四川省宁南县银厂沟—骑骡沟地区铅锌矿成矿规律与成矿预测
|
摘要
本文以四川省宁南县银厂沟-骑骡沟地区铅锌矿为研究对象,通过对区域成矿地质背景、构造控矿、地层岩性组合控矿、矿体赋存、稳定同位素、稀土元素、微量元素等进行研究,厘定它们之间的耦合关系,总结银厂沟矿段铅锌矿的成矿规律,建立找矿标志及找矿模型。然后,借助于银厂沟矿段的成矿规律和找矿模型,综合其它矿段的地、化、遥等资料,圈定与银厂沟矿段成矿规律相似的地段(靶区)。最后,概算其余矿段圈定靶区的远景资源量。
宁南处于扬子板块南部早古生代被动陆缘上近SN向的昆明-昭觉陆架裂陷带的北段,会理-东川拗拉槽北界的天宝山-巧家断裂带附近。银厂沟-骑骡沟地区位于骑骡沟复式背斜西翼,且紧靠背斜轴部。背斜为一区域性背斜,走向近南北,向南倾伏,轴部为元古界会理群通安组地层,两翼由震旦系、寒武系、奥陶系等地层组成。该区出露的主要地层为震旦系和寒武系,次为前震旦系地层及第四系。银厂沟-骑骡沟地区含矿层为震旦系上统灯影组上段(Zbd3),产状215°~245°∠23°~38°,岩性为内碎屑白云岩,由强热液白云石化、密集条带状似碧玉岩化白云岩等组成。区内,未见岩浆岩出露。
矿石矿物有方铅矿、闪锌矿、黝铜矿、黄铁矿、白铅矿、菱锌矿、车轮矿灯。围岩蚀变主要有硅化、白云石化等。
银厂沟-骑骡沟地区,主要控矿因素:①地层岩性控矿,由寒武系下统筇竹寺组(?1q)、震旦系上统灯影组(zbd)和观音组(zbg)构成了地球化学梯度变化带,形成良好的储矿系统。②构造及构造组合控矿,顺层剪切构造、张裂断裂、“入”型构造、断裂与横、纵小背斜或小挠曲的交汇处,为主要的容矿部位。③构造演化控制成矿过程具多期多阶段特征。
通过稳定同位素、稀土元素和微量元素分析,研究区成矿物质与成矿流体具有壳-幔混源特征。均一温度122℃~236℃,属中-低温。矿床类型为具有壳-幔混源特征的浅成中-低温热液铅锌矿床。
研究区内共圈定18个横向褶皱,和1个由18条剖面构成的纵向褶皱。由横向褶皱和纵向褶皱组合构成的区域为A类远景区,由横向褶皱或纵向褶皱构成的区域为B类远景区。然后,由体积成矿系数法,概算的A类远景区和B类远景区的远景资源量,概算结果分别为13万t、94万t。
Based on the NingNa county of sichuan s Yin Changgou-Qi Luogou as the research object, by regional metallogenic geological background of ore-controlling structure, and lithological association ore-controlling cretaceous. the ore, stable isotopes and trace elements and rare earth elements, etc, they studied the coupling relationship between the silver, and summarizes the lead-zinc deposit metallogenic regularities, establishing ore-prospecting criteria and prospecting model. Then, with the silver of metallogenic regularities of ore prospecting model, and the comprehensive other land, and remote data with Yin Changgou-Qi Luogou, the section of metallogenic regularities of similar area (target). Finally, estimate the rest of ore resource delineating the vision.
Building in southern Yangtze plate passive continental margin on the early Paleozoic to kunming - nearly SN ZhaoJiao oil-bearing rifting, listens to the north - with depression and the slot dongchuan the days near baoshan - qiaojia fault. The Yin Changgou-Qi Luogou area located on the Qi Luogou ditch west wing, double anticline axis and abuts anticline. As a regional anticline anticline in the near east, west, north and south, to tilt toward the south, the axis of the 0.932 for general Ann formation, two-wing by sinian, Cambrian, yingshan formation, etc. The formation of mainly for sinian and Cambrian, times before the formation and 4 sinian system for.
The area - the ore-bearing layer is lighted on the sinian section (ec) group, in Zbd3 215°~ 245°∠23°~38°, lithology, clastic dolostone is by hydrothermal dolomitization, dense the ribbon like jasper paleokarstification dolostone, etc. Zone, not seen.
There ore mineral sphalerite and galena, tetrahedrite, pyrite, white lead, zinc mine, wheel miner's. Wall-rock alteration are mainly dolomitization, etc.
