石英脉型钨矿成矿研究进展
|
摘要
我国钨矿的储量、产量、消费量和出口量均处于全球领先地位,尤其是石英脉型钨矿床研究成果最为丰富。本文通过大量查阅国内外有关石英脉型钨矿的文献资料,对石英脉型钨矿的成矿研究成果和观点进行综合评述。石英脉型钨矿在我国各个成矿带均有分布,其空间分布和区域构造单元息息相关,所处的区域构造活动一般都很强烈,经历多次叠加构造运动。钨矿床产在震旦寒武系地层中,特别是在寒武系地层最多。成矿物质主要来源是岩浆热液,岩浆活动频繁为成矿热液的形成创造了必要的前提条件,但也有部分成矿物质源于围岩。石英脉型钨矿成矿模式以"五层楼+地下室"成矿模式最具影响力和实际意义,开创了模式找矿的先河。
The tungsten reserves,output,consumption and exports of China are listed at the front rank in the world and especially most of achievements in study of quartz vein type tungsten deposit are made in China.The research results and viewpoints about such type of tungsten deposit at home and abroad are comprehensively reviewed.The quartz vein type tungsten deposits are distributed in all metallogenic belts.The spatial distribution is closely related to regional tectonic unit.The tectonic activity in the area where the deposit occurs is generally strong and multiply superimposed.The deposit occurs mainly in strata of Sinian and Cambriam Systems,especially in the latter.The orematerials mainly come from magmatic hydrothermal fluid.The multiple stage magmatic activity is prerequisite of such deposit.However,there are some ore materials come from the surroung rock.The "five-story building+basement" model is the most influential and practical and pioneered in tungsten ore prospecting by model in the world.
The tungsten reserves,output,consumption and exports of China are listed at the front rank in the world and especially most of achievements in study of quartz vein type tungsten deposit are made in China.The research results and viewpoints about such type of tungsten deposit at home and abroad are comprehensively reviewed.The quartz vein type tungsten deposits are distributed in all metallogenic belts.The spatial distribution is closely related to regional tectonic unit.The tectonic activity in the area where the deposit occurs is generally strong and multiply superimposed.The deposit occurs mainly in strata of Sinian and Cambriam Systems,especially in the latter.The orematerials mainly come from magmatic hydrothermal fluid.The multiple stage magmatic activity is prerequisite of such deposit.However,there are some ore materials come from the surroung rock.The "five-story building+basement" model is the most influential and practical and pioneered in tungsten ore prospecting by model in the world.
引文
[1]柳志青.脉状钨矿床成矿预测理论[M].北京:科学出版社,1980.
[2]卢焕章.华南钨矿成因[M].重庆:重庆出版社,1986.
[3]冶金部南岭钨矿专题组.华南钨矿[M].北京:冶金工业出版社,1985.
[4]Kwak T A P,White A J R.Contrasting W-Mo-Cu and W-SnFskarn types and related Granitoids[J].Mining Geology,1982,32:339-351.
[5]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.Geologyof Granites and Their Metallogenie Relations.Beijing:Science Press,1984:87-101.
[6]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.
[7]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.
[8]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.
[9]夏宏远,梁书艺,谢为鑫,等.江西黄沙钨矿床的原生分带及其成因[C]∥钨矿地质讨论会论文集.北京:地质出版社,1984:221-230.
[10]徐克勤,胡受奚,孙明志,等.华南钨矿床区域成矿分析[C]∥钨矿地质讨论会论文集.北京:地质出版社,1984:245-249.
[11]陈郑辉,王登红,屈文俊,等.赣南崇义地区淘锡坑钨矿的地质特征与成矿时代[J].地质通报,2006,25(4):496-501.
[12]王燕,陈梦熊,李明高,等.广东瑶岭钨矿矿化类型多样性及成矿规律研究[J].矿产与地质,2006,20(8):334-339.
[13]郑平,徐海珍,黄满湘.湖南衡南杨林坳钨矿床成因与矿模式研究[J].矿产与地质,2007,21(2):126-130.
[14]刘梦庚.中国南方脉型钨矿床的一些特征与成矿模式[C]∥钨矿地质讨论会论文集,北京:地质出版社,1984:93-103.
[15]许泰,李振华.西华山钨矿床流体包裹体特征及成矿流体来源[J].资源调查与环境,2013,34(2):95-101.
