滇东南卡林型金矿地质地球化学与成矿模式
|
摘要
滇东南地区是我国著名的卡林型金矿集中区——滇黔桂“金三角”之一角,对该区卡林型金矿的系统研究目前仍显不足。本文以板块构造理论、区域成矿学、地球化学、成矿预测学和找矿系统工程学为指导,基于十余年滇东南地区的金矿找矿实践,以大量地质地球化学数据为支撑,以滇东南地区卡林型金矿不同亚类典型矿床解剖为切入点,以成矿系列的概念将本区金矿与钨锡、铜铅锌银、砷锑汞(钡)等矿产时空分布上连成一线,以卡林型金矿成矿作用、成矿规律、成矿预测为主线,系统研究了滇东南地区卡林型金矿地质地球化学特征、控矿要素和成矿规律,并开展成矿预测。论文工作重点是以区域成矿学为主的多学科的综合研究,取得的主要成果和认识如下:
1、结合对卡林型金矿研究现状的探讨,提出了卡林型金矿的再定义问题,将卡林型金矿定义为区带上集中分布的(超)微细、浸染、中低温热液金矿床。
2、运用地物化遥等资料系统论述了滇黔桂菱块体(“金三角”)区域成矿地质背景,肯定了右江裂谷带(幔隆带)的存在,论证了滇黔桂“金三角”地区卡林型金矿的物源主要与裂谷和区域性深大断裂附近峨眉地幔柱长期活动相伴的基性火成岩及火山碎屑浊流沉积有关,区域构造运动及其与之相伴的酸性和基性岩浆活动是滇东南地区乃至滇黔桂地区金矿成矿作用最为主要的热源。
3、论证了南盘江盆地的形成与演化,是印度板块、欧亚板块、太平洋板块相互碰撞导致地幔上隆引起玄武岩喷溢和水平拉伸在构造薄弱地段造成差异性下陷的结果,从区域地层地球化学角度指出右江裂谷活动至少始于寒武纪,随着时间的推移,由桂西北逐渐影响到滇东南及黔西南。
4、对滇东南地区卡林型金矿地质特征作了概略性介绍,根据金矿的产出特点、容矿岩石等将滇东南地区卡林型金矿分为细碎屑岩-不纯碳酸盐岩型、不整合面型、基性岩型、红色粘土型。探讨了滇东南地区卡林型金矿与含金建造、岩浆岩、构造的关联,并以典型金矿床为例阐述了该区卡林型金矿的常量元素、微量元素、稀土元素、包裹体、同位素和黄铁矿单矿物等地球化学特征。
5、系统论述了滇东南地区卡林型金矿成矿作用,指出壳幔不均一性及其相互作用→预成矿作用→成矿作用→后成矿作用是大自然对壳幔物质所进行的一系列“选矿”过程,各种成矿作用之间既相互联系又递进发展。提出了“预成矿作用”的概念、可能性及其对卡林型金矿等中低温矿产成矿作用的重要影响。从地球化学角度探讨了金的迁移沉淀机制。
6、用成矿系列的理论将滇东南地区的金矿与钨锡、铜铅锌银、金砷锑汞等矿产进行时空上的关联,提出滇东南地区主要存在如下成矿系列组合:①越北古陆北缘与南盘江盆地演化相关联的预成矿系列组合;②与峨眉地幔柱活动相关联的中低温成矿系列组合;③与燕山期花岗岩浆活动、区域构造运动相关联的叠加改造成矿系列组合。
7、提出了滇东南地区卡林型金矿矿床成因的三因素:(1)壳幔的不均一性及地球从起始演化到现今的过程中元素的分布再分配是形成矿种区域空间分布差异的基础因素;(2)预成矿作用是滇东南地区主要沿加里东不整合面形成不整合面型金矿的重要因素。(3)越北古陆的向北逆冲推覆和几大板块平移走滑所形成的驱动热力和与此相关的断褶带、层间破碎带及岩体外围由岩浆侵位、冷缩形成的密集张裂带是滇东南乃至滇黔桂“金三角”地区卡林型金矿及其他内生矿产形成的决定因素,进一步总结了滇东南地区卡林型金矿成矿规律和成矿模式。
8、以成矿系列理论、区域成矿学、成矿预测学作为指导,对该区金矿进行了有针对性的预测研究。并将研究成果重点应用在曼龙沟金矿深边部及外围新区的地质找矿和工程验证工作中;对个旧矿区外围和邱北某金矿深部进行成矿靶区预测,提出在滇黔桂菱块体内除右江裂谷外金等亲铁元素仍然有其他上升通道,因此,在滇东南乃至滇黔桂“金三角”地区具有找寻大型、超大型原生金矿的良好前景。
Southeast Yunnan province is a part of Dian-Qian-Gui gold-triangle, one of the famous concentration area of carlin-type gold deposits,and presently the systematic research is still insufficient for it.Guided by theory of plate tectonics,regional metallogenics,geochemistry, metallogenic prognosis,prospecting systematic engineering,based on more than ten years of gold-prospecting practice in Southeastern Yunnan area,the author has collected a large number of geological and geochemical data,analyzed different sub-types of the carlin-type gold deposits,and pay attention to the temporal and spatial distribution of gold and tin-tungsten,copper lead,zinc and silver,antimony arsenic mercury(Ba).Furthermore,took the mineralization,metallogenic law, forming within this area as the main line,the author has conducted systematic studies about its geological and geochemical characteristics, metallogenesis,metallogenesis law and metallogenic prognosis.The main achievements and cognitions are as follows:
1.Combined with its existing studies,a redefinition of Carlin-type gold deposits is put forward that is(ultra) fine,disseminated, meso-epithermal gold deposits with concentrated zoning distribution.
2.Regional metallogery geological setting of Dian-Qian-Gui gold-triangle was systematically discussed with geology,geophysics, geochemistry and remote sense data,the existence of Youjiang valley(mantle swell) was also be confirmed,and it was demonstrated that the source material of Carlin-type gold deposits in Dian-Qian-Gui gold-triangle is mainly relative to the basic igneous rock and volcaniclastic turbidite deposition which accompanied with the Emei mantle plume activity happened nearby the rift valley and regional discordogenic fault.The regional structure movement and acidity and the basic magmatic activity accompanying were the most important heat source.
3.It is demonstrated that the formation and evolution of Nanpanjiang basin is the result of the differential subsidence on the weak district caused by the effusion and horizontal stretching of basalt which originated from the collision of Indian,Eurasian and Pacific plates and then the mantle thriving.It is pointed out that,from the regional geochemistry standpoint,the Youjiang Rift activity begins as early as Cambrian Period at least,and splits gradually form western Guangxi to southeastern Yunnan and southwestern Guizhou.
4.A brief introduction about the geological characteristics of carlin-type gold deposit in Southeast Yunnan province is given in the paper.On the basis of its yielding features,host rocks etc.,the Karlin gold ore in southeast Yunnan region could be divided into fine clastic rock-impure carbonatite type,unconformity type,basic rock type and red clay type.Discussed the relationship between Carlin-type gold deposits and gold-bearing construction,magmatic rocks,tectonic,and took the typical gold deposits in this studying area for example,the author presented the geochemical characteristic of the major elements,trace elements,REE,fluid inclusion,isotopes and pyrite single mineral and so on.
5.As for the mineralization of Carlin-type gold deposit in Southeastern Yunnan province,it is indicated that crust-mantle inhomogeneity and their interactions→pre-metallogenesis→metallogenesis→post-metallogenesis is a series of natural "Beneficiation" Process and they contacted and promoted with each other. "pre-metallogenesis" concept,the possibility and its implications for mineralization of epithermal-mesothermal ore deposits(such as carlin-type gold deposit etc.) were put forward in the paper.Furthermore, from the geochemical point of view,the author discussed the mechanism of ore-forming transfer and sedimentation.
6.Using the theory of metallogenic series,the author discussed the space-time relationship between gold deposit and tungsten,tin,copper, lead,zinc,silver,antimony,arsenic,mercury and other minerals,and put forward there are some major metallogenic series combination in Southeast Yunnan including:(1) the pre-metallogenesis series related to the evolution of northern Vietnam oldland and Nanpanjiang basin;(2) the epithermal-mesothermal minerogentic series related to the Emei mantle column activity;(3) the superimpositiom and transformation minerogentic series related to the Yanshanian granitic magma activity and regional tectonic movement.
7.As for the genesis of Carlin-type gold deposit in Southeastern Yunnan,three conclusion are summarized:(1) Crust-mantle inhomogeneity and distribution and redividsion of the elements from original evolution to present are the basic factors of special distribution difference of different ore(2) Pre-metallogenesis is the key factor of the unconformity type gold deposit mainly forming along the Caledonian unconformity surface;(3) Driving heating power came from the northward thrust overriding of Vietnam oldland and strike-slip of a few macroplate,and associated with fault-fold zone,cut-layer fracture structure and the intensive tension zone formed by magmatic intrusion and shrinkage at the external magmatic-body are determinate for the formation of Carlin-type gold deposit and other endogenetic deposit in Dian-Qian-Gui gold-triangle even in southeastern Yunnan province.What's more,the author formerly summed up the metallogenic laws and metallogenic model of Carlin-type gold deposit in Southeastern Yunnan region.