The Yin Changgou-Qi Luogou area, the main ore-control factors: (1) the lithological ore-controlling, from the Cambrian next series field (?1q )group (ec), the sinian 1q (zbd) and light group avalokitesvara (zbg) constitutes the geochemical gradient belts, forming good store ore systerms. (2) structure and structural combination, ore-controlling structures, strong shear fault, "into" type structure, fracture and horizontal, vertical, or small buckling of small anticline, as the main part of the ore. (3) metallogenic tectonic evolution and controlling process with many characters.
Through the stable isotopes and trace elements and rare earth elements, study area of ore-forming materials and ore-forming fluid has shell - mixed characteristics. 122°~ 236°uniform temperature, temperature - c. The copper deposit types for shell - mixed with the characteristics of low - the hypabyssal hydrothermal pb-zn deposit.
Research areas delineated total 18 lateral fold, and 1 by 18 sections of the longitudinal fold. By transverse and longitudinal fold drape of A vision for the region, by lateral fold or longitudinal fold constitute the area for class B vision zone. Then, the volume of metallogenic coefficient method, A kind of vision estimates and class B vision result, the vision of resource estimates 1.3 million ton, 9.4 million ton, respectively.
宁南处于扬子板块南部早古生代被动陆缘上近SN向的昆明-昭觉陆架裂陷带的北段,会理-东川拗拉槽北界的天宝山-巧家断裂带附近。银厂沟-骑骡沟地区位于骑骡沟复式背斜西翼,且紧靠背斜轴部。背斜为一区域性背斜,走向近南北,向南倾伏,轴部为元古界会理群通安组地层,两翼由震旦系、寒武系、奥陶系等地层组成。该区出露的主要地层为震旦系和寒武系,次为前震旦系地层及第四系。银厂沟-骑骡沟地区含矿层为震旦系上统灯影组上段(Zbd3),产状215°~245°∠23°~38°,岩性为内碎屑白云岩,由强热液白云石化、密集条带状似碧玉岩化白云岩等组成。区内,未见岩浆岩出露。
矿石矿物有方铅矿、闪锌矿、黝铜矿、黄铁矿、白铅矿、菱锌矿、车轮矿灯。围岩蚀变主要有硅化、白云石化等。
银厂沟-骑骡沟地区,主要控矿因素:①地层岩性控矿,由寒武系下统筇竹寺组(?1q)、震旦系上统灯影组(zbd)和观音组(zbg)构成了地球化学梯度变化带,形成良好的储矿系统。②构造及构造组合控矿,顺层剪切构造、张裂断裂、“入”型构造、断裂与横、纵小背斜或小挠曲的交汇处,为主要的容矿部位。③构造演化控制成矿过程具多期多阶段特征。
通过稳定同位素、稀土元素和微量元素分析,研究区成矿物质与成矿流体具有壳-幔混源特征。均一温度122℃~236℃,属中-低温。矿床类型为具有壳-幔混源特征的浅成中-低温热液铅锌矿床。
研究区内共圈定18个横向褶皱,和1个由18条剖面构成的纵向褶皱。由横向褶皱和纵向褶皱组合构成的区域为A类远景区,由横向褶皱或纵向褶皱构成的区域为B类远景区。然后,由体积成矿系数法,概算的A类远景区和B类远景区的远景资源量,概算结果分别为13万t、94万t。
Based on the NingNa county of sichuan s Yin Changgou-Qi Luogou as the research object, by regional metallogenic geological background of ore-controlling structure, and lithological association ore-controlling cretaceous. the ore, stable isotopes and trace elements and rare earth elements, etc, they studied the coupling relationship between the silver, and summarizes the lead-zinc deposit metallogenic regularities, establishing ore-prospecting criteria and prospecting model. Then, with the silver of metallogenic regularities of ore prospecting model, and the comprehensive other land, and remote data with Yin Changgou-Qi Luogou, the section of metallogenic regularities of similar area (target). Finally, estimate the rest of ore resource delineating the vision.
Building in southern Yangtze plate passive continental margin on the early Paleozoic to kunming - nearly SN ZhaoJiao oil-bearing rifting, listens to the north - with depression and the slot dongchuan the days near baoshan - qiaojia fault. The Yin Changgou-Qi Luogou area located on the Qi Luogou ditch west wing, double anticline axis and abuts anticline. As a regional anticline anticline in the near east, west, north and south, to tilt toward the south, the axis of the 0.932 for general Ann formation, two-wing by sinian, Cambrian, yingshan formation, etc. The formation of mainly for sinian and Cambrian, times before the formation and 4 sinian system for.
The area - the ore-bearing layer is lighted on the sinian section (ec) group, in Zbd3 215°~ 245°∠23°~38°, lithology, clastic dolostone is by hydrothermal dolomitization, dense the ribbon like jasper paleokarstification dolostone, etc. Zone, not seen.