[16]许泰,高海东,李元志,等.中国钨矿床成矿特征探讨[J].中国钨业,2012,27(3):1-5.
[17]刘志萍,徐勇.浒坑钨矿大脉区矿脉赋存规律及深部探矿方向[J].中国钨业,2004,19(6):30-33.
[18]张作衡,毛景文,杨建民,等.北祁连加里东造山带塔儿沟矽卡岩-石英脉型钨矿床地质及成因[J].矿床地质,2002,21(2):200-211.
[19]刘堆富,陈玉峰.甘肃小柳沟钨矿床矿石特征[J].地质与勘探,2005,41(5):10-16.
[20]刘堆富,陈玉峰.甘肃小柳沟钨矿床石英脉特征及其含矿性评价[J].地质找矿论丛,2005,20(3):182-187.
[21]陈依壤.瑶岗仙脉钨矿床地质特征与找矿标志[J].地质与勘探,1981(2):25-30.
[22]林新多,张德会,章传玲.湖南宜章瑶岗仙黑钨矿石英脉成矿流体性质的探讨[J].地球科学(武汉地质学院学报),1986,11(2):153-160.
[23]吴永乐,梅勇文,刘鹏程,等.西华山钨矿地质[M].北京:地质出版社,1987.
[24]周宏.甘肃省小柳沟钨矿区成矿流体特征[J].地质找矿论丛,2004.19(2):110-113.
[25]周宏,林森,司雪峰.甘肃小柳沟钨矿床微量元素地球化学特征[J].桂林工学院学报,2004,24(3):243-247.
[26]许泰,王勇.赣南西华山钨矿床硫、铅同位素组成对成矿物质来源的示踪[J].矿物岩石地球化学通报,2014,33(3):342-347.
[27]马春,王素娟.江苏镇江谏壁岩体特征与钼(钨)矿床类型[J].江苏地质,2003,27(3):152-158.
[28]朱祥培,张永忠,徐九发.江西崇义塘漂孜岩体型钨矿床地质特征及其找矿意义[J].资源调查与环境,2006,27(2):450-456.
[29]胡朋,聂凤军,赫英,等.内蒙古沙麦钨矿床地质及流体包裹体研究[J].矿床地质,2005,24(6):603-612.
[30]顾雪祥,刘建明,Oskar Schulz,等.湖南沃溪金-锑-钨矿床成因的稀土元素地球化学证据[J].地球化学,2005,34(5):428-442.
[31]康永孚,苗树屏,李崇佑,等.中国钨矿床[M].北京:地质出版社,1994.
[32]古菊云.华南钨矿脉的形态分类[M].北京:地质出版社,1981.
[33]陈依壤.瑶岗仙花岗岩地质地球化学特征与成岩成矿作用[J].矿产与地质,1988(1):62-72.
[34]杨明桂.论成矿预测中的控矿构造型式研究[J].江西地质,1989,3(3):256-274.
[35]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.
[36]曾载淋,田幽军.赣南地区钨矿找矿史回顾及新一轮钨矿找矿思考[J].资源调查与环境,2006,27(2):94-102.
[37]周济元,肖惠良.成矿结构体系及其钨矿找矿意义[J].资源调查与环境,2006,27(2):110-119.
[38]许建祥,曾载淋,王登红,等.赣南钨矿新类型及“五层搂+地下室”找矿模型[J].地质学报,2008,82(7):880-887.
[39]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.
[2]卢焕章.华南钨矿成因[M].重庆:重庆出版社,1986.
[3]冶金部南岭钨矿专题组.华南钨矿[M].北京:冶金工业出版社,1985.
[4]Kwak T A P,White A J R.Contrasting W-Mo-Cu and W-SnFskarn types and related Granitoids[J].Mining Geology,1982,32:339-351.
[5]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.Geologyof Granites and Their Metallogenie Relations.Beijing:Science Press,1984:87-101.
[6]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.
[7]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.
[8]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.
[9]夏宏远,梁书艺,谢为鑫,等.江西黄沙钨矿床的原生分带及其成因[C]∥钨矿地质讨论会论文集.北京:地质出版社,1984:221-230.
[10]徐克勤,胡受奚,孙明志,等.华南钨矿床区域成矿分析[C]∥钨矿地质讨论会论文集.北京:地质出版社,1984:245-249.