8.As for the gold prospect of the region,guided by theory of metallogenic series,regional metallogenics,metallogenic prognosis,the author made some pertinence investigation,and then focus on the application of research results at geology prospecting and engineering approval in deep ditch and external edge of Manlonggou gold deposit.At the same time,The author predicted the ore-forming targets at the outskirts of Gejiu deposit and deep part of one gold deposit in Qiubei, and put forward that in addition to Youjiang rift,there are still have others ascending passageway for the gold and other siderophile elements in Dian-Qian-Gui gold-triangle.Therefore,it is good prospect to look for large,superlarge primary gold deposit in southeastern Yunnan even in Dian-Qian-Gui gold-triangle area.
1、结合对卡林型金矿研究现状的探讨,提出了卡林型金矿的再定义问题,将卡林型金矿定义为区带上集中分布的(超)微细、浸染、中低温热液金矿床。
2、运用地物化遥等资料系统论述了滇黔桂菱块体(“金三角”)区域成矿地质背景,肯定了右江裂谷带(幔隆带)的存在,论证了滇黔桂“金三角”地区卡林型金矿的物源主要与裂谷和区域性深大断裂附近峨眉地幔柱长期活动相伴的基性火成岩及火山碎屑浊流沉积有关,区域构造运动及其与之相伴的酸性和基性岩浆活动是滇东南地区乃至滇黔桂地区金矿成矿作用最为主要的热源。
3、论证了南盘江盆地的形成与演化,是印度板块、欧亚板块、太平洋板块相互碰撞导致地幔上隆引起玄武岩喷溢和水平拉伸在构造薄弱地段造成差异性下陷的结果,从区域地层地球化学角度指出右江裂谷活动至少始于寒武纪,随着时间的推移,由桂西北逐渐影响到滇东南及黔西南。
4、对滇东南地区卡林型金矿地质特征作了概略性介绍,根据金矿的产出特点、容矿岩石等将滇东南地区卡林型金矿分为细碎屑岩-不纯碳酸盐岩型、不整合面型、基性岩型、红色粘土型。探讨了滇东南地区卡林型金矿与含金建造、岩浆岩、构造的关联,并以典型金矿床为例阐述了该区卡林型金矿的常量元素、微量元素、稀土元素、包裹体、同位素和黄铁矿单矿物等地球化学特征。
5、系统论述了滇东南地区卡林型金矿成矿作用,指出壳幔不均一性及其相互作用→预成矿作用→成矿作用→后成矿作用是大自然对壳幔物质所进行的一系列“选矿”过程,各种成矿作用之间既相互联系又递进发展。提出了“预成矿作用”的概念、可能性及其对卡林型金矿等中低温矿产成矿作用的重要影响。从地球化学角度探讨了金的迁移沉淀机制。
6、用成矿系列的理论将滇东南地区的金矿与钨锡、铜铅锌银、金砷锑汞等矿产进行时空上的关联,提出滇东南地区主要存在如下成矿系列组合:①越北古陆北缘与南盘江盆地演化相关联的预成矿系列组合;②与峨眉地幔柱活动相关联的中低温成矿系列组合;③与燕山期花岗岩浆活动、区域构造运动相关联的叠加改造成矿系列组合。
7、提出了滇东南地区卡林型金矿矿床成因的三因素:(1)壳幔的不均一性及地球从起始演化到现今的过程中元素的分布再分配是形成矿种区域空间分布差异的基础因素;(2)预成矿作用是滇东南地区主要沿加里东不整合面形成不整合面型金矿的重要因素。(3)越北古陆的向北逆冲推覆和几大板块平移走滑所形成的驱动热力和与此相关的断褶带、层间破碎带及岩体外围由岩浆侵位、冷缩形成的密集张裂带是滇东南乃至滇黔桂“金三角”地区卡林型金矿及其他内生矿产形成的决定因素,进一步总结了滇东南地区卡林型金矿成矿规律和成矿模式。
8、以成矿系列理论、区域成矿学、成矿预测学作为指导,对该区金矿进行了有针对性的预测研究。并将研究成果重点应用在曼龙沟金矿深边部及外围新区的地质找矿和工程验证工作中;对个旧矿区外围和邱北某金矿深部进行成矿靶区预测,提出在滇黔桂菱块体内除右江裂谷外金等亲铁元素仍然有其他上升通道,因此,在滇东南乃至滇黔桂“金三角”地区具有找寻大型、超大型原生金矿的良好前景。
Southeast Yunnan province is a part of Dian-Qian-Gui gold-triangle, one of the famous concentration area of carlin-type gold deposits,and presently the systematic research is still insufficient for it.Guided by theory of plate tectonics,regional metallogenics,geochemistry, metallogenic prognosis,prospecting systematic engineering,based on more than ten years of gold-prospecting practice in Southeastern Yunnan area,the author has collected a large number of geological and geochemical data,analyzed different sub-types of the carlin-type gold deposits,and pay attention to the temporal and spatial distribution of gold and tin-tungsten,copper lead,zinc and silver,antimony arsenic mercury(Ba).Furthermore,took the mineralization,metallogenic law, forming within this area as the main line,the author has conducted systematic studies about its geological and geochemical characteristics, metallogenesis,metallogenesis law and metallogenic prognosis.The main achievements and cognitions are as follows:
1.Combined with its existing studies,a redefinition of Carlin-type gold deposits is put forward that is(ultra) fine,disseminated, meso-epithermal gold deposits with concentrated zoning distribution.
2.Regional metallogery geological setting of Dian-Qian-Gui gold-triangle was systematically discussed with geology,geophysics, geochemistry and remote sense data,the existence of Youjiang valley(mantle swell) was also be confirmed,and it was demonstrated that the source material of Carlin-type gold deposits in Dian-Qian-Gui gold-triangle is mainly relative to the basic igneous rock and volcaniclastic turbidite deposition which accompanied with the Emei mantle plume activity happened nearby the rift valley and regional discordogenic fault.The regional structure movement and acidity and the basic magmatic activity accompanying were the most important heat source.
3.It is demonstrated that the formation and evolution of Nanpanjiang basin is the result of the differential subsidence on the weak district caused by the effusion and horizontal stretching of basalt which originated from the collision of Indian,Eurasian and Pacific plates and then the mantle thriving.It is pointed out that,from the regional geochemistry standpoint,the Youjiang Rift activity begins as early as Cambrian Period at least,and splits gradually form western Guangxi to southeastern Yunnan and southwestern Guizhou.
4.A brief introduction about the geological characteristics of carlin-type gold deposit in Southeast Yunnan province is given in the paper.On the basis of its yielding features,host rocks etc.,the Karlin gold ore in southeast Yunnan region could be divided into fine clastic rock-impure carbonatite type,unconformity type,basic rock type and red clay type.Discussed the relationship between Carlin-type gold deposits and gold-bearing construction,magmatic rocks,tectonic,and took the typical gold deposits in this studying area for example,the author presented the geochemical characteristic of the major elements,trace elements,REE,fluid inclusion,isotopes and pyrite single mineral and so on.
5.As for the mineralization of Carlin-type gold deposit in Southeastern Yunnan province,it is indicated that crust-mantle inhomogeneity and their interactions→pre-metallogenesis→metallogenesis→post-metallogenesis is a series of natural "Beneficiation" Process and they contacted and promoted with each other. "pre-metallogenesis" concept,the possibility and its implications for mineralization of epithermal-mesothermal ore deposits(such as carlin-type gold deposit etc.) were put forward in the paper.Furthermore, from the geochemical point of view,the author discussed the mechanism of ore-forming transfer and sedimentation.
6.Using the theory of metallogenic series,the author discussed the space-time relationship between gold deposit and tungsten,tin,copper, lead,zinc,silver,antimony,arsenic,mercury and other minerals,and put forward there are some major metallogenic series combination in Southeast Yunnan including:(1) the pre-metallogenesis series related to the evolution of northern Vietnam oldland and Nanpanjiang basin;(2) the epithermal-mesothermal minerogentic series related to the Emei mantle column activity;(3) the superimpositiom and transformation minerogentic series related to the Yanshanian granitic magma activity and regional tectonic movement.
7.As for the genesis of Carlin-type gold deposit in Southeastern Yunnan,three conclusion are summarized:(1) Crust-mantle inhomogeneity and distribution and redividsion of the elements from original evolution to present are the basic factors of special distribution difference of different ore(2) Pre-metallogenesis is the key factor of the unconformity type gold deposit mainly forming along the Caledonian unconformity surface;(3) Driving heating power came from the northward thrust overriding of Vietnam oldland and strike-slip of a few macroplate,and associated with fault-fold zone,cut-layer fracture structure and the intensive tension zone formed by magmatic intrusion and shrinkage at the external magmatic-body are determinate for the formation of Carlin-type gold deposit and other endogenetic deposit in Dian-Qian-Gui gold-triangle even in southeastern Yunnan province.What's more,the author formerly summed up the metallogenic laws and metallogenic model of Carlin-type gold deposit in Southeastern Yunnan region.
8.As for the gold prospect of the region,guided by theory of metallogenic series,regional metallogenics,metallogenic prognosis,the author made some pertinence investigation,and then focus on the application of research results at geology prospecting and engineering approval in deep ditch and external edge of Manlonggou gold deposit.At the same time,The author predicted the ore-forming targets at the outskirts of Gejiu deposit and deep part of one gold deposit in Qiubei, and put forward that in addition to Youjiang rift,there are still have others ascending passageway for the gold and other siderophile elements in Dian-Qian-Gui gold-triangle.Therefore,it is good prospect to look for large,superlarge primary gold deposit in southeastern Yunnan even in Dian-Qian-Gui gold-triangle area.
引文
[1]郭富达,华南地区物化遥编图滇黔桂片区滇东南地区遥感解译总结,云南地矿局物化探队(内部资料),1994,2-8。
[1]Radtke,A.S.Geology of the Carlin gold deposit,Nevada:USGS openfile.1981,187:81-97
[2]Cox,D.P.and Singer,D.A.,Grade and tonnage model of distal disseminated Ag-Au,in Bliss,J.D.,ed.,Developments in mineral deposit modeling:U.S.Geological Survey Bulletin,2004,1992,p.20-22.
[3]Zhiping Li,Stephen G.Peters,Comparative Geology and Geochemistry of Sedimentary-Rock-Hosted(Carlin-Type) Gold Deposits in the People's Republic of China and in Nevada,USA,U.S.DEPARTMENT OF THE INTERIOR,U.S.GEOLOGICAL SURVEY,1998,1-12
[4]Lewis Teal,Mac Jackson,Geologic Overview of the Carlin Trend Gold Deposits and Descriptions of RecentDeep Discoveries,CARLIN-TYPE GOLD DEPOSITS FIELD CONFERENCE Edited by Peter Vikre,Tommy B.Thompson,Keith Bettles et al.,SOCIETY OF ECONOMIC GEOLOGISTS,1997:3-37
[5]王登红.卡林型金矿找矿新进展及其意义.地质地球化学,2000,28(1):92-94.
[6]谭延松.石峡微细浸染型金矿金的赋存状态及其回收预测.地质与勘探,1980(9):
[7]王学求.矿产勘查地球化学:过去的成就与未来的挑战.地学前缘,2003,10(1):239-246
[8]张复新,侯俊富,张存旺,等.甘肃阳山超大型卡林—类卡林型复合式金矿床特征.中国地质,2007,34(6):1062-1072
[9]A.S.拉德克.卡林金矿地质学.贵州省地质矿产局科技情报室,1987,57-72
[10]韦永福,吕英杰,等.中国金矿床.北京:地震出版社,1994.39-49
[11]李舒,李景春,卲军,等.中国金矿床工业类型及其特征.北京:地震出版社,1999.1-8
[12]陈毓川,李兆鼎,母瑞身,等.中国金矿床及其成矿规律.北京:地质出版社.2001.2-11
[13]刘东升,谭运金,王建业,等.中国卡林型(微细浸染型)金矿.南京:南京大学出版社,1994.1-36
[14]张贻侠,寸珪,刘连登,等.中国金矿床进展与思考.北京:地质出版社,1996.10-21
[15]波利申科,纳乌莫夫,巴甫洛娃,等.卞善涛,蒋琪,译.金—汞矿床:矿床类型、分布规律和成因模式.云南地质,2006,25(1):45-52
[16]Stephen G.Peters,Huang Jiazhan,Li Zhiping,et al.Introduction to and Classification of Sedimentary Rock-Hosted Au Deposits in P.R.China.USGS,2002:26-43
[17]Mao J,Qiu Y,Goldfarb,et al.Geology,distribution,and classification of Gold deposits in the western Qinling belt,China.Min Dep,2002,37:352-377
[18]A.H.Hofstra,P.Emsbo,W.D.Christiansen,et al,Source of ore fluids in Carlin-type gold deposits,China:Implications for genetic models,Mineral Deposit Research:Meeting the Global Challenge,Proceedings of the Eighth Biennial SGA Meeting,Beijing,China,18-21 August 2005:533-536
[19]刘继顺,舒广龙,高珍权.鄂东丰山矿田卡林型金矿地质地球化学特征.地学前缘,2004,11(2):379-385
[20]Herzig P M,Hannington M D.Polymetallic massive sulfides at the modern seafloor-areview.Ore Geol Rev,1995,10:95-115
[21]李朝阳.有关卡林型金矿的几点认识.矿物学报,1995,15(2):132-137
[22]涂光炽.低温地球化学.北京:科学出版社,1996.1-202
[23]王可勇,姚书振,吕新标.国内外微细浸染型金矿床研究现状及发展趋势.贵金属地质,2000,9(4):223-228
[24]Kuehn C.A.,Rose A.W.Carlin gold deposit.Nevada:Origin in a deep zone of mixing between normally pressured and overpressured fluids,Ec onomic,Geology,1995,90:17-36
[25]Sillitoe R.H.,Bonham H.F.Sediment-hosted gold deposits;distal products of magmatic-hydrothermal systems.Geology.1990;18:157-161
[26]谭运金.滇黔桂地区微细粒浸染型金矿床的地球化学类型.矿床地质,1994,13(4):308-321
[27]侯宗林,杨庆得.滇黔桂地区微细浸染型金矿成矿条件及成矿模式.地质找矿论丛,1989,4(3):1-11
[28]万兵.滇黔桂三角区金(银)矿床地质特征及成矿条件.矿产与地质,1991,5(3):169-172
[29]张兴余译.碳酸盐岩为主岩的浸染型金矿床形成模式.国外铀矿地质,1998,(2):12-18
[30]Nessbitt B E.Gold deposit continuum:A genetic model for lode Au mineralization in the continental crust.Geology,1988,16:1044-1048
[31]王登红,林文蔚,杨建民,等.试论地幔柱对我国两大金矿集中区的控制意义.地球学报,1999,20(2):157-162
[32]高振敏,李红阳,杨竹森,等.滇黔地区主要类型金矿的成矿与找矿.北京:地质出版社,2002.30-58
[33]Wang G Z,Hu R Z,Su W C,et al.Fluid flow and mineralization of Youjiang Basin in the Yunnan-Guizhou-Guangxi area,China.SCIENCE IN CHINA(Series D),2003,Vol.46 Supp:99-109
[34]周余国,刘继顺,王作华,等.从滇黔桂“金三角”区域地层地球化学特征探讨卡林型金矿的物质来源.地学前缘,2009,16(2):1-10
[35]张秋明译.矿床模式(九):浸染型金矿床.国外矿产地质,1987,(1):1-4
[36]汪东坡,邵世才,徐勇.金矿化过程中两个地球化学问题探讨.地球科学—中国地质大学学报,1999,24(3):292-296
[37]汪东波.金与铅锌矿化的关系.矿床地质,1998,17(增刊):345-348
[38]刘家军,刘建明,顾雪详,等.黔西南微细浸染型金矿的喷流沉积成因.科学通报,42卷:2126-2127
[39]刘家军,郑明华,顾雪祥,等.海底喷流作用对金富集成矿的意义.矿产与地质,1997,11(5):289-295
[40]周余国,刘继顺,欧阳玉飞,等.卡林型金矿的再定义.黄金,2008,29(11):7-11
[41]谢学锦.区域化探全国扫面积划.物化探研究报导,1978,3:28-36
[42]王淑玲.世界矿产资源年评2003:金.国土资源部信息中心编:183-194
[43]杨科佑,等.滇黔桂及川西北卡林型金矿.中国科学院黄金科技工作领导小组办公室编,中国金矿研究新进展.北京:地震出版社,1994.284-350
[44]周永峰.区域重力资料研究在广西深部地质和成矿预测中的应用.广西地质,1993,2
[45]黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,51(2):117-135
[46]张文佑.中国及邻区海陆大地构造图.北京:科学出版社,1983
[47]张文佑.断块构造导论.北京:石油出版社,1984
[48]任纪舜,姜春发,张正坤,等.中国大地构造及其演化.北京:科学出版社,1980:1-124.
[49]广西壮族自治区地质矿产局.广西壮族自治区区域地质志.北京:地质出版社,1985:1-853
[50]柳淮之,钟自云,姚明,等.右江裂谷带初探.桂林冶金地质学院学报, 1986,6(1):9-19
[51]王鸿桢.中国华南地区地壳构造发展的轮廓—华南地区古大陆边缘构造史.武汉:武汉地质学院出版社,1986.1-15
[52]刘本培.华南地区海西印支阶段构造带地理格局//王鸿桢,杨巍然,刘本培.华南地区古大陆边缘构造史.武汉:武汉地质学院出版社.1986
[53]许靖华,孙枢,李继亮.是华南造山带而不是华南地台.中国科学(B),1987,10:1107-1115
[54]王宝禄,郭富达,何邵麟,等.华南地区物探化探遥感成果编图/黔桂滇重点片综合解释成果报告.地矿部华南地区物探化探遥感编图委员会滇黔桂重点片综合解译组,1995,1-180
[55]朱炳泉,常向阳,邱华宁,等.地球化学急变带的元古宙基底特征及其与超大型矿床产出的关系.中国科学(D辑),1998a,28(增刊):63-70
[56]朱炳泉,常向阳.地球化学省与地球化学边界.地球科学进展,2001,16(2):153-162
[57]朱炳泉.壳幔化学不均一性与块体地球化学边界研究.地学前缘,1998,5(1、2):72-82
[58]梅冥相,马永生,邓军.加里东运动构造古地理及滇黔桂盆地的形成.地学前缘,2005,3:227-236
[59]陈旭等,戎嘉余,周志毅,等.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升.科学通报,2001,46(12):1052-1056
[60]苏文博.上扬子地台东南缘奥陶纪层序地层及海平面变化研究.北京:地质出版社,2001.1-106
[61]马文璞.区域构造解析-方法理论和中国板块构造.北京:地质出版社,1992.1-308
[62]章雨旭.地质学研究中常见逻辑方面的问题分析.高校地质学报,2006,12(1):147-152
[63]赵自强,丁启秀.中南区区域地层.武汉:中国地质大学出版社,1996:71-118
[64]曾允孚,张锦泉,刘文均,等.中国南方泥盆纪岩相古地理与成矿作用.北京:地质出版社,2001:1-120
[65]梅冥相,马永生,戴少武,等.南盘江盆地晚古生代盆地充填序列特征及生储盖组合划分.现代地质,2001,15(1):74-82
[66]梅冥相,马永生,高金汉,等.滇黔桂盆地及其邻区晚古生代层序地层格架及相对海平面变化.现代地质,2002,16(4):365-373
[67]梅冥相,李仲远.滇黔桂地区晚古生代至三叠纪盆层序地层序列及沉积盆地演化.现代地质,2004,18(4):555-563
[68]吴浩若.晚古生代-三叠纪南盘江海的构造古地理问题.古地理学报,2003,5(1):63-74
[69]章正军,丁俊,赵珉.滇东南及邻区晚古生代-中生代沉积盆地演化及微细粒型金矿成矿作用分析.云南地质,1996,15(3):282-288
[70]翟佑华,朱凯,万子益,等.桂黔滇毗邻地区红土型金矿地质特征与赵矿选区研究.2001:1-98
[71]郑荣才,张锦泉.滇东黔西南泥盆纪构造格局及岩相古地理演化.成都地质学院学报,1989,1(1):51-60
[72]吴怡.广西泥盆纪火山岩及其分布特征.广西地质,1991,4(4):17-26
[73]吴浩若,邝国敦,王忠诚.桂西北晚古生代基性岩的再认识及其大地构造意义,地质科学,1993,28:288-289
[74]吴浩若,邝国敦,王忠诚.广西晚古生代构造沉积背景的初步研究.地质科学,1997,32:11-18
[75]云南地矿局.中华人民共和国区域地质调查报告富宁幅(1:20万).1978
[76]钟大赉,吴根耀,季建清,等.滇东南发现蛇绿岩.科学通报,1998,43(13):1365-1370
[77]苏文超.杨子地块西南缘卡林型金矿成矿流体地球化学研究[博士论文]:贵阳:中国科学院贵阳地球化学研究所,2002
[78]宋谢炎,侯增谦,汪云亮,等.峨眉山玄武岩的地幔热柱成因.矿物岩石,2002,22(4):27-32
[79]张旗,钱青,王焰,等.扬子地块西南缘晚古生代急性岩浆岩的性质与古特提斯洋的演化.岩石学报,1999,15(4):576-583
[80]张成江,刘家铎,刘显凡,等.峨眉火成岩省成矿效应初探.矿物岩石,2004,24(1):5-9
[81]侯增谦,卢纪仁,汪云亮,等.峨眉火成岩省:结构、成因与特色.地质论评,1999,45(增刊):885-891
[82]Hu R Z,Su W C,Bi X W,et al.Geology and geochemistry of Carlintype gold deposits in China.Mineralium Deposita,2002,37:378-392
[83]Gill J B,Oregenic and plate tectonics.Berlin:Springer-Verlag,1981:358
[84]肖龙,徐义刚,梅厚钧,等.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系——地球化学证据.岩石学报,2003,19(1):38-48
[85]杨科佑,等.滇黔桂地区微细浸染型金矿成矿条件和矿床预测研究(科 研报告).1992
[86]谢学锦,刘大文,向运川,等.地球化学块体—概念和方法学的发展.中国地质,2002,29(3):225-233
[87]涂光炽,高振敏,胡瑞忠,等.分散元素地球化学及成矿机制.北京:地质出版社,2004.69-115
[88]李方夏.东南亚地质矿产与矿业经济.1995,52-138
[89]江鑫培.滇东南地区金矿类型及成矿地质条件分析.云南地质,1996,15(3):277-281
[90]杨云保.滇东南微细粒金矿成矿讨论.地质与勘探,2004,40(3):31-35
[91]李志伟,刘和林,钱祥贵.不整合界面及其后期转化在金矿成2矿中的意义-以滇黔桂毗邻区金矿为例.大地构造与成矿学,2000,24(增刊):52-57
[92]周余国,刘德利,刘继顺.滇东南曼龙沟金矿地质地球化学特征.地学前缘,2005,12(4):534
[93]焦玉凯.滇东南广南地区金矿床地质特征及成因研究.广西地质,2002,15(3):41-45
[94]吕世琨,李爱平,杨绍文,等.滇东南那能金矿带之断裂控矿.云南地质,2003,22(1):47-55
[95]云南省矿业协会黄金课题组.云南省黄金资源前景及开发战略部署研究.1992:65-125
[96]刘继顺,周余国,韩海涛,等.滇东南底圩金矿地质特征及找矿预测.吉林大学学报,2007,37(4):652-658
[97]国家辉,陈树旺,崔显德.金坝金矿床地质特征.地质与资源,2001a,10(2):71-79
[98]曾祥平.胜境关-东铺金矿矿田地质.云南地质,2003,22(1):39-46
[99]黄智龙,陈进,韩润生,等.云南会泽超大型铅锌矿床地球化学及成因—兼论峨眉山玄武岩与铅锌矿的关系.北京:地质出版社,2004.87-118
[100]於崇文,唐元骏,石平方,等.个旧锡-多金属成矿区内生成矿作用的动力学体系.武汉:中国地质大学出版社,1988.2-82
[101]官容生.滇东南构造岩浆带花岗岩体的含矿性探讨.矿物岩石,1991,11(1):92-101
[102]王新光,朱金初.个旧花岗岩的成因、演化及其成矿意义.大地构造与成矿学,1992,16(16):79-387
[103]俞开基.老君山锡多金属矿区地质概论.地质与勘探,1984,20(11):2-7
[104]李志群.个旧复式侵入岩体成岩系列研究.云南地质,1992,11(1):15-20
[105]高子英.蒙自白牛厂银多金属矿床的成矿作用.昆明:云南科技出版社,1998.14-96
[106]张世涛,陈国昌.滇东南薄竹山复式岩体的地质特征及其演化规律.云南地质,1997,222-230
[107]涂光炽.西南秦岭与西南贵州铀金成矿带及其与美国西部卡林型金矿的类似性.铀矿地质,1990,6(6):321-325
[108]马振东,李艳霞.沉积改造型矿床的物源及富集机制的地球化学研究.矿床地质,1999,18(2):110-120
[109]毛景文,李红艳,王登红.华南地区中生代多金属矿床形成与地幔柱关系.矿物岩石地球化学通报,1998,19(2):110-120
[110]李余华.滇东南金成矿区资源信息集成于靶区圈定:[工程硕士论文].昆明:昆明理工大学,2005
[111]韦龙明,卢汉堤,刘东升,等.卡林型金矿床稀土元素地球化学.矿产与地质,1995,9(50):487-492
[112]国家辉.金坝金矿床成矿作用探讨及找矿条件、标志分析.地质与资源,2001b,10(3):153-161
[113]靳是琴,李鸿超.成因矿物学(下).长春:吉林大学出版社,1984.32-50
[114]邵洁涟.金矿找矿矿物学.武汉:中国地质大学出版社,1988.1-72
[115]贾大成,胡瑞忠.滇黔桂地区卡林型金矿成因探讨.矿床地质,2001,20(4):379-383
[116]李振海,王国田,陈尚迪,等.广西金牙金矿床地质特征及成因.刘东升主编,中国卡林型(微细浸染型)金矿.南京:南京大学出版社,1994.37-78
[117]Chung S L,John B M.Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary.Geology,1995,23:889-892
[118]Song X Y,Zhou M,Hou Z Q,Cao Z M,et al.Geochemical Constraints on the Mantle Source of the Upper Permian Emeishan Continental Flood Basalts,Southwester China.Inter geol rev,2001,43:213-225
[119]Xu Y G,Chung S L,Jahn B M,et al.Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwester China.Lithos,2001,58:145-168
[120]黄智龙,陈进,刘丛强,等.峨眉山玄武岩与铅锌成矿:以云南会泽铅锌矿为例.矿物学报,2001,31(4):691-688
[121]迟清华.岩石化学元素丰度在地球化学块体研究中的意.物探与化探,2003,27(6):428-431
[122]鄢明才,迟清华.中国东部地壳与岩石的化学组成.北京:科学出版社,1997.11-155
[123]刘大文,向运川,连长云,等.水系沉积物中的金属元素在中国东部不同构造单元的分布特征.地质与勘探,2002,38(增刊):156-163
[124]黎应书,秦德先,党玉涛,等.锡矿床与基性岩超基性岩的关系探讨.中国工程科学,2005,7(增刊),269-274
[125]殷成玉,邓燕芷,马洁,等.个旧锡矿金银的赋存状态即赋存规律.云南地质,1990,9(7):65-74
[126]黎应书.云南个旧玄武岩及其成矿作用研究:[博士学位论文].昆明:昆明理工大学,2005
[127]李家和.个旧含金矽卡岩矿床.西南矿产地质,1990,4(4):66-73
[128]刘凤山,石准立.国外岩浆热液成矿理论研究现状与进展.地质科技情报,1994,13(2):75-81
[129]阮天建,朱有光,地球化学找矿.北京:地质出版社,1985.45-58
[130]李文达.华南红土化作用地球化学及红土型金矿形成的可能性.北京:地质出版社,1995
[131]陈守金,等.中国南方不可忽视的金矿新类型-红土型金矿.矿产资源定量预测及勘查评价,1999
[132]潘锦.红土化作用国际讨论会.地质科技动态,北京:中国科学院,1982
[133]黄镇国,张伟强,陈俊鸿,等.中国南方红色风化壳.北京:海洋出版社,1996
[134]郎光武,龙学耀.滇东南地区岩溶型砂金矿床的产出特征及找矿方向.云南地质,1996,15(4):351-358
[135]刘英俊,曹励明,李兆麟,等.元素地球化学.北京:科学技术出版社,1984.1-517
[136]韦龙明,刘鸾玲.中国卡林型金矿床金的赋存状态研究.地质与勘探,1995,31(6):31-35
[137]Drews Armitage S P,Rornberger S B,Whitney C G.Clay alteration and gold deposition in the genesis of Blue star deposits,Eurka County,Nevada,Econ. Geol.,1996,91:1383-1393
[138]刘建明.评《低温地球化学》.自然科学进展,1999,9,3:283-285
[139]何立贤,曾若兰,林立清.贵州金矿地质,北京:地质出版社,1993
[140]Disnar J R,Sureau J F.Organic matter in ore genanic.Progress and perapectives.Organic Geochemistry,1990,16(1-3):577-599
[141]Gize A P,Manning D A.Aspects of the organic geochemistry and petrology of metalliferous ores.In:Engel M H Macko,S A(eds.),Organic Geochemistry.New York:Plenum Press,1993.565-580
[142]李九玲,亓锋,徐庆生.微细浸染型(卡林)型金矿成矿过程中碳和有机质的作用.矿床地质,1996,15(3):193-206
[143]向才富,庄兴国,张文淮,等.成矿流体运移的输导体系研究-以右江地区微细浸染型金矿为例.地质科技情报,2000,19(4):65-69
[144]向才富,庄兴国,陆有明,等.有机流体成矿作用与古油藏成藏作用的相互耦合-以右江盆地微细浸染型金矿为例.地球科学—中国地质大学学报,2002,27(1):35-39
[145]向才富,胡建武.右江盆地流体运移过程中成矿与成藏作用.地球学报,2003,24(5):423-428
[146]顾学祥,李葆华,徐仕海,等.右江盆地含油气成矿流体性质及其成藏-成矿作用.地学前缘,2007,14(5):133-146
[147]傅家谟,贾蓉芬,刘德汉,等.碳酸盐有机地球化学.北京:科学出版社,1989.1-23
[148]张金亮,常象春.金顶Pb、Zn矿床油气地球化学特征及其成矿作用探讨.青岛海洋大学学报,2003,33(2):264-274
[149]张起钻.广西大厂锡多金属矿田100号矿体地质特征及成矿机理探讨.矿产与地质,1999,13(6):542-547
[150]陈广坡,徐国盛,王天奇,等.论油气成藏与金属成矿的关系及综合勘探.地学前缘,2008,15(2):200-206
[151]李惠.金矿床地球化学异常评价.吴昌荣编,地球化学异常评价文集,1989:108-109
[152]R.G.罗伯茨.矿床模式讲座(十一):太古宙岩金矿床.国外地质科技,1988.3:1-17
[153]程裕淇,陈毓川,赵一鸣,等.初论矿床的成矿系列问题.中国地质科学院院报,1979,第1号,37-58
[154]程裕淇,陈毓川,赵一鸣,等.再论矿床的成矿系列问题.地质论评, 1983,(6):1-33
[155]翟裕生.成矿系列研究问题.现代地质,1992,6(3):301-308
[156]章少华,蔡克勤.成矿系列研究若干问题讨论.地质论评,1993,39(5):404-411
[157]陈毓川.矿床成矿系列.地学前缘,1994,1(3～4):90-93
[158]王世称,陈永清.成矿系列预测的基本原则及特点.地质找矿论丛,1994,9(4):79-85
[159]陈毓川.矿床的成矿系列研究现状与趋势.地质与勘探,1997,33(1):21-25
[160]翟裕生,姚书振,崔彬,等.成矿系列研究.武汉:中国地质大学出版社,1996.192
[161]翟裕生,邓军,李小波.区域成矿学.北京:地质出版社,1999.154-171
[162]陈昌勇.成矿系列研究现状及展望.昆明理工大学学报,1997,22(2):12-16
[163]陈从喜,沈宝琳,蔡克勤.矿床成矿系列研究评述.建材地质,1997,5:3-8
[164]陈从喜,沈宝琳.矿床成矿系列研究的若干问题与方向.地质论评,1998,44(6):596-602
[165]程裕淇,宋天锐.关于中国矿床成矿系列.国外矿床地质,1995,(4):4-5
[166]陈毓川,裴荣富,宋天锐.中国矿床成矿系列初论.北京:地质出版社,1998.1-14
[167]谭运金.矿床地球化学类型与成因类型和成矿系列的关系.中国钨业,2000,15(2):16-20
[168]谈树成.个旧锡-多金属矿床成矿系列研究:[博士学位论文].昆明:昆明理工大学,2004
[169]卢作祥,范永香,刘辅臣,等.成矿规律和成矿预测学.武汉:中国地质大学出版社,1989.1-245
[170]D.P考克斯,D.A.矿床模式.北京:地质出版社,1990.1-378
[171]张贻侠.矿床模型导论.北京:地质出版社,1993.162-170
[172]R.V.Kirkham,W.D.Sinclair,R.I.Thorpe et al.Mineral Deposit Modeling.Geological Association of Canada Special Paper 40,1993" 1-493
[173]Thomas M D,Parkhill M.Gravity and magnetic prospecting for massive sulfide deposits.Atlantic Geology,1996,32(1):87-88
[174]张均.矿床定位预测的研究现状与趋向.地球科学进展,1997,12(3):242-246
[175]Cooke D R,Large R R.Practical uses of chemical modeling:difining new exploration in sedimentary basins.A GSO J,Australian Geology and Geophysics,1998,17(4):259-275
[176]翟裕生.走向21世纪的矿床学.矿床地质,2001,20(1):10-14
[177]翟裕生.论成矿系统.地学前缘.1999,6(1):13-27
[178]王仰之.中国地质学简史.北京:中国科学技术出版社,1994,1-23
[179]朱裕生.矿产预测理论-区域成矿学向矿产勘查延伸的理论体系.地质学报,2006,80(10):1518-1527
[180]刘石年.成矿预测学.长沙:中南大学出版社,1993.1-25
[181]秦德先.个旧锡矿地矿床成因与找矿新发现.昆明理工大学学报(理工版),2001,26(6):38
[182]秦德先,谈树成,范柱国,等.个旧-大厂地区地质构造演化及锡多金属成矿.矿物学报,2004,24(2):117-123
[183]翟裕生.成矿系统研究的思维与方法-地球系统、成矿系统到勘查系统.全国固体矿产勘查理论与技术方法高级培训班教材,北京:中国矿业联合会地质勘察协会,2007.1-58
[184]郑有业,高顺宝,张大全.西藏朱诺斑岩铜矿发现的重大意义及启示.地学前缘,2006,13(4):233-239
[185]郭令智,钟志洪,王良书,等.莺歌海盆地周边区域构造演化.高校地质学报,2001,7(1):1-12
[186]王承书.东南亚的活动俯冲和碰撞.沉积与特提斯地质,2002,22(1):92-112
[187]谈树成,秦德先,陈爱兵,等.个旧锡矿区区域地壳演化与成矿探讨.2004,矿物学报,24(6):157-163
[188]梅燕雄,朱裕生,叶锦华.中国超大型矿床的若干统计特征.地球学报,1997,18(4):358-366
[189]方维萱,胡瑞忠,苏文超,等.初论特提斯构造域一些大型-超大型金属矿床集中区聚矿构造.矿物岩石地球化学通报,2000,19(4):409-413
[1]Radtke,A.S.Geology of the Carlin gold deposit,Nevada:USGS openfile.1981,187:81-97
[2]Cox,D.P.and Singer,D.A.,Grade and tonnage model of distal disseminated Ag-Au,in Bliss,J.D.,ed.,Developments in mineral deposit modeling:U.S.Geological Survey Bulletin,2004,1992,p.20-22.
[3]Zhiping Li,Stephen G.Peters,Comparative Geology and Geochemistry of Sedimentary-Rock-Hosted(Carlin-Type) Gold Deposits in the People's Republic of China and in Nevada,USA,U.S.DEPARTMENT OF THE INTERIOR,U.S.GEOLOGICAL SURVEY,1998,1-12
[4]Lewis Teal,Mac Jackson,Geologic Overview of the Carlin Trend Gold Deposits and Descriptions of RecentDeep Discoveries,CARLIN-TYPE GOLD DEPOSITS FIELD CONFERENCE Edited by Peter Vikre,Tommy B.Thompson,Keith Bettles et al.,SOCIETY OF ECONOMIC GEOLOGISTS,1997:3-37
[5]王登红.卡林型金矿找矿新进展及其意义.地质地球化学,2000,28(1):92-94.
[6]谭延松.石峡微细浸染型金矿金的赋存状态及其回收预测.地质与勘探,1980(9):
[7]王学求.矿产勘查地球化学:过去的成就与未来的挑战.地学前缘,2003,10(1):239-246
[8]张复新,侯俊富,张存旺,等.甘肃阳山超大型卡林—类卡林型复合式金矿床特征.中国地质,2007,34(6):1062-1072
[9]A.S.拉德克.卡林金矿地质学.贵州省地质矿产局科技情报室,1987,57-72
[10]韦永福,吕英杰,等.中国金矿床.北京:地震出版社,1994.39-49
[11]李舒,李景春,卲军,等.中国金矿床工业类型及其特征.北京:地震出版社,1999.1-8
[12]陈毓川,李兆鼎,母瑞身,等.中国金矿床及其成矿规律.北京:地质出版社.2001.2-11
[13]刘东升,谭运金,王建业,等.中国卡林型(微细浸染型)金矿.南京:南京大学出版社,1994.1-36
[14]张贻侠,寸珪,刘连登,等.中国金矿床进展与思考.北京:地质出版社,1996.10-21
[15]波利申科,纳乌莫夫,巴甫洛娃,等.卞善涛,蒋琪,译.金—汞矿床:矿床类型、分布规律和成因模式.云南地质,2006,25(1):45-52
[16]Stephen G.Peters,Huang Jiazhan,Li Zhiping,et al.Introduction to and Classification of Sedimentary Rock-Hosted Au Deposits in P.R.China.USGS,2002:26-43
[17]Mao J,Qiu Y,Goldfarb,et al.Geology,distribution,and classification of Gold deposits in the western Qinling belt,China.Min Dep,2002,37:352-377
[18]A.H.Hofstra,P.Emsbo,W.D.Christiansen,et al,Source of ore fluids in Carlin-type gold deposits,China:Implications for genetic models,Mineral Deposit Research:Meeting the Global Challenge,Proceedings of the Eighth Biennial SGA Meeting,Beijing,China,18-21 August 2005:533-536
[19]刘继顺,舒广龙,高珍权.鄂东丰山矿田卡林型金矿地质地球化学特征.地学前缘,2004,11(2):379-385
[20]Herzig P M,Hannington M D.Polymetallic massive sulfides at the modern seafloor-areview.Ore Geol Rev,1995,10:95-115
[21]李朝阳.有关卡林型金矿的几点认识.矿物学报,1995,15(2):132-137
[22]涂光炽.低温地球化学.北京:科学出版社,1996.1-202
[23]王可勇,姚书振,吕新标.国内外微细浸染型金矿床研究现状及发展趋势.贵金属地质,2000,9(4):223-228
[24]Kuehn C.A.,Rose A.W.Carlin gold deposit.Nevada:Origin in a deep zone of mixing between normally pressured and overpressured fluids,Ec onomic,Geology,1995,90:17-36
[25]Sillitoe R.H.,Bonham H.F.Sediment-hosted gold deposits;distal products of magmatic-hydrothermal systems.Geology.1990;18:157-161
[26]谭运金.滇黔桂地区微细粒浸染型金矿床的地球化学类型.矿床地质,1994,13(4):308-321
[27]侯宗林,杨庆得.滇黔桂地区微细浸染型金矿成矿条件及成矿模式.地质找矿论丛,1989,4(3):1-11
[28]万兵.滇黔桂三角区金(银)矿床地质特征及成矿条件.矿产与地质,1991,5(3):169-172
[29]张兴余译.碳酸盐岩为主岩的浸染型金矿床形成模式.国外铀矿地质,1998,(2):12-18
[30]Nessbitt B E.Gold deposit continuum:A genetic model for lode Au mineralization in the continental crust.Geology,1988,16:1044-1048
[31]王登红,林文蔚,杨建民,等.试论地幔柱对我国两大金矿集中区的控制意义.地球学报,1999,20(2):157-162
[32]高振敏,李红阳,杨竹森,等.滇黔地区主要类型金矿的成矿与找矿.北京:地质出版社,2002.30-58
[33]Wang G Z,Hu R Z,Su W C,et al.Fluid flow and mineralization of Youjiang Basin in the Yunnan-Guizhou-Guangxi area,China.SCIENCE IN CHINA(Series D),2003,Vol.46 Supp:99-109
[34]周余国,刘继顺,王作华,等.从滇黔桂“金三角”区域地层地球化学特征探讨卡林型金矿的物质来源.地学前缘,2009,16(2):1-10
[35]张秋明译.矿床模式(九):浸染型金矿床.国外矿产地质,1987,(1):1-4
[36]汪东坡,邵世才,徐勇.金矿化过程中两个地球化学问题探讨.地球科学—中国地质大学学报,1999,24(3):292-296
[37]汪东波.金与铅锌矿化的关系.矿床地质,1998,17(增刊):345-348
[38]刘家军,刘建明,顾雪详,等.黔西南微细浸染型金矿的喷流沉积成因.科学通报,42卷:2126-2127
[39]刘家军,郑明华,顾雪祥,等.海底喷流作用对金富集成矿的意义.矿产与地质,1997,11(5):289-295
[40]周余国,刘继顺,欧阳玉飞,等.卡林型金矿的再定义.黄金,2008,29(11):7-11
[41]谢学锦.区域化探全国扫面积划.物化探研究报导,1978,3:28-36
[42]王淑玲.世界矿产资源年评2003:金.国土资源部信息中心编:183-194
[43]杨科佑,等.滇黔桂及川西北卡林型金矿.中国科学院黄金科技工作领导小组办公室编,中国金矿研究新进展.北京:地震出版社,1994.284-350
[44]周永峰.区域重力资料研究在广西深部地质和成矿预测中的应用.广西地质,1993,2
[45]黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,51(2):117-135
[46]张文佑.中国及邻区海陆大地构造图.北京:科学出版社,1983
[47]张文佑.断块构造导论.北京:石油出版社,1984
[48]任纪舜,姜春发,张正坤,等.中国大地构造及其演化.北京:科学出版社,1980:1-124.
[49]广西壮族自治区地质矿产局.广西壮族自治区区域地质志.北京:地质出版社,1985:1-853
[50]柳淮之,钟自云,姚明,等.右江裂谷带初探.桂林冶金地质学院学报, 1986,6(1):9-19
[51]王鸿桢.中国华南地区地壳构造发展的轮廓—华南地区古大陆边缘构造史.武汉:武汉地质学院出版社,1986.1-15
[52]刘本培.华南地区海西印支阶段构造带地理格局//王鸿桢,杨巍然,刘本培.华南地区古大陆边缘构造史.武汉:武汉地质学院出版社.1986
[53]许靖华,孙枢,李继亮.是华南造山带而不是华南地台.中国科学(B),1987,10:1107-1115
[54]王宝禄,郭富达,何邵麟,等.华南地区物探化探遥感成果编图/黔桂滇重点片综合解释成果报告.地矿部华南地区物探化探遥感编图委员会滇黔桂重点片综合解译组,1995,1-180
[55]朱炳泉,常向阳,邱华宁,等.地球化学急变带的元古宙基底特征及其与超大型矿床产出的关系.中国科学(D辑),1998a,28(增刊):63-70
[56]朱炳泉,常向阳.地球化学省与地球化学边界.地球科学进展,2001,16(2):153-162
[57]朱炳泉.壳幔化学不均一性与块体地球化学边界研究.地学前缘,1998,5(1、2):72-82
[58]梅冥相,马永生,邓军.加里东运动构造古地理及滇黔桂盆地的形成.地学前缘,2005,3:227-236
[59]陈旭等,戎嘉余,周志毅,等.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升.科学通报,2001,46(12):1052-1056
[60]苏文博.上扬子地台东南缘奥陶纪层序地层及海平面变化研究.北京:地质出版社,2001.1-106
[61]马文璞.区域构造解析-方法理论和中国板块构造.北京:地质出版社,1992.1-308
[62]章雨旭.地质学研究中常见逻辑方面的问题分析.高校地质学报,2006,12(1):147-152
[63]赵自强,丁启秀.中南区区域地层.武汉:中国地质大学出版社,1996:71-118
[64]曾允孚,张锦泉,刘文均,等.中国南方泥盆纪岩相古地理与成矿作用.北京:地质出版社,2001:1-120
[65]梅冥相,马永生,戴少武,等.南盘江盆地晚古生代盆地充填序列特征及生储盖组合划分.现代地质,2001,15(1):74-82
[66]梅冥相,马永生,高金汉,等.滇黔桂盆地及其邻区晚古生代层序地层格架及相对海平面变化.现代地质,2002,16(4):365-373
[67]梅冥相,李仲远.滇黔桂地区晚古生代至三叠纪盆层序地层序列及沉积盆地演化.现代地质,2004,18(4):555-563
[68]吴浩若.晚古生代-三叠纪南盘江海的构造古地理问题.古地理学报,2003,5(1):63-74
[69]章正军,丁俊,赵珉.滇东南及邻区晚古生代-中生代沉积盆地演化及微细粒型金矿成矿作用分析.云南地质,1996,15(3):282-288
[70]翟佑华,朱凯,万子益,等.桂黔滇毗邻地区红土型金矿地质特征与赵矿选区研究.2001:1-98
[71]郑荣才,张锦泉.滇东黔西南泥盆纪构造格局及岩相古地理演化.成都地质学院学报,1989,1(1):51-60
[72]吴怡.广西泥盆纪火山岩及其分布特征.广西地质,1991,4(4):17-26
[73]吴浩若,邝国敦,王忠诚.桂西北晚古生代基性岩的再认识及其大地构造意义,地质科学,1993,28:288-289
[74]吴浩若,邝国敦,王忠诚.广西晚古生代构造沉积背景的初步研究.地质科学,1997,32:11-18
[75]云南地矿局.中华人民共和国区域地质调查报告富宁幅(1:20万).1978
[76]钟大赉,吴根耀,季建清,等.滇东南发现蛇绿岩.科学通报,1998,43(13):1365-1370
[77]苏文超.杨子地块西南缘卡林型金矿成矿流体地球化学研究[博士论文]:贵阳:中国科学院贵阳地球化学研究所,2002
[78]宋谢炎,侯增谦,汪云亮,等.峨眉山玄武岩的地幔热柱成因.矿物岩石,2002,22(4):27-32
[79]张旗,钱青,王焰,等.扬子地块西南缘晚古生代急性岩浆岩的性质与古特提斯洋的演化.岩石学报,1999,15(4):576-583
[80]张成江,刘家铎,刘显凡,等.峨眉火成岩省成矿效应初探.矿物岩石,2004,24(1):5-9
[81]侯增谦,卢纪仁,汪云亮,等.峨眉火成岩省:结构、成因与特色.地质论评,1999,45(增刊):885-891
[82]Hu R Z,Su W C,Bi X W,et al.Geology and geochemistry of Carlintype gold deposits in China.Mineralium Deposita,2002,37:378-392
[83]Gill J B,Oregenic and plate tectonics.Berlin:Springer-Verlag,1981:358
[84]肖龙,徐义刚,梅厚钧,等.云南金平晚二叠纪玄武岩特征及其与峨眉地幔柱关系——地球化学证据.岩石学报,2003,19(1):38-48
[85]杨科佑,等.滇黔桂地区微细浸染型金矿成矿条件和矿床预测研究(科 研报告).1992
[86]谢学锦,刘大文,向运川,等.地球化学块体—概念和方法学的发展.中国地质,2002,29(3):225-233
[87]涂光炽,高振敏,胡瑞忠,等.分散元素地球化学及成矿机制.北京:地质出版社,2004.69-115
[88]李方夏.东南亚地质矿产与矿业经济.1995,52-138
[89]江鑫培.滇东南地区金矿类型及成矿地质条件分析.云南地质,1996,15(3):277-281
[90]杨云保.滇东南微细粒金矿成矿讨论.地质与勘探,2004,40(3):31-35
[91]李志伟,刘和林,钱祥贵.不整合界面及其后期转化在金矿成2矿中的意义-以滇黔桂毗邻区金矿为例.大地构造与成矿学,2000,24(增刊):52-57
[92]周余国,刘德利,刘继顺.滇东南曼龙沟金矿地质地球化学特征.地学前缘,2005,12(4):534
[93]焦玉凯.滇东南广南地区金矿床地质特征及成因研究.广西地质,2002,15(3):41-45
[94]吕世琨,李爱平,杨绍文,等.滇东南那能金矿带之断裂控矿.云南地质,2003,22(1):47-55
[95]云南省矿业协会黄金课题组.云南省黄金资源前景及开发战略部署研究.1992:65-125
[96]刘继顺,周余国,韩海涛,等.滇东南底圩金矿地质特征及找矿预测.吉林大学学报,2007,37(4):652-658
[97]国家辉,陈树旺,崔显德.金坝金矿床地质特征.地质与资源,2001a,10(2):71-79
[98]曾祥平.胜境关-东铺金矿矿田地质.云南地质,2003,22(1):39-46
[99]黄智龙,陈进,韩润生,等.云南会泽超大型铅锌矿床地球化学及成因—兼论峨眉山玄武岩与铅锌矿的关系.北京:地质出版社,2004.87-118
[100]於崇文,唐元骏,石平方,等.个旧锡-多金属成矿区内生成矿作用的动力学体系.武汉:中国地质大学出版社,1988.2-82
[101]官容生.滇东南构造岩浆带花岗岩体的含矿性探讨.矿物岩石,1991,11(1):92-101
[102]王新光,朱金初.个旧花岗岩的成因、演化及其成矿意义.大地构造与成矿学,1992,16(16):79-387
[103]俞开基.老君山锡多金属矿区地质概论.地质与勘探,1984,20(11):2-7
[104]李志群.个旧复式侵入岩体成岩系列研究.云南地质,1992,11(1):15-20
[105]高子英.蒙自白牛厂银多金属矿床的成矿作用.昆明:云南科技出版社,1998.14-96
[106]张世涛,陈国昌.滇东南薄竹山复式岩体的地质特征及其演化规律.云南地质,1997,222-230
[107]涂光炽.西南秦岭与西南贵州铀金成矿带及其与美国西部卡林型金矿的类似性.铀矿地质,1990,6(6):321-325
[108]马振东,李艳霞.沉积改造型矿床的物源及富集机制的地球化学研究.矿床地质,1999,18(2):110-120
[109]毛景文,李红艳,王登红.华南地区中生代多金属矿床形成与地幔柱关系.矿物岩石地球化学通报,1998,19(2):110-120
[110]李余华.滇东南金成矿区资源信息集成于靶区圈定:[工程硕士论文].昆明:昆明理工大学,2005
[111]韦龙明,卢汉堤,刘东升,等.卡林型金矿床稀土元素地球化学.矿产与地质,1995,9(50):487-492
[112]国家辉.金坝金矿床成矿作用探讨及找矿条件、标志分析.地质与资源,2001b,10(3):153-161
[113]靳是琴,李鸿超.成因矿物学(下).长春:吉林大学出版社,1984.32-50
[114]邵洁涟.金矿找矿矿物学.武汉:中国地质大学出版社,1988.1-72
[115]贾大成,胡瑞忠.滇黔桂地区卡林型金矿成因探讨.矿床地质,2001,20(4):379-383
[116]李振海,王国田,陈尚迪,等.广西金牙金矿床地质特征及成因.刘东升主编,中国卡林型(微细浸染型)金矿.南京:南京大学出版社,1994.37-78
[117]Chung S L,John B M.Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary.Geology,1995,23:889-892
[118]Song X Y,Zhou M,Hou Z Q,Cao Z M,et al.Geochemical Constraints on the Mantle Source of the Upper Permian Emeishan Continental Flood Basalts,Southwester China.Inter geol rev,2001,43:213-225
[119]Xu Y G,Chung S L,Jahn B M,et al.Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwester China.Lithos,2001,58:145-168
[120]黄智龙,陈进,刘丛强,等.峨眉山玄武岩与铅锌成矿:以云南会泽铅锌矿为例.矿物学报,2001,31(4):691-688
[121]迟清华.岩石化学元素丰度在地球化学块体研究中的意.物探与化探,2003,27(6):428-431
[122]鄢明才,迟清华.中国东部地壳与岩石的化学组成.北京:科学出版社,1997.11-155
[123]刘大文,向运川,连长云,等.水系沉积物中的金属元素在中国东部不同构造单元的分布特征.地质与勘探,2002,38(增刊):156-163
[124]黎应书,秦德先,党玉涛,等.锡矿床与基性岩超基性岩的关系探讨.中国工程科学,2005,7(增刊),269-274
[125]殷成玉,邓燕芷,马洁,等.个旧锡矿金银的赋存状态即赋存规律.云南地质,1990,9(7):65-74
[126]黎应书.云南个旧玄武岩及其成矿作用研究:[博士学位论文].昆明:昆明理工大学,2005
[127]李家和.个旧含金矽卡岩矿床.西南矿产地质,1990,4(4):66-73
[128]刘凤山,石准立.国外岩浆热液成矿理论研究现状与进展.地质科技情报,1994,13(2):75-81
[129]阮天建,朱有光,地球化学找矿.北京:地质出版社,1985.45-58
[130]李文达.华南红土化作用地球化学及红土型金矿形成的可能性.北京:地质出版社,1995
[131]陈守金,等.中国南方不可忽视的金矿新类型-红土型金矿.矿产资源定量预测及勘查评价,1999
[132]潘锦.红土化作用国际讨论会.地质科技动态,北京:中国科学院,1982
[133]黄镇国,张伟强,陈俊鸿,等.中国南方红色风化壳.北京:海洋出版社,1996
[134]郎光武,龙学耀.滇东南地区岩溶型砂金矿床的产出特征及找矿方向.云南地质,1996,15(4):351-358
[135]刘英俊,曹励明,李兆麟,等.元素地球化学.北京:科学技术出版社,1984.1-517
[136]韦龙明,刘鸾玲.中国卡林型金矿床金的赋存状态研究.地质与勘探,1995,31(6):31-35
[137]Drews Armitage S P,Rornberger S B,Whitney C G.Clay alteration and gold deposition in the genesis of Blue star deposits,Eurka County,Nevada,Econ. Geol.,1996,91:1383-1393
[138]刘建明.评《低温地球化学》.自然科学进展,1999,9,3:283-285
[139]何立贤,曾若兰,林立清.贵州金矿地质,北京:地质出版社,1993
[140]Disnar J R,Sureau J F.Organic matter in ore genanic.Progress and perapectives.Organic Geochemistry,1990,16(1-3):577-599
[141]Gize A P,Manning D A.Aspects of the organic geochemistry and petrology of metalliferous ores.In:Engel M H Macko,S A(eds.),Organic Geochemistry.New York:Plenum Press,1993.565-580
[142]李九玲,亓锋,徐庆生.微细浸染型(卡林)型金矿成矿过程中碳和有机质的作用.矿床地质,1996,15(3):193-206
[143]向才富,庄兴国,张文淮,等.成矿流体运移的输导体系研究-以右江地区微细浸染型金矿为例.地质科技情报,2000,19(4):65-69
[144]向才富,庄兴国,陆有明,等.有机流体成矿作用与古油藏成藏作用的相互耦合-以右江盆地微细浸染型金矿为例.地球科学—中国地质大学学报,2002,27(1):35-39
[145]向才富,胡建武.右江盆地流体运移过程中成矿与成藏作用.地球学报,2003,24(5):423-428
[146]顾学祥,李葆华,徐仕海,等.右江盆地含油气成矿流体性质及其成藏-成矿作用.地学前缘,2007,14(5):133-146
[147]傅家谟,贾蓉芬,刘德汉,等.碳酸盐有机地球化学.北京:科学出版社,1989.1-23
[148]张金亮,常象春.金顶Pb、Zn矿床油气地球化学特征及其成矿作用探讨.青岛海洋大学学报,2003,33(2):264-274
[149]张起钻.广西大厂锡多金属矿田100号矿体地质特征及成矿机理探讨.矿产与地质,1999,13(6):542-547
[150]陈广坡,徐国盛,王天奇,等.论油气成藏与金属成矿的关系及综合勘探.地学前缘,2008,15(2):200-206
[151]李惠.金矿床地球化学异常评价.吴昌荣编,地球化学异常评价文集,1989:108-109
[152]R.G.罗伯茨.矿床模式讲座(十一):太古宙岩金矿床.国外地质科技,1988.3:1-17
[153]程裕淇,陈毓川,赵一鸣,等.初论矿床的成矿系列问题.中国地质科学院院报,1979,第1号,37-58
[154]程裕淇,陈毓川,赵一鸣,等.再论矿床的成矿系列问题.地质论评, 1983,(6):1-33
[155]翟裕生.成矿系列研究问题.现代地质,1992,6(3):301-308
[156]章少华,蔡克勤.成矿系列研究若干问题讨论.地质论评,1993,39(5):404-411
[157]陈毓川.矿床成矿系列.地学前缘,1994,1(3～4):90-93
[158]王世称,陈永清.成矿系列预测的基本原则及特点.地质找矿论丛,1994,9(4):79-85
[159]陈毓川.矿床的成矿系列研究现状与趋势.地质与勘探,1997,33(1):21-25
[160]翟裕生,姚书振,崔彬,等.成矿系列研究.武汉:中国地质大学出版社,1996.192
[161]翟裕生,邓军,李小波.区域成矿学.北京:地质出版社,1999.154-171
[162]陈昌勇.成矿系列研究现状及展望.昆明理工大学学报,1997,22(2):12-16
[163]陈从喜,沈宝琳,蔡克勤.矿床成矿系列研究评述.建材地质,1997,5:3-8
[164]陈从喜,沈宝琳.矿床成矿系列研究的若干问题与方向.地质论评,1998,44(6):596-602
[165]程裕淇,宋天锐.关于中国矿床成矿系列.国外矿床地质,1995,(4):4-5
[166]陈毓川,裴荣富,宋天锐.中国矿床成矿系列初论.北京:地质出版社,1998.1-14
[167]谭运金.矿床地球化学类型与成因类型和成矿系列的关系.中国钨业,2000,15(2):16-20
[168]谈树成.个旧锡-多金属矿床成矿系列研究:[博士学位论文].昆明:昆明理工大学,2004
[169]卢作祥,范永香,刘辅臣,等.成矿规律和成矿预测学.武汉:中国地质大学出版社,1989.1-245
[170]D.P考克斯,D.A.矿床模式.北京:地质出版社,1990.1-378
[171]张贻侠.矿床模型导论.北京:地质出版社,1993.162-170
[172]R.V.Kirkham,W.D.Sinclair,R.I.Thorpe et al.Mineral Deposit Modeling.Geological Association of Canada Special Paper 40,1993" 1-493
[173]Thomas M D,Parkhill M.Gravity and magnetic prospecting for massive sulfide deposits.Atlantic Geology,1996,32(1):87-88
[174]张均.矿床定位预测的研究现状与趋向.地球科学进展,1997,12(3):242-246
[175]Cooke D R,Large R R.Practical uses of chemical modeling:difining new exploration in sedimentary basins.A GSO J,Australian Geology and Geophysics,1998,17(4):259-275
[176]翟裕生.走向21世纪的矿床学.矿床地质,2001,20(1):10-14
[177]翟裕生.论成矿系统.地学前缘.1999,6(1):13-27
[178]王仰之.中国地质学简史.北京:中国科学技术出版社,1994,1-23
[179]朱裕生.矿产预测理论-区域成矿学向矿产勘查延伸的理论体系.地质学报,2006,80(10):1518-1527
[180]刘石年.成矿预测学.长沙:中南大学出版社,1993.1-25
[181]秦德先.个旧锡矿地矿床成因与找矿新发现.昆明理工大学学报(理工版),2001,26(6):38
[182]秦德先,谈树成,范柱国,等.个旧-大厂地区地质构造演化及锡多金属成矿.矿物学报,2004,24(2):117-123
[183]翟裕生.成矿系统研究的思维与方法-地球系统、成矿系统到勘查系统.全国固体矿产勘查理论与技术方法高级培训班教材,北京:中国矿业联合会地质勘察协会,2007.1-58
[184]郑有业,高顺宝,张大全.西藏朱诺斑岩铜矿发现的重大意义及启示.地学前缘,2006,13(4):233-239
[185]郭令智,钟志洪,王良书,等.莺歌海盆地周边区域构造演化.高校地质学报,2001,7(1):1-12
[186]王承书.东南亚的活动俯冲和碰撞.沉积与特提斯地质,2002,22(1):92-112
[187]谈树成,秦德先,陈爱兵,等.个旧锡矿区区域地壳演化与成矿探讨.2004,矿物学报,24(6):157-163
[188]梅燕雄,朱裕生,叶锦华.中国超大型矿床的若干统计特征.地球学报,1997,18(4):358-366
[189]方维萱,胡瑞忠,苏文超,等.初论特提斯构造域一些大型-超大型金属矿床集中区聚矿构造.矿物岩石地球化学通报,2000,19(4):409-413