内蒙古北山北带斑岩型矿床特征与成矿系统分析
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摘要
笔者运用成矿系统理论，从控制矿床形成及保存的全部地质要素和成矿作用过程等一般矿床学研究入手，从宏观上将成矿时间、空间、物质、运动等要素有机结合，对内蒙古北山北带会聚型陆缘斑岩成矿系统进行了分析研究。
通过对比研究认为，内蒙古北山北带为会聚型板块边缘，属于塔里木—哈萨克斯坦联合板块北部陆缘增生带。随着古亚洲洋板块消减于塔里木—哈萨克斯坦联合板块之下，古亚洲洋逐渐闭合，最终导致塔里木—哈萨克斯坦联合板块与西伯利亚板块发生陆陆碰撞造山。使北山北带成为了斑岩型矿床形成的有利地带。
本文对小狐狸山斑岩型钼多金属矿床等3个典型矿床进行了剖析，对比研究了小狐狸山等矿床级别的斑岩型成矿亚系统，提出该成矿亚系统成矿作用过程由成矿物质供应子系统、成矿流体子系统、成矿能量子系统、成矿空间子系统、矿床形成变化保存的时间子系统等5个子系统有机结合而成。
在剖析典型矿床的基础上总结了北山北带会聚型陆缘斑岩成矿系统各子系统的基本构成和总体特征；建立了北山北带区域性斑岩型矿床的成矿模式、区域矿化网络、区域成矿系统结构。
研究发现，本区北西西向、北西向断裂构造与北东向断裂构造相互交切形成的网格状构造组合构成了内蒙古北山北带区域矿化网络的主体格架，各构造节点具有明显的控岩控矿作用，目前已发现的矿床（点）均分布于网络格架的节点附近。
通过研究区域成矿规律和成矿区带的划分，总结了北山北带斑岩型矿床的六个找矿标志，初步建立了该类型矿床的找矿模型，确定了由面到点、由表及里、由浅入深、循序渐进的找矿思路，提出了该地区寻找斑岩型矿床的技术方法组合。
圈定了甜水井－流沙山钼、金、铜、铁找矿靶区、额勒根乌兰乌拉－乌珠尔嘎顺钼、铜、铁找矿靶区、高石山—小狐狸山铜、钼、金、铅、锌、稀有金属找矿靶区等3个找矿靶区，明确了各找矿靶区的主攻矿种及主攻矿床类型。为内蒙古北山北带今后的找矿工作提供了参考意见，体现了成矿系统理论与生产实践的有机结合。
This paper guided by the theory of Metallogenic System, started with generalstudy of mineral deposit, which included the essential geologic factors of controllingdeposits formation to preservation and metallogenic process. By integrated theelements of mineralization time, space, material, and transport, the authorcomprehensively discussed the porphyry metallogenic system in north belt of theBeishan Mountain, Inner Mongolia.
The north belt of the Beishan Mountain was convergent continental margin,which belonged to the northern margin accretion zone of Tarim-Kazakhstan joint plate.With the Paleo-Asian Ocean plate subducted to Tarim-Kazakhstan joint plate, thePaleo-Asian Ocean gradually closed, and eventual led to continent-continent collisionorogeny of the Tarim-Kazakhstan joint plate and the Siberian plate. This evolutionmade the north belt of the Beishan Mountain became a beneficial area ofporphyry-type deposits formation.
The author analyzed three typical deposits included Xiaohulishan porphyrymolybdenum polymetallic deposits, contrasted study of the deposit-level porphyrymetallogenic system like Xiaohulishan deposit, proposed that the mineralizationsystem was organic combined by the five subsystem: the metallogenic material supplysubsystem, the ore-forming fluid subsystem, the ore-forming energy subsystem, theore-forming spatial subsystem, and the post-ore change-preservation temporalsubsystem.
Based on the typical ore deposits study, the author summarized the basicstructure and general characteristics of each subsystem in the north belt of the BeishanMountain convergent continental margin metallogenic system, established theprospecting model, mineralization network, metallogenic system structure of theregional porphyry deposits in north belt of the Beishan Mountain.
The study results showed that NWW-NW and NE faults cross-cut to form agrid-like structure constituted the main framework of regional mineralization networkin the north belt of the Beishan Mountain, Inner Mongolia. Each structure joint wasbeneficial lithology and ore controlling place. All the discovered mineral deposits (orore occurrences) are located near the network framework.
After divided the regional metallogenic regularity and metallogenic belts, the author summed up six prospecting criteria of porphyry type deposits in north belt ofthe Beishan Mountain, preliminary established the prospecting model of this typedeposits, determined the“point to region, surface to depth, follow in proper sequence”prospecting idea, proposed the technical method in search of porphyry-type oredeposits in this area.
The author delineated three prospecting targets: Tianshuijing-LiushanshanMo-Au-Cu-Fe area, Erlegenwulawula-Wuzhuergashun Mo-Cu-Fe area andGaoshishan-Xiaohulishan Cu-Mo-Au-Pb-Zn-Rare Metal area, confirmed the mainmineral resources and ore deposits in each prospecting target. This study offers veryuseful reference for future prospecting work in north belt of the Beishan Mountain,and reflects the organic combination of the Metallogenic System and prospectingpractices.
通过对比研究认为，内蒙古北山北带为会聚型板块边缘，属于塔里木—哈萨克斯坦联合板块北部陆缘增生带。随着古亚洲洋板块消减于塔里木—哈萨克斯坦联合板块之下，古亚洲洋逐渐闭合，最终导致塔里木—哈萨克斯坦联合板块与西伯利亚板块发生陆陆碰撞造山。使北山北带成为了斑岩型矿床形成的有利地带。
本文对小狐狸山斑岩型钼多金属矿床等3个典型矿床进行了剖析，对比研究了小狐狸山等矿床级别的斑岩型成矿亚系统，提出该成矿亚系统成矿作用过程由成矿物质供应子系统、成矿流体子系统、成矿能量子系统、成矿空间子系统、矿床形成变化保存的时间子系统等5个子系统有机结合而成。
在剖析典型矿床的基础上总结了北山北带会聚型陆缘斑岩成矿系统各子系统的基本构成和总体特征；建立了北山北带区域性斑岩型矿床的成矿模式、区域矿化网络、区域成矿系统结构。
研究发现，本区北西西向、北西向断裂构造与北东向断裂构造相互交切形成的网格状构造组合构成了内蒙古北山北带区域矿化网络的主体格架，各构造节点具有明显的控岩控矿作用，目前已发现的矿床（点）均分布于网络格架的节点附近。
通过研究区域成矿规律和成矿区带的划分，总结了北山北带斑岩型矿床的六个找矿标志，初步建立了该类型矿床的找矿模型，确定了由面到点、由表及里、由浅入深、循序渐进的找矿思路，提出了该地区寻找斑岩型矿床的技术方法组合。
圈定了甜水井－流沙山钼、金、铜、铁找矿靶区、额勒根乌兰乌拉－乌珠尔嘎顺钼、铜、铁找矿靶区、高石山—小狐狸山铜、钼、金、铅、锌、稀有金属找矿靶区等3个找矿靶区，明确了各找矿靶区的主攻矿种及主攻矿床类型。为内蒙古北山北带今后的找矿工作提供了参考意见，体现了成矿系统理论与生产实践的有机结合。
This paper guided by the theory of Metallogenic System, started with generalstudy of mineral deposit, which included the essential geologic factors of controllingdeposits formation to preservation and metallogenic process. By integrated theelements of mineralization time, space, material, and transport, the authorcomprehensively discussed the porphyry metallogenic system in north belt of theBeishan Mountain, Inner Mongolia.
The north belt of the Beishan Mountain was convergent continental margin,which belonged to the northern margin accretion zone of Tarim-Kazakhstan joint plate.With the Paleo-Asian Ocean plate subducted to Tarim-Kazakhstan joint plate, thePaleo-Asian Ocean gradually closed, and eventual led to continent-continent collisionorogeny of the Tarim-Kazakhstan joint plate and the Siberian plate. This evolutionmade the north belt of the Beishan Mountain became a beneficial area ofporphyry-type deposits formation.
The author analyzed three typical deposits included Xiaohulishan porphyrymolybdenum polymetallic deposits, contrasted study of the deposit-level porphyrymetallogenic system like Xiaohulishan deposit, proposed that the mineralizationsystem was organic combined by the five subsystem: the metallogenic material supplysubsystem, the ore-forming fluid subsystem, the ore-forming energy subsystem, theore-forming spatial subsystem, and the post-ore change-preservation temporalsubsystem.
Based on the typical ore deposits study, the author summarized the basicstructure and general characteristics of each subsystem in the north belt of the BeishanMountain convergent continental margin metallogenic system, established theprospecting model, mineralization network, metallogenic system structure of theregional porphyry deposits in north belt of the Beishan Mountain.
The study results showed that NWW-NW and NE faults cross-cut to form agrid-like structure constituted the main framework of regional mineralization networkin the north belt of the Beishan Mountain, Inner Mongolia. Each structure joint wasbeneficial lithology and ore controlling place. All the discovered mineral deposits (orore occurrences) are located near the network framework.
After divided the regional metallogenic regularity and metallogenic belts, the author summed up six prospecting criteria of porphyry type deposits in north belt ofthe Beishan Mountain, preliminary established the prospecting model of this typedeposits, determined the“point to region, surface to depth, follow in proper sequence”prospecting idea, proposed the technical method in search of porphyry-type oredeposits in this area.
The author delineated three prospecting targets: Tianshuijing-LiushanshanMo-Au-Cu-Fe area, Erlegenwulawula-Wuzhuergashun Mo-Cu-Fe area andGaoshishan-Xiaohulishan Cu-Mo-Au-Pb-Zn-Rare Metal area, confirmed the mainmineral resources and ore deposits in each prospecting target. This study offers veryuseful reference for future prospecting work in north belt of the Beishan Mountain,and reflects the organic combination of the Metallogenic System and prospectingpractices.
引文
白瑾.造山带构造样式的恢复及其构造环境意义[J] .地质调查与研究,2003,26（1）:38-45
陈富文,李华芹,蔡红等.新疆东部金窝子金矿床成因讨论—同位素地质年代学证据[J].地质论评,1999,45（3）:247-254
陈毓川,裴荣富,宋天锐. 1998.年中国矿床成矿系列初论[M].北京,地质出版社
陈毓川主编. 1999.中国主要成矿区带矿产资源远景评价[M].北京,地质出版社
陈祖伊,张学权,张昭明等著.北山区域地质发展史和金矿区域成矿模式[Ｊ] .铀矿地质,1993,9（2）:65-75
程小珍,杨伦,张晓.内蒙古小东沟钼矿成矿地质条件分析[J].地质与勘探,2007,43(05),11-16
程裕淇,陈毓川等.初论矿床的成矿系列问题.中国地质科学院院报,1979,第1号
崔惠文,陈祖伊. 1996.甘肃北山地区金矿地质[Ｍ] .北京:地质出版社.