[11]陈郑辉,王登红,屈文俊,等.赣南崇义地区淘锡坑钨矿的地质特征与成矿时代[J].地质通报,2006,25(4):496-501.
[12]王燕,陈梦熊,李明高,等.广东瑶岭钨矿矿化类型多样性及成矿规律研究[J].矿产与地质,2006,20(8):334-339.
[13]郑平,徐海珍,黄满湘.湖南衡南杨林坳钨矿床成因与矿模式研究[J].矿产与地质,2007,21(2):126-130.
[14]刘梦庚.中国南方脉型钨矿床的一些特征与成矿模式[C]∥钨矿地质讨论会论文集,北京:地质出版社,1984:93-103.
[15]许泰,李振华.西华山钨矿床流体包裹体特征及成矿流体来源[J].资源调查与环境,2013,34(2):95-101.
[16]许泰,高海东,李元志,等.中国钨矿床成矿特征探讨[J].中国钨业,2012,27(3):1-5.
[17]刘志萍,徐勇.浒坑钨矿大脉区矿脉赋存规律及深部探矿方向[J].中国钨业,2004,19(6):30-33.
[18]张作衡,毛景文,杨建民,等.北祁连加里东造山带塔儿沟矽卡岩-石英脉型钨矿床地质及成因[J].矿床地质,2002,21(2):200-211.
[19]刘堆富,陈玉峰.甘肃小柳沟钨矿床矿石特征[J].地质与勘探,2005,41(5):10-16.
[20]刘堆富,陈玉峰.甘肃小柳沟钨矿床石英脉特征及其含矿性评价[J].地质找矿论丛,2005,20(3):182-187.
[21]陈依壤.瑶岗仙脉钨矿床地质特征与找矿标志[J].地质与勘探,1981(2):25-30.
[22]林新多,张德会,章传玲.湖南宜章瑶岗仙黑钨矿石英脉成矿流体性质的探讨[J].地球科学(武汉地质学院学报),1986,11(2):153-160.
[23]吴永乐,梅勇文,刘鹏程,等.西华山钨矿地质[M].北京:地质出版社,1987.
[24]周宏.甘肃省小柳沟钨矿区成矿流体特征[J].地质找矿论丛,2004.19(2):110-113.
[25]周宏,林森,司雪峰.甘肃小柳沟钨矿床微量元素地球化学特征[J].桂林工学院学报,2004,24(3):243-247.
[26]许泰,王勇.赣南西华山钨矿床硫、铅同位素组成对成矿物质来源的示踪[J].矿物岩石地球化学通报,2014,33(3):342-347.
[27]马春,王素娟.江苏镇江谏壁岩体特征与钼(钨)矿床类型[J].江苏地质,2003,27(3):152-158.
[28]朱祥培,张永忠,徐九发.江西崇义塘漂孜岩体型钨矿床地质特征及其找矿意义[J].资源调查与环境,2006,27(2):450-456.
[29]胡朋,聂凤军,赫英,等.内蒙古沙麦钨矿床地质及流体包裹体研究[J].矿床地质,2005,24(6):603-612.
[30]顾雪祥,刘建明,Oskar Schulz,等.湖南沃溪金-锑-钨矿床成因的稀土元素地球化学证据[J].地球化学,2005,34(5):428-442.
[31]康永孚,苗树屏,李崇佑,等.中国钨矿床[M].北京:地质出版社,1994.
[32]古菊云.华南钨矿脉的形态分类[M].北京:地质出版社,1981.
[33]陈依壤.瑶岗仙花岗岩地质地球化学特征与成岩成矿作用[J].矿产与地质,1988(1):62-72.
[34]杨明桂.论成矿预测中的控矿构造型式研究[J].江西地质,1989,3(3):256-274.
[35]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.
[36]曾载淋,田幽军.赣南地区钨矿找矿史回顾及新一轮钨矿找矿思考[J].资源调查与环境,2006,27(2):94-102.
[37]周济元,肖惠良.成矿结构体系及其钨矿找矿意义[J].资源调查与环境,2006,27(2):110-119.
[38]许建祥,曾载淋,王登红,等.赣南钨矿新类型及“五层搂+地下室”找矿模型[J].地质学报,2008,82(7):880-887.
[39]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.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |