September 2014

P618.67

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	ZHAO Xin-min
	GUO Zhou-ping
	BAI Yun

Cite this article:

ZHAO Xin-min,GUO Zhou-ping,BAI Yun. Advances in Study of Skarn-type Scheelite Deposit[J]. , 2015, 2(1): 9-13.

URL:

http://114.242.223.217/EN/ OR http://114.242.223.217/EN/Y2015/V2/I1/9

[1] 徐克勤, 程海. 中国钨矿形成的大地构造背景[J]. 地质找矿论丛, 1987, 2(2): 1-7.
[2] Meinert L D. Skarns and skarn deposits[J]. Geoscience Canada, 1992, 19(4): 145-162.
[3] 石洪召, 林方成, 张林奎. 钨矿床的时空分布及研究现状[J]. 沉积与特提斯地质, 2009, 29(4): 90-95.
[4] 毕承思. 中国矽卡岩型白钨矿矿床成矿基本地质特征[J]. 中国地质科学院院报, 1987, 17: 49-64.
[5] 康永孚, 李崇佑. 中国钨矿床地质特征、类型及其分布[J]. 矿床地质, 1991, 10(1): 1-22.
[6] 康永孚, 苗树屏, 李崇佑, 等. 中国钨矿床[M]//宋叔和.中国矿床. 北京: 地质出版社, 1994: 1-102.
[7] Einaudi M T, Meinert L D, Newberry R J. Skarn deposits[J]. Economic Geology,1981,75:317-391.
[8] Kwak T A P. W-Sn Skarn Deposits and Related Metamorphic Skarns and Granitoids[M].Amsterdam:Elsevier, 1987: 1-451.
[9] Solomon M. An introduction to the geology and metallic ore deposits of Tasmania[J]. Economic Geology,1981,76:194-206.
[10]Kwak T A P,White A J R.Contrasting W-Mo-Cu and W-Sn-F skarn types and related Granitoids[J]. Mining Geology, 1982, 32:339-351.
[11]Chappell B W,White A J R.I-and S-type granites in the Lachlan fold belt,southeastern in Australia[M]//Xu K Q,Tu G.Geology of Granites and Their Metallogenie Relations.Beijing: Science Press, 1984: 87-101.
[12]Blevin P L,Chappell B W.Chemistry,origin and evolution of mineralized granites in the Lachlan Fold Belt,Australia:The metallogeny of I-and S-type granites[J]. Economic Geology, 1995, 90: 1604-1619.
[13]Zaw K, Singoyi B. Formation of magnetite-scheelite skarn mineralization at Kara, Northwestern Tasmani: Evidence from mineral chemistry and stable isotopes[J]. Economic Geology,2000,95:1215-1230.
[14]Mao J W, Zhang Z Z, Lehmann B,et al. The Yeniutan granodiorite in Subei County, Gansu Province, China: Petrological features, geological setting and relationship to tungsten mineralization[J]. Episodes, 2000, 23(3): 163-171.
[15]徐克勤, 胡受奚, 孙明志, 等. 华南两个成因系列花岗岩及其成矿特征[J]. 矿床地质, 1982,1(2): 1-14.
[16]刘希禹,司徒铺.白钨矿床及其含矿溶液和岩体成因探讨[J]. 地质与勘探, 1985, 30(11): 18-23.
[17]顾连兴, 杨浩, 郑素娟, 等. 钨和锡——华南型块状硫化物矿床的特征元素[J]. 地质论评, 1990, 36 (4): 298-304.
