里伍铜锌矿床成因及找矿方向研究
|
摘要
里伍铜锌矿床位于四川省西部,地处康滇地轴西侧,松潘—甘孜造山带东南缘,北东向木里—锦屏弧形推覆构造带北西侧,属九龙—木罩变质—推覆复合构造元古宙铜锌多金属成矿带,为川西典型的中型富铜锌多金属矿床。
本文通过对研究区矿床地质特征分析,结合前人研究成果,认为江浪穹隆核部里伍群为里伍铜锌矿床的含矿岩层,含矿岩层为一套海相火山—浊流碎屑岩建造,其下盘紧贴变基性火山岩—次火山岩,显示出成矿作用与侵入岩体空间和成因上的关系。同位素与包裹体分析表明,里伍铜锌矿床成矿物质具多源性,中晚元古代弧后盆地环境下沉积的碎屑岩基础上叠加多次岩浆与构造变质作用,从而形成原始含矿层。成矿物质中的金属组分以深源为主,硫元素则主要来自上地幔,并混合有海水硫,成矿流体以岩浆水、变质水为主,后期混有海水、大气水,里伍铜锌矿床具典型的海相火山碎屑沉积—变质成因的特征。
里伍铜锌矿床位于江浪矿田外矿带,矿体呈似层状、透镜状,大体顺层或叠瓦状排列,显示受构造控制明显的特征。受区域构造旋回控制,里伍铜锌矿床成矿作用具多期次特征。结合同位素测年和矿物微相观察,将成矿作用划分为三个期次,其中,奥陶纪(471～473Ma)的构造运动导致区域发生大规模的海侵事件,形成一套陆源火山碎屑岩组成,为区域矿物质的重要沉积时期;印支晚期—燕山早期(184～191Ma)的松藩—甘孜造山运动使江浪变质核杂岩体隆升,为江浪变质核杂岩体的重要构造变形期,核杂岩体受东西向作用发生韧性变形,形成顺层滑脱带和褶皱带,为后期成矿热液体的运移和储存提供了良好的构造空间;133～143Ma为燕山中晚期的构造热液变质作用时期,是区域的重要成矿阶段。构造运动形成大量脆性断裂,岩层伸展变形并使前期的构造复活形成良好的容矿导矿构造,含矿流体在岩浆热驱动下与构造等多因素耦合而形成具有工业意义的硫化物矿床。
根据区域地质、物探、化探、遥异常等找矿标志,应用相似类比等原则认为里伍铜锌矿床的深部、外围,以及江浪变质核杂岩外围长枪等核杂岩体具有良好找矿远景。
The Liwu Cu-Zn deposit is a typical medium-sized polymetallic deposit in the west of Sichuan province,which located in the west of Kangdian Earth's axis,the south edge of Songpan-Granze orogen and the northwest of Muli-Jinping arc thrust tectonic zone,and the deposit is the part of paleoproterozoic Cu-Zn polymetallic metallogenic belt of Jiulong-Muli metamorphic-thrust complex zone.
Study on the geological characteristics of Liwu deposit and link with the former research fruit in the area,the paper indicated that Liwu group in the central portion of Jianglang dome tectonic is the ore-bearing layers of the deposit,which is a formation of marine volcanic-turbidite clastic rocks.The footwall of metamorphosed basic volcanic rocks-subvolcanic rocks indicates that the mineralization have relation with the space and the genesis of the intrusions.The paper indicates that the Liwu Cu-Zn deposit has polygenetic based on the research of isotope and fluid inclusions,the originality ore-bearing layers formed from Meso-Neoproterozoic clastic rocks which sedimented in the rear-arc basin environment,and have been effected by many Magmatic-tectonic movement later.The most ore matter are characterized with deep focus,the sulfur element derives from upper mantle and mixed with seawater sulfur latterly,the ore-forming fluid is composed mainly with magmatic water and metamorphic water,which mixed with seawater and atmospheric water little,the Liwu Cu-Zn deposit is featured with sea facies volcanic clastic-metamorphic genesis.
