石英脉型钨矿“五层楼”模式的研究进展
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摘要
南岭是我国脉状钨矿最重要的集中区,也是"五层楼"找矿模式的发源地。文章介绍了"五层楼"找矿模式的由来,评述近年来"五层楼"模式研究新进展,总结了"五层楼"模式的几何结构,即横剖面呈树枝状分带,纵剖面呈扇形分带;建立了"五层楼+地下室"和"三层楼"等找矿新模式;发现岩体倾覆方向控制钨矿脉的侧伏方向;认为现有"五层楼"模式的基本参数缺乏矿床地球化学特征,建议深化对钨矿脉"五层楼"的水平分带及地球化学找矿标志的研究,"五层楼"模式的完善研究必将带来找矿的新突破。
Nanling is the most important concentrated area of vein type tungsten deposit in China, and also the birthplace of the "five-storeyed" prospecting model. First of all, the origin of "five-storeyed" prospecting model is introduced, its recent progress in research is commented, and the geometric structure is summarized. Its cross section is dendritic, and the longitudinal section is fan-shaped. Then the new prospecting models are proposed, such as "five-storeyed + basement" and "three-storeyed". It is found that the rock mass overturning direction controls the lateral direction of the tungsten vein. It is considered that the basic parameters of the existing "five-storeyed" pattern lack the geochemical characteristic of deposit. It is suggested to deepen the research on the horizontal zoning and geochemical prospecting indicators of "five-storeyed" in the tungsten vein. The perfection of the "five-storeyed" model will definitely bring new breakthroughs in prospecting.
Nanling is the most important concentrated area of vein type tungsten deposit in China, and also the birthplace of the "five-storeyed" prospecting model. First of all, the origin of "five-storeyed" prospecting model is introduced, its recent progress in research is commented, and the geometric structure is summarized. Its cross section is dendritic, and the longitudinal section is fan-shaped. Then the new prospecting models are proposed, such as "five-storeyed + basement" and "three-storeyed". It is found that the rock mass overturning direction controls the lateral direction of the tungsten vein. It is considered that the basic parameters of the existing "five-storeyed" pattern lack the geochemical characteristic of deposit. It is suggested to deepen the research on the horizontal zoning and geochemical prospecting indicators of "five-storeyed" in the tungsten vein. The perfection of the "five-storeyed" model will definitely bring new breakthroughs in prospecting.
引文
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[2]谭运金,苏亚汝.华南地区钨矿床地质找矿回顾与展望[J].中国钨业,2009,24(4):11-14.TAN Yunjin,SU Yaru.Review and prospect on tungsten deposit geological exploration in south China[J].China Tungsten Industry,2009,24(4):11-14.
[3]广东有色金属地质勘探公司九三二队.我们是怎样用五层楼规律寻找,评价和勘探黑钨石英脉矿床的[J].地质与勘探,1966,7(5):15-19.
[4]许建祥,曾载淋,王登红,等.赣南钨矿新类型及“五层楼+地下室”找矿模式[J].地质学报,2008,82(7):880-887.XU Jianxiang,ZENG Zailin,WANG Denghong,et al.A new type of tungsten deposit in southern Jiangxi and the new model of“five floor+basement”for prospecting[J].Acta Geologica Sinica,2008,82(7):880-887.
[5]李逸群,颜晓钟.中国南岭及邻区钨矿床矿物学[M].武汉:中国地质大学出版社,1991:1-50.
[6]胡受奚,周顺之,刘孝善,等.矿床学(上册)[M].北京:地质出版社,1982:206-208.
[7]桂林理工大学.广东石人嶂钨矿床总结研究报告[R].桂林:桂林理工大学,2012.
[8]韦龙明,林锦富,李文铅,等.广东梅子窝钨矿“五层楼”叠加现象探讨[J].地质学报,2008,82(7):888-894.WEI Longming,LIN Jinfu,LI Wenqian,et al.Discussion on“five stored”superposed model of Meiziwo tungsten deposit,Guangdong[J].Acta Geologica Sinica,2008,82(7):888-894.
[9]李中兰,梅勇文.赣南钨矿分布规律及隐伏矿床预测[J].江西地质,1999(4):276-282.LI Zhonglan,MEI Yongwen.The distribution regularity of tungsten deposits and the prognosis of concealed deposits in south Jiangxi[J].Jiangxi Geology,1999(4):276-282.
[10]夏宏远,梁书艺.南岭某些钨锡(钽铌)矿床的原生分带研究[J].矿物岩石(专辑),1986:1-164.
[11]王秋衡.中国钨矿床的成矿系列及其金属元素的带状分布[J].有色金属(矿山部分),1991(6):29-33.
[12]汪劲草,韦龙明,朱文凤,等.南岭钨矿“五层楼模式”的结构与构式-以粤北始兴县梅子窝钨矿为例[J].地质学报,2008,82(7):894-899.WANG Jincao,WEI Longming,ZHU Wenfeng,et al.Texture and tectonic style of“five-storeyed type”for the tungsten deposits in the Nanling mountains,southern China-an example from the Meiziwo tungsten deposit[J].Journal of Geology,2008,82(7):894-899.
[13]WEI Longming,ZHANG Guanghui,HUANG Chaozhu,et al.The prospecting and prediction in the deep and periphery of Shirenzhang tungsten deposit in Guangdong[J].Acta Geologica Sinica(English Edition),2013,87(supply1):798-799.
[14]王登红,唐菊兴,应立娟,等.“五层楼+地下室”找矿模型的适用性及其对深部找矿的意义[J].吉林大学学报(地球科学版),2010,40(4):733-738.WANG Denghong,TANG Juxing,YING Lijuan,et al.Application of“fivelevels+basement”model for prospecting deposits into depth[J].Journal of Jilin University(Earth Science Edition),2010,40(4):733-738.
[15]李建康,王登红,粱婷,等.南岭区域成矿与深部探测的研究进展及其对西藏钨锡找矿的指示[J].地球学报,2013,34(1):58-74.LI Jiankang,WANG Denghong,LIANG Ting,et al.Progress of research on metallogenic regularity and deep exploration in Nanling region and its indication for W-Sn exploration in Tibet[J].Acta Geoscientia Sinica,2013,34(1):58-74.
[16]覃日贤,韦龙明,张广辉,等.广东石人嶂钨矿床研究进展与建议[J].矿产与地质,2013,27(4):265-269.QIN Rixian,WEI Longming,ZHANG Guanghui,et al.Progress of research on Shirenzhang W deposit of Guangdong and some suggestions[J].Mineral Resources and Geology,2013,27(4):265-269.
[17]王莉,孔凡乾,韦龙明,等.石人嶂钨矿床云英岩型矿化及其研究意义[J].有色金属(矿山部分),2014,66(4):47-51,57.WANG Li,KONG Fanqian,WEI Longming,et al.Mineralization of greisen and its research significance in Shirenzhang tungsten deposit[J].Nonferrous Metals(Mine Section),2014,66(4):47-51,57.
[18]朱文凤,杨国高,韦龙明,等.广东石人嶂钨矿床银矿物特征[J].桂林工学院学报,2009,29(3):285-291.ZHU Wenfeng,YANG Guogao,WEI Longming,et al.Preliminary research about silver mineral in Shirenzhang tungsten deposit,Guangdong province[J].Journal of Guilin University of Technology,2009,29(3):285-291.
[19]张少琴,朱文凤,韦龙明.产铀花岗岩体中的晶质铀矿的若干特征-以粤北石人嶂钨矿为例[J].中国矿业,2009,18(11):104-106.ZHANG Shaoqin,ZHU Wenfeng,WEI Longming.Some characteristics of ulrichile in granite-the wolframite of Shirenzhang in north of Guangdong as an example[J].China Mining Magazing,2009,18(11):104-106.
[20]韦龙明,王莉,张广辉,等.广东石人嶂钨矿床中的晶质铀矿研究[J].地质学报,2014,88(4):805-813.WEI Longming,WANG Li,ZHANG Guanghui,et al.Study on the uraninite in Shirenzhang tungsten deposit,Guangdong province[J].Acta Geologica Sinica,2014,88(4):805-813.
[21]王潇潇,孔凡乾,韦龙明,等.粤北石人嶂钨矿放射性矿化研究[J].有色金属(矿山部分),2014,66(5):38-41,46.WANG Xiaoxiao,KONG Fanqian,WEI Longming,et al.Study on radioactive mineralization of Shirenzhang tungsten deposit in northern Guangdong[J].Nonferrous Metals(Mine Section),2014,66(5):38-41,46.
[22]田野,韦龙明,黄朝柱,等.广东石人嶂钨矿床存在多种矿化现象[J].地质论评,2013,59(增刊):357-358.
[23]李水如,王登红,梁婷,等.广西大明山钨矿区成矿时代及其找矿前景分析[J].地质学报,2008,82(7):873-879.LI Shuiru,WANG Denghong,LIANG Ting,et al.Metallogenic epochs of the damingshan tungsten deposit in Guangxi and its prospecting potential[J].Acta Geologica Sinica,2008,82(7):873-879.
[24]杨明桂,卢德揆.钨矿地质讨论会论文集[C].西华山-漂塘地区脉状钨矿的构造特征与排列组合形式,北京:地质出版社,1981:293-303.
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