[18]毛景文, 宋叔和. 桂北地区火成岩系列和锡多金属矿床成矿系列[M]. 北京: 科学技术出版社, 1998: 116-125.
[19]毛景文, 张作衡, 党泽发. 钨矿床研究态势[J]. 矿床地质, 1998, 17(增刊): 5-10.
[20]裴荣富, 熊群尧. 中国特大型金属矿床成矿偏在性与成矿构造聚敛(场) [J]. 矿床地质, 1999, 18(1): 37-46.
[21]毛景文. 超大型钨多金属矿床成矿特殊性——以湖南柿竹园矿床为例[J]. 地质科学, 1997, 32(3): 351-363.
[22]Lu H Z, Liu Y M, Wang C L, et al. Mineralization and fluid inclusion study of the Shizhuyuan W-Sn-Bi-Mo-F skarn deposit, Hunan Province, China[J]. Economic Geology, 2003, 98: 955-974.
[23]吴胜华, 王旭东, 熊必康. 江西香炉山矽卡岩型钨矿床流体包裹体研究[J]. 岩石学报, 2014, 30(1): 78-88.
[24]徐克勤. 湘南钨铁锰矿矿区中矽嘎岩型钙钨矿的发现,并论两类矿床在成因上的关系[J]. 地质学报, 1957, 37(2): 117-151.
[25]康永孚.钨的地球化学与矿床类型[J].地质地球化学, 1981,9(1): 1-6.
[26]祝新友, 王艳丽, 王京彬, 等. 南岭地区石英脉型黑钨矿与矽卡岩型白钨矿矿床成因关系探讨[J]. 矿床地质, 2010,29(增刊):367-369.
[27]刘英俊, 马东升. 钨的地球化学[M].北京:科学出版社, 1987:1-232.
[28]Landis G P,Rye R O.Geologic,fluid inclusion and stable isotope studies of the Pasto Bueno tungsten base metal deposit, Northern Peru[J]. Economic Geology, 1974, 69: 1025-1059.
[29]Higgins N C. Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions[J]. Canadian Journal of Earth Science, 1980, 17(7): 823-830.
[30]Ramboz C, Schnapper D, Dubessy J. The P-V-T-X-fO₂ evolution of H₂O-CO₂ -CH₄-bearing fluids in a wolframite vein:Reconstruction from fliud inclusion studies[J]. Geochim Cosmochim Acta, 1985, 49: 205-219.
[31]徐克勤, 孙鼐, 王德滋, 等. 华南多旋回的花岗岩类的侵入时代、岩性特征、分布规律及其成矿属性的探讨[J]. 地质学报, 1963, 43(2):141-155.
[32]徐克勤, 朱金初, 徐士进, 等. 华南含钨、锡、铌(钽)花岗岩及有关矿床产出的地质环境和地球化学差异[J]. 南京大学学报(地球科学版), 1989,1(1): 1-16.
[33]南京大学地质系. 华南不同时代花岗岩及其成矿关系[M]. 北京: 科学出版社, 1981:1-472.
[34]王联魁, 朱为方, 张绍立. 华南花岗岩两个成岩成矿系列的演化[J]. 地球化学, 1982, 11(4): 329-339.
[35]陈毓川, 裴荣富, 张宏良, 等. 南岭地区与中生代花岗岩类有关的有色及稀有金属矿床[M]. 北京: 地质出版社, 1989: 1-316.
[36]刘家远. 西华山钨矿的花岗岩组成及与成矿的关系[J]. 地质找矿论丛, 2005, 20(1): 1-7.
[37]华仁民, 陈培荣, 张文兰, 等. 南岭与中生代花岗岩类有关的成矿作用及其大地构造背景[J]. 高校地质学报, 2005, 11(3): 291-304.
[38]徐克勤, 孙鼐, 王德滋, 等. 华南花岗岩与成矿[M]//徐克勤. 花岗岩地质和成矿关系. 南京: 江苏科学技术出版社, 1984: 1-20.
[39]翟裕生. 中国区域成矿特征探讨[J]. 地质与勘探, 2002, 38(5): 1-4.
[40]刘英俊. 论钨的成矿地球化学[J]. 地质与勘探, 1982, 28(1): 15-23.
[41]包正相. 层控白钨矿床新层位及其地质特征[J]. 地质论评, 1984, 30(6): 595-599.
[42]毛景文, 张招崇, 杨建民, 等. 北祁连山西段铜金铁钨多金属矿床成矿系列和找矿评价[M]. 北京: 地质出版社, 2003: 1-437.
[43]赵一鸣, 林文蔚, 毕承思. 中国矽卡岩矿床[M]. 北京: 地质出版社, 2012: 1-272.