The Liwu Cu-Zn deposit is in the outside of Jianglang ore filed,the ore body are ranged bedding and imbricate which controlled by tectonic obviously.The mineralization which controlled by the tectonic gyration are featured with polyphase, and the mineralization are divided into three phases based on the isotope dating and the microphase research.The tectonic movement resulted in transgression in ordovician period(471～473Ma),and in this time there had a series volcano-clastic rocks sediment in the area.The late Indosinina-early Yanshan stage(184～191Ma) is the tectonic deformation era of the Jianglang metamorphic core complex,and in which time Jianglang metamorphic core complex uplifted by the Songpan-Granze orogen.Because of the east-west ductile deformation,there formed the surge belt and the drape belt which were the good tectonic space for ore fluid moving and depositing in the metamorphic core complex.The middle-late Yanshan stage(133～143Ma) is the most important phases of mineralization in which there had a lot of tectonic movement in the area.The extentional movement of the terrane relived the former ductile structure,and all the faulting were good for the movement and the deposit of the ore fluid,the ore fluid formed the industrial sulfide deposit when it coupling coexistence with structure and other factors.
According to the ore prospecting sign,such as regional geologic,geophysical exploration,chemical exploration,and Remote-sensing anomalies,and apply the comparability-analogy rules,it is thought that the areas,which are the deep and outskirts of Liwu Cu-Zc deposit,and Changqiang metamorphic core complex etc are the perspective area of mineral prospecting.
本文通过对研究区矿床地质特征分析,结合前人研究成果,认为江浪穹隆核部里伍群为里伍铜锌矿床的含矿岩层,含矿岩层为一套海相火山—浊流碎屑岩建造,其下盘紧贴变基性火山岩—次火山岩,显示出成矿作用与侵入岩体空间和成因上的关系。同位素与包裹体分析表明,里伍铜锌矿床成矿物质具多源性,中晚元古代弧后盆地环境下沉积的碎屑岩基础上叠加多次岩浆与构造变质作用,从而形成原始含矿层。成矿物质中的金属组分以深源为主,硫元素则主要来自上地幔,并混合有海水硫,成矿流体以岩浆水、变质水为主,后期混有海水、大气水,里伍铜锌矿床具典型的海相火山碎屑沉积—变质成因的特征。
里伍铜锌矿床位于江浪矿田外矿带,矿体呈似层状、透镜状,大体顺层或叠瓦状排列,显示受构造控制明显的特征。受区域构造旋回控制,里伍铜锌矿床成矿作用具多期次特征。结合同位素测年和矿物微相观察,将成矿作用划分为三个期次,其中,奥陶纪(471～473Ma)的构造运动导致区域发生大规模的海侵事件,形成一套陆源火山碎屑岩组成,为区域矿物质的重要沉积时期;印支晚期—燕山早期(184～191Ma)的松藩—甘孜造山运动使江浪变质核杂岩体隆升,为江浪变质核杂岩体的重要构造变形期,核杂岩体受东西向作用发生韧性变形,形成顺层滑脱带和褶皱带,为后期成矿热液体的运移和储存提供了良好的构造空间;133～143Ma为燕山中晚期的构造热液变质作用时期,是区域的重要成矿阶段。构造运动形成大量脆性断裂,岩层伸展变形并使前期的构造复活形成良好的容矿导矿构造,含矿流体在岩浆热驱动下与构造等多因素耦合而形成具有工业意义的硫化物矿床。
根据区域地质、物探、化探、遥异常等找矿标志,应用相似类比等原则认为里伍铜锌矿床的深部、外围,以及江浪变质核杂岩外围长枪等核杂岩体具有良好找矿远景。
The Liwu Cu-Zn deposit is a typical medium-sized polymetallic deposit in the west of Sichuan province,which located in the west of Kangdian Earth's axis,the south edge of Songpan-Granze orogen and the northwest of Muli-Jinping arc thrust tectonic zone,and the deposit is the part of paleoproterozoic Cu-Zn polymetallic metallogenic belt of Jiulong-Muli metamorphic-thrust complex zone.