There ore mineral sphalerite and galena, tetrahedrite, pyrite, white lead, zinc mine, wheel miner's. Wall-rock alteration are mainly dolomitization, etc.
The Yin Changgou-Qi Luogou area, the main ore-control factors: (1) the lithological ore-controlling, from the Cambrian next series field (?1q )group (ec), the sinian 1q (zbd) and light group avalokitesvara (zbg) constitutes the geochemical gradient belts, forming good store ore systerms. (2) structure and structural combination, ore-controlling structures, strong shear fault, "into" type structure, fracture and horizontal, vertical, or small buckling of small anticline, as the main part of the ore. (3) metallogenic tectonic evolution and controlling process with many characters.
Through the stable isotopes and trace elements and rare earth elements, study area of ore-forming materials and ore-forming fluid has shell - mixed characteristics. 122°~ 236°uniform temperature, temperature - c. The copper deposit types for shell - mixed with the characteristics of low - the hypabyssal hydrothermal pb-zn deposit.
Research areas delineated total 18 lateral fold, and 1 by 18 sections of the longitudinal fold. By transverse and longitudinal fold drape of A vision for the region, by lateral fold or longitudinal fold constitute the area for class B vision zone. Then, the volume of metallogenic coefficient method, A kind of vision estimates and class B vision result, the vision of resource estimates 1.3 million ton, 9.4 million ton, respectively.
引文
[1]蒋其胜,赵自宏,黄建满.安徽南陵姚家岭铜铅锌矿床的发现及意义[J].中国地质. 2008-35-2:314-321.
[2]刘友勋,刘亚新,曾钦旺,黄革非,李建中.郴州西山地区银铅锌矿床地质特征及找矿方向[J].湖南地质.2002-21-4:282-285.
[3]刘家铎,张成江,刘显凡等.川滇黔相邻区域铜铅锌金银矿床与峨眉火成岩省的关系探讨[J].矿物岩石. 2003(12):74-79.
[4]周云满.滇东北乐红铅锌矿床地质特征及找矿远景[J].地质地球化学.2003年第31卷第4期:16-21.
[5]薛传东,韩润生,杨海林,杨志明等.滇西北保山核桃坪铅锌矿床成矿流体来源的同位素地球化学证据[J].矿床地质.2008-27-2:243-252.
[6]陈学明,邓军,沈崇辉,兰景志.凡口超大型铅锌矿床成矿流体的物理特征和地球化学特征[J]地球科学-中国地质大学学报.2000-25-4:438-442.
[7].雷良奇,宋慈安,冯佐海.佛子冲火山岩区隐伏铅锌矿床的类型归属及成矿远景[J].地质与勘探.2002-38-1:9-14.
[8]刘华东.福建黄地铅锌矿地质特征及成因探讨[J] .江西有色金属.2008-22-1:11-15.
[9]林仟同.福建建瓯八外洋铅锌矿床地质特征及其成因分析[J].福建地质第四期:178-185.
[10]陈火炮,李敬珠.福建顺昌山后铅锌矿床地质特征及成因探讨[J] .福建地质.第二期:204-210.
[11]祝新友,汪东波,卫冶国,邱小平,王瑞廷.甘肃代家庄铅锌矿的地质特征与找矿意义[J].地球学报.2006-27-7:595-602.
[12]刘伟,罗学红,王立波.关陵根铅锌矿矿床地质特征及成因探讨[J].甘肃地质.2008-17-1:47-53.
[13]张少萍.广东省连平县大尖山铅锌矿床成因及围岩含矿性[J] .科技资讯.2007-24:27-28.
[14]高凤颖.广东省紫金县苏石坑铅锌矿地质特征及成因[J].科技资讯导报. (2007)07(c)-0072-02:72-73.
[15]毛党龙.湖南保靖县且溪科铅锌矿地质特征[J] .化工矿产地质.2008-30-3:143-162.
[16]伍磊.广西贵港-平南地区铅锌矿带地质特征及找矿方向[J].矿产与地质.2001-15-5:329-334.
[17]郑星辉,周春玲,李建强,蓝元利.桂平市锡基坑铅锌矿床地质特征及外围找矿潜力分析[J].南方国土资源.2008-9:40-42.
[6]王长明,张寿庭,邓军,孙艳霞等.河南冷水北沟铅锌矿地质地球化学特征及成因探讨[J].矿床地质. 2007-26-2:175-183.
[18]王长明,邓军,张寿庭.燕长海.河南省卢氏栾川地区铅锌矿成矿多样性分析及成矿预测[J].地质通报.24 (10211) :1074~1080.
[19]常雪生.新疆西昆仑地区铅锌矿成矿特征与找矿前景.新疆有色金属.2003:2~8.
[20]李祥能.湖南后江桥铅锌矿地质特征及矿床成因[J] .地质找矿论丛. 2002-17-1:41-46.
[21]杨长明,李诚.湖南黄沙寺铜2铅2锌矿床控矿因素浅析[J] .矿产与地质. 2006-20-6:632-634.
[22]黄满相.湖南桥口铅锌矿床成矿流体特征[J] .湖北地矿.2004-18-2:14-18.
[23]张庆华.湖南水口山铅锌矿田地质特征及找矿思路[J].有色金属矿产与勘查.1999-8-3:141-146.
[24]段士刚,薛春纪,燕长海,刘国印,宋要武,张德会.华北陆块南、北缘铅锌矿床成矿特征对比[J].矿床地质.2008-07-3:383-393.
[25]刘崇民,马生明,胡树起等.火山热液型铅锌矿床岩石地球化学特征及预测指标[J].物探与化探.2008-32-2:154-158.
[26]杨斌,彭省临,杨牧,林德松,何国朝.江西银山铜铅锌矿床热液对流与蚀变矿化分带机制[J].桂林工学院学报.2004-04-4:395-401.
[27]彭晓明.将乐八里桥铅锌多金属矿地质特征及成因初探[J].资源与产业.2008-10-6:119-124.
[28]王京彬,姜俊康.吉昌可可塔勒矿带铅锌矿床找矿评价方法[J].新疆地质.2001-19-1:64-69.
[29]刘凤鸣.库尔尕生铅锌矿床地质特征及成因浅析[J] .新疆有色金属.第三期:4-6.
[30]王新利,庞艳春.澜沧老厂银铜铅锌多金属矿床地质特征及成因探讨[J].地质与资源.2006-15-3:200-221.
[31]王艳.辽宁本溪盘岭地区铜、铅锌矿床成矿条件探讨[J] .辽宁地质.2001-18-1:28-42.
[32]李南生.闽清牛路坑铅锌矿床地质特征与成因初探[J].福建地质第一期:22-38.
[33]狄永军,吴淦国,张达等.闽中地区铅锌矿床辉石成分特征及其成因意义[J].矿床地质. 2006-25-2:123-134.
[34]张生辉,石建基,狄永军,余心起等.闽中裂谷块状硫化物型铅锌矿床的地质特征及找矿意义[J] .现代地质.2005-19-3:375-384.
[35]李振祥,谢振玉,刘召,李淑果.内蒙古西乌珠穆沁旗花敖包特银铅锌矿矿床地质特征及成因初探[J].地质与资源.2008-17-4:278-281.
[36]方如恒.中朝古元古代层控铅锌矿床类型及其比较[J].辽宁地质.1999-16-1:43-56
[37]徐发,王永军,刘国庆.内蒙古扎鲁特旗香山铜铅锌矿区成矿地质条件分析及找矿潜力[J].矿产与地质.2004-102-2:148-151.
[38]陈国勇.黔南台陷碳酸盐型铅锌矿床成矿条件及找矿模型[J].贵州地质.2002-19-1:20-26.
[39]贾润幸,郭健等.秦岭凤太成矿区多金属矿床成矿流体地球化学特征[J].中国地质.2004-31-2:192-198.
[40]孙文涛,孙吉国,孙红云,谢常君.青城子矿田杨树区超大型金银铅锌矿床地质特征及成矿机理[J].地质与勘探.2008-44-4:24-30.
[41]侯满堂,王党国,高杰,高怀雄.陕西马元地区铅锌矿矿石特征研究[J].陕西地质.2007-25-1:1-37.
[42]朱华平,张德全.陕西南秦岭志留系中铅锌矿床地质地球化学特征研究[J].地质找矿论丛2004-19-2:76-86.
[43]齐文.陕西商州龙庙铅锌矿床特征及成因探讨[J].陕西地质.2002-20-1:28-38.
[44]何显刚,李淑慧,谢恩顺.四川巴塘砂西银铅锌矿床特征与找矿远景[J].四川地质学报.2004-24-2:77-81.
[45]旦贵兵,杨大宏,沈史日.四川宁南雀珠山地区铅锌矿床特征与找矿远景[J].四川地质学报2007-27-2:96-98.
[46]贺光兴,孙启武,夏传见,邓斌武.四川省宁南县跑马铅锌矿成因浅析[J].地质找矿论丛.2006-21:81-84.
[47]匡文龙,刘继顺等.塔西南MVT型铅锌矿床成矿作用机制研究[J].新疆地质.2003-21-1:136-140.
[48]印建平,田培仁,戚学祥,陈克强.西昆仑塔木-卡兰古铅锌铜矿带含矿岩系的地质地球化学特征[J] .现代地质.2003-17-2:143-150.
[49]张守训.西秦岭代家庄中泥盆统沉积盆地铅锌矿同位素地质特征[J].甘肃科技.2007-23-10:70-73.
[50]祝新友,邓吉牛,王京彬,林龙军,樊俊昌.锡铁山铅锌矿床的找矿潜力与找矿方向[J].地质与勘探.2006-43-3:18-23.
[51]匡文龙,刘新华,陈年生等.湘西北下光荣矿区铅锌矿床主要地球化学特征[J].地质科学.2008:685-694.
[52]杨绍祥.湘西铅锌矿找矿前景分析[J] .湖南地质.2003-22-2:107-111.
[53]彭明兴,桑少杰,朱才,陈杰.新疆彩霞山铅锌矿床成因分析及与MVT型矿床成因对比[J].新疆地质.2007-25-4:373-383.
[54]王劲.新疆哈密市白干湖铅锌矿床地质特征及成因探讨[J] .新疆有色金属.第1期:6-8
[55]董永观,郭坤一,廖圣兵.新疆西昆仑科库西里克铅锌矿床地质及元素地球化学特征[J].地质学报.2006-80-11:1730-1738.
[56]高若峰.伊春市五星铅锌矿床地质特征与成因[J].黑龙江水利科技.2008-3-36:136.
[57]查世新,韩忠义.岳山银铅锌矿床地球化学特征[J].资源调查与环境.2002-23-4:272-280.
[58]牛文革,秦臻,李耀辉.云南省白竹箐-阳文山NE向构造带铅锌矿成矿地质条件及找矿方向[J].矿产与地质.2004-3-18:249-251.
[59]邹海俊,韩润生,胡彬,刘鸿.云南昭通毛坪铅锌矿床成矿物质来源的新证据[J].地质与勘探.2004-40-5:43-48.
[60]董文伟,陈少玲.镇康芦子园铅锌矿床特征及成因[J].云南地质.2007-26-4:404-410.
[61]臧世权,侯满堂,王文.昭镇旬铅锌矿田矿物包裹体研究[J].陕西地质.2001-19-1:30-36.
[62]侯满堂,藏世权,王文昭.镇旬铅锌矿田主要矿物的标型特征研究[J].陕西地质.2000-18-2:9-37.
[63]Brian jones,Kurto konhauser,Robn Wrenayut.Microbial silicification in Iodine Pool,Waimangu geothermal area,North Island,New Zealand:implications for recognition and identification of ancient silicified microbes[J].Journal of the Geological Society,London,2004-161:983-993.
[64]S.J.Pannalal,D.T.A.Symons,D.F.Sangster.Paleomagnetic dating of Upper Mississippi Valley zinc-lead mineralization,WI,USA[J].Journal of Applied Geophysics.2004-56:135-153.
[65]N.I.BASUKI and E.T.C.SPOONER.A Review of Fluid Inclusion Temperatures and Salinities in Mississippi Valley-type Zn-PbDeposits:Identifying Thresholds for Metal Transport[J].Explor.Mining Geol,2002.
[66]BRIAN JONES,ROBINW.RENAUT ect.Silicified Microbes in a Geyser Mound:The Enigma of Low-Temperature Cyanobacteria in a High-Temperature Setting[J].Palaios,2003-18:87-109. Joanne Nelson,Suzanne Paradis ect.Canadian Cordilleran Mississippi Valley-Type Deposits:A Case for Devonian-Mississippian Back-Arc Hydrothermal Origin[J].Economic Ceology,2002-97:1013-1036.
[67]S.Makhoukhi,J.M.Schmitt,M.Bouabdelli.Modelling of an MVT deposit:Touissit-Bou Beker district[J].Journal of Geochemical Exploration,2000-69-70:109-113.
[68]Robert C.R.Willan,Debbie C.Armstrong.Successive geothermal,volcanic-hydrothermal and contact-metasomatic events in Cenozoic volcanic-arc basalts,South Shetland Islands,Antarctica[J].Geol.Mag,2002-139:209-231.
[69]A.F.Kamona,G.H.Friedrich.Geology,mineralogy and stable isotope geochemistry of the Kabwe carbonate-hosted Pb-Zn deoosit,Central Zambia[J].Ore GeologyReviews,2007-30:217-243.
[70]D.J.MacKenzie,D.Craw,M.Begbie.Mineralogy,geochemistry,and structural controls of a disseminated gold-bearing alteration halo around the schist-hosted Bullendale orogenic gold deposit,New Zealand[J].Journal of Geochemical Exploration,2007-93:160-176.
[71]H.Albert Gilg,Maria Boni,Rupert Hochleitner,Ulrich Struck el.Stable isotope geochemistry of carbonate minerals in supergene oxidation zones of Zn-Pb deoosits[J].Ore Geology Reviews,2008-33:117-133.
[72]M.N.C.Araujo,F.C.Alnes da Silva,E,F,Jardim de Sa,R,J,Holcombe.Geometry and structural control of gold vein mineralizations in the Serido Belt,northeastern Brazil[J].Journal of South American Earth Sciences,2002-15:337-348.
[73]J-M.Schramm,J.T.Weidinger,H.J.Ibetsberger.Petrologic and structural controls on geomorphology of prehistoric Tsergo Ri slope failure,Langtang Himal,Nepal[J].Geomophology,1998-26:107-121.
[2]刘友勋,刘亚新,曾钦旺,黄革非,李建中.郴州西山地区银铅锌矿床地质特征及找矿方向[J].湖南地质.2002-21-4:282-285.
[3]刘家铎,张成江,刘显凡等.川滇黔相邻区域铜铅锌金银矿床与峨眉火成岩省的关系探讨[J].矿物岩石. 2003(12):74-79.
[4]周云满.滇东北乐红铅锌矿床地质特征及找矿远景[J].地质地球化学.2003年第31卷第4期:16-21.
[5]薛传东,韩润生,杨海林,杨志明等.滇西北保山核桃坪铅锌矿床成矿流体来源的同位素地球化学证据[J].矿床地质.2008-27-2:243-252.
[6]陈学明,邓军,沈崇辉,兰景志.凡口超大型铅锌矿床成矿流体的物理特征和地球化学特征[J]地球科学-中国地质大学学报.2000-25-4:438-442.
[7].雷良奇,宋慈安,冯佐海.佛子冲火山岩区隐伏铅锌矿床的类型归属及成矿远景[J].地质与勘探.2002-38-1:9-14.
[8]刘华东.福建黄地铅锌矿地质特征及成因探讨[J] .江西有色金属.2008-22-1:11-15.
[9]林仟同.福建建瓯八外洋铅锌矿床地质特征及其成因分析[J].福建地质第四期:178-185.
[10]陈火炮,李敬珠.福建顺昌山后铅锌矿床地质特征及成因探讨[J] .福建地质.第二期:204-210.
[11]祝新友,汪东波,卫冶国,邱小平,王瑞廷.甘肃代家庄铅锌矿的地质特征与找矿意义[J].地球学报.2006-27-7:595-602.
[12]刘伟,罗学红,王立波.关陵根铅锌矿矿床地质特征及成因探讨[J].甘肃地质.2008-17-1:47-53.
[13]张少萍.广东省连平县大尖山铅锌矿床成因及围岩含矿性[J] .科技资讯.2007-24:27-28.
[14]高凤颖.广东省紫金县苏石坑铅锌矿地质特征及成因[J].科技资讯导报. (2007)07(c)-0072-02:72-73.
[15]毛党龙.湖南保靖县且溪科铅锌矿地质特征[J] .化工矿产地质.2008-30-3:143-162.
[16]伍磊.广西贵港-平南地区铅锌矿带地质特征及找矿方向[J].矿产与地质.2001-15-5:329-334.
[17]郑星辉,周春玲,李建强,蓝元利.桂平市锡基坑铅锌矿床地质特征及外围找矿潜力分析[J].南方国土资源.2008-9:40-42.
[6]王长明,张寿庭,邓军,孙艳霞等.河南冷水北沟铅锌矿地质地球化学特征及成因探讨[J].矿床地质. 2007-26-2:175-183.
[18]王长明,邓军,张寿庭.燕长海.河南省卢氏栾川地区铅锌矿成矿多样性分析及成矿预测[J].地质通报.24 (10211) :1074~1080.
[19]常雪生.新疆西昆仑地区铅锌矿成矿特征与找矿前景.新疆有色金属.2003:2~8.
[20]李祥能.湖南后江桥铅锌矿地质特征及矿床成因[J] .地质找矿论丛. 2002-17-1:41-46.
[21]杨长明,李诚.湖南黄沙寺铜2铅2锌矿床控矿因素浅析[J] .矿产与地质. 2006-20-6:632-634.
[22]黄满相.湖南桥口铅锌矿床成矿流体特征[J] .湖北地矿.2004-18-2:14-18.
[23]张庆华.湖南水口山铅锌矿田地质特征及找矿思路[J].有色金属矿产与勘查.1999-8-3:141-146.
[24]段士刚,薛春纪,燕长海,刘国印,宋要武,张德会.华北陆块南、北缘铅锌矿床成矿特征对比[J].矿床地质.2008-07-3:383-393.
[25]刘崇民,马生明,胡树起等.火山热液型铅锌矿床岩石地球化学特征及预测指标[J].物探与化探.2008-32-2:154-158.
[26]杨斌,彭省临,杨牧,林德松,何国朝.江西银山铜铅锌矿床热液对流与蚀变矿化分带机制[J].桂林工学院学报.2004-04-4:395-401.
[27]彭晓明.将乐八里桥铅锌多金属矿地质特征及成因初探[J].资源与产业.2008-10-6:119-124.
[28]王京彬,姜俊康.吉昌可可塔勒矿带铅锌矿床找矿评价方法[J].新疆地质.2001-19-1:64-69.
[29]刘凤鸣.库尔尕生铅锌矿床地质特征及成因浅析[J] .新疆有色金属.第三期:4-6.
[30]王新利,庞艳春.澜沧老厂银铜铅锌多金属矿床地质特征及成因探讨[J].地质与资源.2006-15-3:200-221.
[31]王艳.辽宁本溪盘岭地区铜、铅锌矿床成矿条件探讨[J] .辽宁地质.2001-18-1:28-42.
[32]李南生.闽清牛路坑铅锌矿床地质特征与成因初探[J].福建地质第一期:22-38.
[33]狄永军,吴淦国,张达等.闽中地区铅锌矿床辉石成分特征及其成因意义[J].矿床地质. 2006-25-2:123-134.
[34]张生辉,石建基,狄永军,余心起等.闽中裂谷块状硫化物型铅锌矿床的地质特征及找矿意义[J] .现代地质.2005-19-3:375-384.
[35]李振祥,谢振玉,刘召,李淑果.内蒙古西乌珠穆沁旗花敖包特银铅锌矿矿床地质特征及成因初探[J].地质与资源.2008-17-4:278-281.
[36]方如恒.中朝古元古代层控铅锌矿床类型及其比较[J].辽宁地质.1999-16-1:43-56
[37]徐发,王永军,刘国庆.内蒙古扎鲁特旗香山铜铅锌矿区成矿地质条件分析及找矿潜力[J].矿产与地质.2004-102-2:148-151.
[38]陈国勇.黔南台陷碳酸盐型铅锌矿床成矿条件及找矿模型[J].贵州地质.2002-19-1:20-26.
[39]贾润幸,郭健等.秦岭凤太成矿区多金属矿床成矿流体地球化学特征[J].中国地质.2004-31-2:192-198.
[40]孙文涛,孙吉国,孙红云,谢常君.青城子矿田杨树区超大型金银铅锌矿床地质特征及成矿机理[J].地质与勘探.2008-44-4:24-30.
[41]侯满堂,王党国,高杰,高怀雄.陕西马元地区铅锌矿矿石特征研究[J].陕西地质.2007-25-1:1-37.
[42]朱华平,张德全.陕西南秦岭志留系中铅锌矿床地质地球化学特征研究[J].地质找矿论丛2004-19-2:76-86.
[43]齐文.陕西商州龙庙铅锌矿床特征及成因探讨[J].陕西地质.2002-20-1:28-38.
[44]何显刚,李淑慧,谢恩顺.四川巴塘砂西银铅锌矿床特征与找矿远景[J].四川地质学报.2004-24-2:77-81.
[45]旦贵兵,杨大宏,沈史日.四川宁南雀珠山地区铅锌矿床特征与找矿远景[J].四川地质学报2007-27-2:96-98.
[46]贺光兴,孙启武,夏传见,邓斌武.四川省宁南县跑马铅锌矿成因浅析[J].地质找矿论丛.2006-21:81-84.
[47]匡文龙,刘继顺等.塔西南MVT型铅锌矿床成矿作用机制研究[J].新疆地质.2003-21-1:136-140.
[48]印建平,田培仁,戚学祥,陈克强.西昆仑塔木-卡兰古铅锌铜矿带含矿岩系的地质地球化学特征[J] .现代地质.2003-17-2:143-150.
[49]张守训.西秦岭代家庄中泥盆统沉积盆地铅锌矿同位素地质特征[J].甘肃科技.2007-23-10:70-73.
[50]祝新友,邓吉牛,王京彬,林龙军,樊俊昌.锡铁山铅锌矿床的找矿潜力与找矿方向[J].地质与勘探.2006-43-3:18-23.
[51]匡文龙,刘新华,陈年生等.湘西北下光荣矿区铅锌矿床主要地球化学特征[J].地质科学.2008:685-694.
[52]杨绍祥.湘西铅锌矿找矿前景分析[J] .湖南地质.2003-22-2:107-111.
[53]彭明兴,桑少杰,朱才,陈杰.新疆彩霞山铅锌矿床成因分析及与MVT型矿床成因对比[J].新疆地质.2007-25-4:373-383.
[54]王劲.新疆哈密市白干湖铅锌矿床地质特征及成因探讨[J] .新疆有色金属.第1期:6-8
[55]董永观,郭坤一,廖圣兵.新疆西昆仑科库西里克铅锌矿床地质及元素地球化学特征[J].地质学报.2006-80-11:1730-1738.
[56]高若峰.伊春市五星铅锌矿床地质特征与成因[J].黑龙江水利科技.2008-3-36:136.
[57]查世新,韩忠义.岳山银铅锌矿床地球化学特征[J].资源调查与环境.2002-23-4:272-280.
[58]牛文革,秦臻,李耀辉.云南省白竹箐-阳文山NE向构造带铅锌矿成矿地质条件及找矿方向[J].矿产与地质.2004-3-18:249-251.
[59]邹海俊,韩润生,胡彬,刘鸿.云南昭通毛坪铅锌矿床成矿物质来源的新证据[J].地质与勘探.2004-40-5:43-48.
[60]董文伟,陈少玲.镇康芦子园铅锌矿床特征及成因[J].云南地质.2007-26-4:404-410.
[61]臧世权,侯满堂,王文.昭镇旬铅锌矿田矿物包裹体研究[J].陕西地质.2001-19-1:30-36.
[62]侯满堂,藏世权,王文昭.镇旬铅锌矿田主要矿物的标型特征研究[J].陕西地质.2000-18-2:9-37.
[63]Brian jones,Kurto konhauser,Robn Wrenayut.Microbial silicification in Iodine Pool,Waimangu geothermal area,North Island,New Zealand:implications for recognition and identification of ancient silicified microbes[J].Journal of the Geological Society,London,2004-161:983-993.
[64]S.J.Pannalal,D.T.A.Symons,D.F.Sangster.Paleomagnetic dating of Upper Mississippi Valley zinc-lead mineralization,WI,USA[J].Journal of Applied Geophysics.2004-56:135-153.
[65]N.I.BASUKI and E.T.C.SPOONER.A Review of Fluid Inclusion Temperatures and Salinities in Mississippi Valley-type Zn-PbDeposits:Identifying Thresholds for Metal Transport[J].Explor.Mining Geol,2002.
[66]BRIAN JONES,ROBINW.RENAUT ect.Silicified Microbes in a Geyser Mound:The Enigma of Low-Temperature Cyanobacteria in a High-Temperature Setting[J].Palaios,2003-18:87-109. Joanne Nelson,Suzanne Paradis ect.Canadian Cordilleran Mississippi Valley-Type Deposits:A Case for Devonian-Mississippian Back-Arc Hydrothermal Origin[J].Economic Ceology,2002-97:1013-1036.
[67]S.Makhoukhi,J.M.Schmitt,M.Bouabdelli.Modelling of an MVT deposit:Touissit-Bou Beker district[J].Journal of Geochemical Exploration,2000-69-70:109-113.
[68]Robert C.R.Willan,Debbie C.Armstrong.Successive geothermal,volcanic-hydrothermal and contact-metasomatic events in Cenozoic volcanic-arc basalts,South Shetland Islands,Antarctica[J].Geol.Mag,2002-139:209-231.
[69]A.F.Kamona,G.H.Friedrich.Geology,mineralogy and stable isotope geochemistry of the Kabwe carbonate-hosted Pb-Zn deoosit,Central Zambia[J].Ore GeologyReviews,2007-30:217-243.
[70]D.J.MacKenzie,D.Craw,M.Begbie.Mineralogy,geochemistry,and structural controls of a disseminated gold-bearing alteration halo around the schist-hosted Bullendale orogenic gold deposit,New Zealand[J].Journal of Geochemical Exploration,2007-93:160-176.
[71]H.Albert Gilg,Maria Boni,Rupert Hochleitner,Ulrich Struck el.Stable isotope geochemistry of carbonate minerals in supergene oxidation zones of Zn-Pb deoosits[J].Ore Geology Reviews,2008-33:117-133.
[72]M.N.C.Araujo,F.C.Alnes da Silva,E,F,Jardim de Sa,R,J,Holcombe.Geometry and structural control of gold vein mineralizations in the Serido Belt,northeastern Brazil[J].Journal of South American Earth Sciences,2002-15:337-348.
[73]J-M.Schramm,J.T.Weidinger,H.J.Ibetsberger.Petrologic and structural controls on geomorphology of prehistoric Tsergo Ri slope failure,Langtang Himal,Nepal[J].Geomophology,1998-26:107-121.