Study on the geological characteristics of Liwu deposit and link with the former research fruit in the area,the paper indicated that Liwu group in the central portion of Jianglang dome tectonic is the ore-bearing layers of the deposit,which is a formation of marine volcanic-turbidite clastic rocks.The footwall of metamorphosed basic volcanic rocks-subvolcanic rocks indicates that the mineralization have relation with the space and the genesis of the intrusions.The paper indicates that the Liwu Cu-Zn deposit has polygenetic based on the research of isotope and fluid inclusions,the originality ore-bearing layers formed from Meso-Neoproterozoic clastic rocks which sedimented in the rear-arc basin environment,and have been effected by many Magmatic-tectonic movement later.The most ore matter are characterized with deep focus,the sulfur element derives from upper mantle and mixed with seawater sulfur latterly,the ore-forming fluid is composed mainly with magmatic water and metamorphic water,which mixed with seawater and atmospheric water little,the Liwu Cu-Zn deposit is featured with sea facies volcanic clastic-metamorphic genesis.
The Liwu Cu-Zn deposit is in the outside of Jianglang ore filed,the ore body are ranged bedding and imbricate which controlled by tectonic obviously.The mineralization which controlled by the tectonic gyration are featured with polyphase, and the mineralization are divided into three phases based on the isotope dating and the microphase research.The tectonic movement resulted in transgression in ordovician period(471～473Ma),and in this time there had a series volcano-clastic rocks sediment in the area.The late Indosinina-early Yanshan stage(184～191Ma) is the tectonic deformation era of the Jianglang metamorphic core complex,and in which time Jianglang metamorphic core complex uplifted by the Songpan-Granze orogen.Because of the east-west ductile deformation,there formed the surge belt and the drape belt which were the good tectonic space for ore fluid moving and depositing in the metamorphic core complex.The middle-late Yanshan stage(133～143Ma) is the most important phases of mineralization in which there had a lot of tectonic movement in the area.The extentional movement of the terrane relived the former ductile structure,and all the faulting were good for the movement and the deposit of the ore fluid,the ore fluid formed the industrial sulfide deposit when it coupling coexistence with structure and other factors.
According to the ore prospecting sign,such as regional geologic,geophysical exploration,chemical exploration,and Remote-sensing anomalies,and apply the comparability-analogy rules,it is thought that the areas,which are the deep and outskirts of Liwu Cu-Zc deposit,and Changqiang metamorphic core complex etc are the perspective area of mineral prospecting.
引文
[1]里伍矿区铜矿详细勘探地质报告[M],四川省地质局406地质队,1976,60-72.
[2]Liu Demin.Review of the basic characteristics of the metamorphic core complexs in China.Geoscience,2003,17(2):125-130.
[3]Song Honglin.An overview of metamorphic core complex-characteristics and origin[J].Earth SciFrontiers,1995,2(122):103-111.
[4]Song Honglin.Some characteristics of metamorphic core complexes[J].Geol Bull China,2002,21(4-5),193-97.
[5]Lister GS,Baldwin SL.Plutonism and the origin of metamorphic core complexes[J].Geology,1993,21..607-610.
[6]Wang Dezi,Shen Weizhou.Genesis of granitoids and crustal evolution in southeast China[J].Earth Sci Frontiers,2003,10(3):209-220.
[7]Zhang Jinjiang,Zheng Yadong.Review on the relationship between the formation of metamorphic core complexes and the magmatism[J].Geol Sci Techn Information,1998,17(1):19-25.
[8]翟裕生.构造—流体—成矿系统及其动力学的理论格架与方法体系[J].中国地质大学学报,2000,25(1):71-78.
[9]翟裕生,论成矿系统[J].地学前缘,1999,6(1):13-28.
[10]裕生,邓军,崔彬,等.成矿系统及综合地质异常[J].现代地质,1999,13(1):99-104.
[11]翟裕生,彭润民,邓军,王建平.成矿系统分析与新类型矿床预测[J].地学前缘,2000,7(1):123-130.
[12]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统[J].现代地质,1998,12(4):493-500.
[13]宋鸿林,田竟亚,颜丹平,等.扬子地台西缘江浪变质核杂岩体变形变质作用及里伍式铜矿成矿模式[R].中国地质大学,四川地质局404队.1995.2.
[14]姚家栋.李五式铜矿床成矿控制条什与找矿前景[J].四川地质学报,1991,11(1):29-36.
[15]颜丹平,宋鸿林,傅昭仁四川省九龙县江浪弯隆的变形变质作用与里伍铜锌矿床控矿构造模式[J].矿床地质,1994,13(增刊):120-121.
[16]傅昭仁,宋鸿林,颜丹平,等.扬子地台西缘江浪变质核杂岩结构及对成矿的控制[M].地质学报,1997.71(2):113-122.
[17]Yan Danping.New development in the research of metamorphic core complexes[J].Geol Sci Technlnformation,1997,16(3):13-19.
[18]Zhang Jiasheng.A review on late orogenic extension studies[J].Earth Sci Frontiers,1995,2(1-2):67-84.
[19]贾跃明.流体成矿系统与成矿作川研究[J].地学前缘,1996,3(4):253-258.
[20]Lou Fasheng,Shu Liangshu,Yu Jinhai,Wang Dezi.Petrological and geochemical characteristics and origin of the Wugongshan dome granite,Jiangxi province[J].Geol Rev,2002a,48(1):80-88.
[21]Wang Genhou,Zhou Xiang,Zeng Qinggao,etal.The structural study of the Kangma metamorphic core complexes in the Tibet[J].Chengdu University of Technology,1997,24(2):62-67.
[22]李人澍.成矿系统分析的理论与实践[M].地质出版社,1996.1-180.
[23]翟裕生.区域构造地球化学与成矿[J].区域调查与研究,2003,26(1):1-7.
[24]张荣华,胡书敏,张雪彤,苏艳丰.重要金属矿来源—迁移—堆积过程和化学动力学[M].北京:科学出版社,2006.
[25]Abers GA,Mutter CZ,Fang J.Shallow dips of normal faults during rapid extension earthquaks in the Woodlark2D Entrecasteaux rift system,Papua New Guinea[J].Geophys Research,1997,102:153012-15317.
[26]於崇文.成矿作用动力学—理论体系和方法论[J].地学前缘,1994,1(3):54-82.
[25]邓军,翟裕生,杨立强,等.剪切带构造—流体—成矿系统动力学模拟[J].地学前缘,1999.6(1):115-127.
[26]於崇文,岑况,鲍征宇,等.成矿作用动力学[M].北京:地质出版社,1998.1-230.
[27]李红阳,杨秋荣,李英杰.现代成矿理论[M].北京;地震出版社.2006,150-172.
[28]Avigad D,Garfunkel Z,Jolivet Let al.Back arc extension and denudation of Mediterranean eclogites[J].Tectonics,1997,16:924-941.
[29]Buck WR.Comment on Yin A"Origin of regional,rooted low-angle normal faults:a mechanical model and its tectonic implications"[J].Tectonics,1990,9:545-546.
[30]翟裕生.矿床地质学的发展前景和思维方法[J].地学前缘,1994,1(3):1-8.
[31]Barley ME,Groves DL.Supercontinent cycles and the distribution of metal deposits through time[J].Geology,1992,20:291-294.
[32]Armstrong R L.Cordilleran metamorphic core complexes-from Arizona to Southern Canada.Annu Rev[J].Earth Planet Sci,1982,10:129-154.
[33]Andersen T B.,Extensional tectonics in the Caledonides of southern Norway an overview[J].Tectonophysics,1998,285,333-351.
[34]翟裕生,中国区域成矿若干问题探讨[J].矿床地质,1999,18(4):323-332.
[35]颜丹平,宋鸿林,傅昭仁.扬子地台西缘江浪变质核杂岩的出露地壳剖面构造地层柱[J].现代地质,1997.1(3):290-297.
[36]刘肇昌,李凡友,钟康惠,等.扬子地台西缘构造演化与成矿[M].成都:电子科技大学出版社.1996.
[37]吴健民,刘肇昌,黎功举,等.扬子地台西缘铜矿床地质[M].北京:中国地质大学出版社.1998,1-271.
[38]唐高林,王发清,寇林林,里伍铜矿矿床地质特征及找矿前景[J].四川有色金属,2006,4:21-25.
[39]邹光富,汪名杰,李建忠,姚鹏,唐高林,李贵鸿.四川里伍铜矿区成矿规律与深部找矿[J].中国地质,2007,34(增):168-172.
[40]杜亚军,田竞亚.李伍铜矿床控矿构造地质特征及演化模式探讨[J].四川地质学报,1996,16(3):213-218.
[41]许志琴,侯立玮,傅小方,等.中国松潘—甘孜造山带的造山过程[M].北京:地质出版社,1992.
[42]冉崇英.康滇地轴东川式层状铜矿的沉积环境及成岩成矿作用[J].地球化学,1981,(2):114-119.
[43]李天福,蒋家申,陈贤胜.易门狮子山铜矿成矿环境及稀矿山式铁铜矿特征[J].云南地质,1996,15(2):192-204.
[44]冉崇英,张智筠,刘卫华,等.康滇裂谷旋迥与铜矿层楼结构及其地球化学演化[J].中国科学(B辑),1994,24(3):325-330.
[45]刘肇昌,钟康惠,李凡友,等.里伍矿床外围地区有色金属矿产资源找矿开发前景调查报 告[R].2001.1.
[46]冯孝良,汪名杰,文成敏,张惠华.浅析里伍铜矿外围找矿前景[J].沉积与特提斯,2007,27(1):9-37.
[47]李建忠,汪名杰,等.四川九龙黑牛洞铜矿床地质特征及其外围找矿方向初探[J].沉积与特提斯地质,2006,26(4):69-77.
[48]刘肇昌,钟康惠,李凡友,等.里伍外围石笋和大水沟及三垭瓦洛布地区铜铅锌地质找矿评价研究报告[R].20022.
[49]德先,田毓龙,燕永锋,等.云南易门狮子山铜矿的地球化学[J].地质学报,2000,74(1):72-84.
[50]刘俊思,阚泽忠,秦华中,曾祥贵.四川木里长枪穹隆石英流体包裹体特征及其地质意义[J].四川地质学报,2005,25(4):202-206.
[51]翟裕生,邓军,彭润民.矿床变化与保存的研究内容和研究方法[J].地球科学,2000,25(4):340-345.
[52]Kerrick R.The characteristics origins and dynamic setting of supergiant gold metallogenic provinces[J].Science in China(series D)supplement,2000,(4):1-81.
[53]Rose AW,Hawkes HE,Webb JS.Geochemistry in Mineral Exploration[M],New York,Academic Press,1979,657.
[54]Davis GH and Coney PJ.Geologic development of the Cordilleran metamorphic core complex.[J].Geology,7:120-124.
[55]顾连兴,汤晓茜,吴昌志,等.辽宁红透山块状硫化物矿床矿石糜棱岩铜金富集机制[J].地学前缘,2004,11(2):339～351.
[56]李紫金,傅昭仁,扬兆萍,等.四川九龙里伍型铜矿床地质概念模型[M].成都:四川科技出版社,1996.285-289.
[57]Malavieille JP.Kinematics ofcompressional and extensional ductile shearing deformation in a metamorphic core complex of the north-eastern Basin and Range[J].Struct Geol,1987,5-6:541-554.
[58]姚敬金,张素兰,曹落华,等.中国主要大型有色、贵金属矿床综合信息找矿模型[M].北京:地质出版社,2002.4-9.
[59]范永香,阳正熙.成矿规律与成矿预测[M].北京:中国矿业大学出版社,2005.147-150.
[60]何政伟,孙传敏,朱章森.搜索法——种无模型矿产预测的方法[J].矿物岩石,2000,20(3):81-37.
[61]何政伟.求同理论指导下的无模型预测[J].成都理工学院学报,1998,23(增):28-31.
[62]Zhu Zhicheng.Review on metamorphic core complex and extensional tectonic[J]Geol Sci Techn Information,11994,3(3):1-9.
[63]杨世瑜,王瑞雪.矿床遥感地质问题[M].昆明:云南大学出版社,2003.115-117.
[64]孙华山,,赵鹏大,张寿庭,夏庆霖.基于5P成矿预测与定量评价的系统勘查理论与实践[J].地球科学,2005,30(2):199-205.
[65]赵鹏大,陈建平,张寿庭.“三联式”成矿预测新进展[J].2003,10(2):453-462.
[66]ZHAO Pengda."Three2step"quantitative forecasting and assessment of resource—theory of digital exploration and discussion onpractice[J].Earth Science,2002,27(5):482-489
[67]CHEN Jianping,ZHANG Shouting,TANG Jun,etaI.Theoretical consideration to quantitative forecasting of nontraditional mineral resource[J].Progress in Geophysics,2002,17(2):342-348.
[68]ZHAO Pengda,CHEN Jianping,CHEN Jianguo.On diversity of mineralization and the spectrum of ore deposit[J]Earth Science,2001,26(2):111-117.
[69]孙华山,赵鹏大,张寿庭,夏庆霖.因子分析在成矿多样性定量化研究中的应用—以滇西北富碱斑岩矿产类型成矿多样性分析为例[J].成都理工大学学报,2005,32(1):82-86.
[70]张寿庭,赵鹏大,陈建平,徐旃章.多目标矿产预测评价及其研究意义[J].成都理工大学学报,2003,30(5):441-446.
[71]王锡华,李伟.红透山矿床变质岩系褶皱构造特征浅析[J].矿床与地质,2004,16(6):245-248.
[72]于凤金、王恩德.红透山式块状硫化物铜锌矿床古火山环境及与成矿关系研[J].矿产与地质,2005,19(1):12-14.
[73]于凤金.红透山式矿床成矿模式与找矿模型研究[D].沈刚:东北大学,2006.
[2]Liu Demin.Review of the basic characteristics of the metamorphic core complexs in China.Geoscience,2003,17(2):125-130.
[3]Song Honglin.An overview of metamorphic core complex-characteristics and origin[J].Earth SciFrontiers,1995,2(122):103-111.
[4]Song Honglin.Some characteristics of metamorphic core complexes[J].Geol Bull China,2002,21(4-5),193-97.
[5]Lister GS,Baldwin SL.Plutonism and the origin of metamorphic core complexes[J].Geology,1993,21..607-610.
[6]Wang Dezi,Shen Weizhou.Genesis of granitoids and crustal evolution in southeast China[J].Earth Sci Frontiers,2003,10(3):209-220.
[7]Zhang Jinjiang,Zheng Yadong.Review on the relationship between the formation of metamorphic core complexes and the magmatism[J].Geol Sci Techn Information,1998,17(1):19-25.
[8]翟裕生.构造—流体—成矿系统及其动力学的理论格架与方法体系[J].中国地质大学学报,2000,25(1):71-78.
[9]翟裕生,论成矿系统[J].地学前缘,1999,6(1):13-28.
[10]裕生,邓军,崔彬,等.成矿系统及综合地质异常[J].现代地质,1999,13(1):99-104.
[11]翟裕生,彭润民,邓军,王建平.成矿系统分析与新类型矿床预测[J].地学前缘,2000,7(1):123-130.
[12]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统[J].现代地质,1998,12(4):493-500.
[13]宋鸿林,田竟亚,颜丹平,等.扬子地台西缘江浪变质核杂岩体变形变质作用及里伍式铜矿成矿模式[R].中国地质大学,四川地质局404队.1995.2.
[14]姚家栋.李五式铜矿床成矿控制条什与找矿前景[J].四川地质学报,1991,11(1):29-36.
[15]颜丹平,宋鸿林,傅昭仁四川省九龙县江浪弯隆的变形变质作用与里伍铜锌矿床控矿构造模式[J].矿床地质,1994,13(增刊):120-121.
[16]傅昭仁,宋鸿林,颜丹平,等.扬子地台西缘江浪变质核杂岩结构及对成矿的控制[M].地质学报,1997.71(2):113-122.
[17]Yan Danping.New development in the research of metamorphic core complexes[J].Geol Sci Technlnformation,1997,16(3):13-19.
[18]Zhang Jiasheng.A review on late orogenic extension studies[J].Earth Sci Frontiers,1995,2(1-2):67-84.
[19]贾跃明.流体成矿系统与成矿作川研究[J].地学前缘,1996,3(4):253-258.
[20]Lou Fasheng,Shu Liangshu,Yu Jinhai,Wang Dezi.Petrological and geochemical characteristics and origin of the Wugongshan dome granite,Jiangxi province[J].Geol Rev,2002a,48(1):80-88.
[21]Wang Genhou,Zhou Xiang,Zeng Qinggao,etal.The structural study of the Kangma metamorphic core complexes in the Tibet[J].Chengdu University of Technology,1997,24(2):62-67.
[22]李人澍.成矿系统分析的理论与实践[M].地质出版社,1996.1-180.
[23]翟裕生.区域构造地球化学与成矿[J].区域调查与研究,2003,26(1):1-7.
[24]张荣华,胡书敏,张雪彤,苏艳丰.重要金属矿来源—迁移—堆积过程和化学动力学[M].北京:科学出版社,2006.
[25]Abers GA,Mutter CZ,Fang J.Shallow dips of normal faults during rapid extension earthquaks in the Woodlark2D Entrecasteaux rift system,Papua New Guinea[J].Geophys Research,1997,102:153012-15317.
[26]於崇文.成矿作用动力学—理论体系和方法论[J].地学前缘,1994,1(3):54-82.
[25]邓军,翟裕生,杨立强,等.剪切带构造—流体—成矿系统动力学模拟[J].地学前缘,1999.6(1):115-127.
[26]於崇文,岑况,鲍征宇,等.成矿作用动力学[M].北京:地质出版社,1998.1-230.
[27]李红阳,杨秋荣,李英杰.现代成矿理论[M].北京;地震出版社.2006,150-172.
[28]Avigad D,Garfunkel Z,Jolivet Let al.Back arc extension and denudation of Mediterranean eclogites[J].Tectonics,1997,16:924-941.
[29]Buck WR.Comment on Yin A"Origin of regional,rooted low-angle normal faults:a mechanical model and its tectonic implications"[J].Tectonics,1990,9:545-546.
[30]翟裕生.矿床地质学的发展前景和思维方法[J].地学前缘,1994,1(3):1-8.
[31]Barley ME,Groves DL.Supercontinent cycles and the distribution of metal deposits through time[J].Geology,1992,20:291-294.
[32]Armstrong R L.Cordilleran metamorphic core complexes-from Arizona to Southern Canada.Annu Rev[J].Earth Planet Sci,1982,10:129-154.
[33]Andersen T B.,Extensional tectonics in the Caledonides of southern Norway an overview[J].Tectonophysics,1998,285,333-351.
[34]翟裕生,中国区域成矿若干问题探讨[J].矿床地质,1999,18(4):323-332.
[35]颜丹平,宋鸿林,傅昭仁.扬子地台西缘江浪变质核杂岩的出露地壳剖面构造地层柱[J].现代地质,1997.1(3):290-297.
[36]刘肇昌,李凡友,钟康惠,等.扬子地台西缘构造演化与成矿[M].成都:电子科技大学出版社.1996.
[37]吴健民,刘肇昌,黎功举,等.扬子地台西缘铜矿床地质[M].北京:中国地质大学出版社.1998,1-271.
[38]唐高林,王发清,寇林林,里伍铜矿矿床地质特征及找矿前景[J].四川有色金属,2006,4:21-25.
[39]邹光富,汪名杰,李建忠,姚鹏,唐高林,李贵鸿.四川里伍铜矿区成矿规律与深部找矿[J].中国地质,2007,34(增):168-172.
[40]杜亚军,田竞亚.李伍铜矿床控矿构造地质特征及演化模式探讨[J].四川地质学报,1996,16(3):213-218.
[41]许志琴,侯立玮,傅小方,等.中国松潘—甘孜造山带的造山过程[M].北京:地质出版社,1992.
[42]冉崇英.康滇地轴东川式层状铜矿的沉积环境及成岩成矿作用[J].地球化学,1981,(2):114-119.
[43]李天福,蒋家申,陈贤胜.易门狮子山铜矿成矿环境及稀矿山式铁铜矿特征[J].云南地质,1996,15(2):192-204.
[44]冉崇英,张智筠,刘卫华,等.康滇裂谷旋迥与铜矿层楼结构及其地球化学演化[J].中国科学(B辑),1994,24(3):325-330.
[45]刘肇昌,钟康惠,李凡友,等.里伍矿床外围地区有色金属矿产资源找矿开发前景调查报 告[R].2001.1.
[46]冯孝良,汪名杰,文成敏,张惠华.浅析里伍铜矿外围找矿前景[J].沉积与特提斯,2007,27(1):9-37.
[47]李建忠,汪名杰,等.四川九龙黑牛洞铜矿床地质特征及其外围找矿方向初探[J].沉积与特提斯地质,2006,26(4):69-77.
[48]刘肇昌,钟康惠,李凡友,等.里伍外围石笋和大水沟及三垭瓦洛布地区铜铅锌地质找矿评价研究报告[R].20022.
[49]德先,田毓龙,燕永锋,等.云南易门狮子山铜矿的地球化学[J].地质学报,2000,74(1):72-84.
[50]刘俊思,阚泽忠,秦华中,曾祥贵.四川木里长枪穹隆石英流体包裹体特征及其地质意义[J].四川地质学报,2005,25(4):202-206.
[51]翟裕生,邓军,彭润民.矿床变化与保存的研究内容和研究方法[J].地球科学,2000,25(4):340-345.
[52]Kerrick R.The characteristics origins and dynamic setting of supergiant gold metallogenic provinces[J].Science in China(series D)supplement,2000,(4):1-81.
[53]Rose AW,Hawkes HE,Webb JS.Geochemistry in Mineral Exploration[M],New York,Academic Press,1979,657.
[54]Davis GH and Coney PJ.Geologic development of the Cordilleran metamorphic core complex.[J].Geology,7:120-124.
[55]顾连兴,汤晓茜,吴昌志,等.辽宁红透山块状硫化物矿床矿石糜棱岩铜金富集机制[J].地学前缘,2004,11(2):339～351.
[56]李紫金,傅昭仁,扬兆萍,等.四川九龙里伍型铜矿床地质概念模型[M].成都:四川科技出版社,1996.285-289.
[57]Malavieille JP.Kinematics ofcompressional and extensional ductile shearing deformation in a metamorphic core complex of the north-eastern Basin and Range[J].Struct Geol,1987,5-6:541-554.
[58]姚敬金,张素兰,曹落华,等.中国主要大型有色、贵金属矿床综合信息找矿模型[M].北京:地质出版社,2002.4-9.
[59]范永香,阳正熙.成矿规律与成矿预测[M].北京:中国矿业大学出版社,2005.147-150.
[60]何政伟,孙传敏,朱章森.搜索法——种无模型矿产预测的方法[J].矿物岩石,2000,20(3):81-37.
[61]何政伟.求同理论指导下的无模型预测[J].成都理工学院学报,1998,23(增):28-31.
[62]Zhu Zhicheng.Review on metamorphic core complex and extensional tectonic[J]Geol Sci Techn Information,11994,3(3):1-9.
[63]杨世瑜,王瑞雪.矿床遥感地质问题[M].昆明:云南大学出版社,2003.115-117.
[64]孙华山,,赵鹏大,张寿庭,夏庆霖.基于5P成矿预测与定量评价的系统勘查理论与实践[J].地球科学,2005,30(2):199-205.
[65]赵鹏大,陈建平,张寿庭.“三联式”成矿预测新进展[J].2003,10(2):453-462.
[66]ZHAO Pengda."Three2step"quantitative forecasting and assessment of resource—theory of digital exploration and discussion onpractice[J].Earth Science,2002,27(5):482-489
[67]CHEN Jianping,ZHANG Shouting,TANG Jun,etaI.Theoretical consideration to quantitative forecasting of nontraditional mineral resource[J].Progress in Geophysics,2002,17(2):342-348.
[68]ZHAO Pengda,CHEN Jianping,CHEN Jianguo.On diversity of mineralization and the spectrum of ore deposit[J]Earth Science,2001,26(2):111-117.
[69]孙华山,赵鹏大,张寿庭,夏庆霖.因子分析在成矿多样性定量化研究中的应用—以滇西北富碱斑岩矿产类型成矿多样性分析为例[J].成都理工大学学报,2005,32(1):82-86.
[70]张寿庭,赵鹏大,陈建平,徐旃章.多目标矿产预测评价及其研究意义[J].成都理工大学学报,2003,30(5):441-446.
[71]王锡华,李伟.红透山矿床变质岩系褶皱构造特征浅析[J].矿床与地质,2004,16(6):245-248.
[72]于凤金、王恩德.红透山式块状硫化物铜锌矿床古火山环境及与成矿关系研[J].矿产与地质,2005,19(1):12-14.
[73]于凤金.红透山式矿床成矿模式与找矿模型研究[D].沈刚:东北大学,2006.
© 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 |