崔惠文.甘肃北山古岛弧期后张裂带[J].贵金属地质,1996,5（4）:306-314
杜安道,何红蓼,殷宁万等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347
冯铁全,左国朝,金松桥.北山窑洞努如—公婆泉岛弧火山岩岩石地球化学特征（摘要）[Ｊ].甘肃地质学报,1997,6（增刊）:23-24
龚全胜,刘明强,梁明宏等.北山造山带大地构造相及构造演化[Ｊ].西北地质,2003,36（1）:11-17
龚全胜,刘明强,李海林等.甘肃北山造山带类型及基本特征[Ｊ].西北地质,2002,35（3）:28-34
葛肖虹著.中亚大陆一次重要的板内会聚事件[Ｊ].地学前缘,1999,6(4):330
洪大卫,黄怀曾,肖宜君等.内蒙中部二叠纪碱性花岗岩及其地球动力学意义[Ｊ].地质学报,1994,68(3):219-230
洪大卫,王式光,谢锡林等.试析地幔来源物质成矿域—以中亚造山带为例[J].矿床地质,2003,22（1）:41-55
何建坤,刘金朝.下地壳流变与造山带同挤压期地壳伸展的动力学关系[J].地球物理学报,2002,45（4）:502-516
何国琦,李茂松,刘德权著. 1994.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社
黄崇轲,白冶,朱裕生等著. 2001.中国铜矿床[Ｍ].北京地质出版社
江思宏,聂凤军,陈文等著.北山明水地区花岗岩时代的确定及其地质意义[J].岩石矿物学杂志,2003,22（2）:107-111
雷洪平,徐玉麟著. 1984.内蒙古自治区额济纳旗流沙山钼矿区详细普查地质报告[R].甘肃省地质矿产局第四地质队.
李人澍.成矿系统分析的理论与实践. [M].地质出版社, 1996.
李述靖,张维杰,耿明山著.1998.蒙古弧地质构造特征及形成演化概论[M].北京:地质出版社.
李双林,欧阳自远.兴蒙造山带及邻区的构造格局与构造演化[J].海洋地质与第四纪地质,1998,18(3):45-54
李文国,姜万德,王惠等. 1996.内蒙古岩石地层[M].中国地质大学出版社
李景春,赵安生,崔惠文.北山北带地质构造特征[J].贵金属地质，1965（1）:59-68
李华芹,谢才富,常海亮. 1998 .新疆北部有色贵金属矿床成矿作用年代学[Ｍ].北京地质出版社
李奋其,王成善.甘肃公婆泉铜矿田地质特征和控矿因素分析[J].成都理工大学学报(自然科学版),2003,30（2）:120-125
梁明宏,龚全胜,李海林等.造山带花岗岩类型及填图方法的实践—以甘肃北山造山带为例.岩石矿物学杂志,2002,21（2）:174-178
刘明强,党引业,龚全胜.甘肃北山平头山逆冲推覆构造的特征.西北地质,2002,35（1）:22-27
刘雪亚,王荃.中国西部北山造山带的大地构造及其演化[Ｊ] .地学研究,1995,28:37-48
刘益康,徐叶兵.蒙古Oyu Tolgoi斑岩铜金矿的勘查[J].地质与勘探,2003,39 (1),1-4
吕志成.与危机矿山接替资源勘查有关的成矿找矿模式[J].矿床地质,2006,25 (增刊),439-442
吕志成,戴自希,蔺志永,彦廷杰.危机矿山接替资源找矿勘查相关成矿理论与技术方法[J].矿物岩石地球化学通报,23卷增刊,132-133.
毛景文,杨建民,屈文俊等.新疆黄山东铜镍硫化物矿床Ｒｅ-Ｏｓ同位素测定及其地球动力学意义[Ｊ] .矿床地质,2002,21(4),323-330
穆治国,刘驰,黄宝玲,侯贵廷,左国朝等.甘肃北山古生代造山带地壳演化的同位素和稀土元素地球化学特征[J] .北京大学学报(自然科学版),1994,30（2）:202-214
聂凤军,江思宏,白大明等. 2002.北山地区金属矿床成矿规律及找矿方向[M].地质出版社
聂凤军,江思宏,赵省民.内蒙古流沙山金(钼)矿床地质特征及矿床类型划分[J].地质地球化学,2002,30(1):1-7
聂凤军,江思宏,白大明等.北山中南带海西-印支期岩浆活动与金的成矿作用[J].地球学报，2003,24(5):415-422
聂凤军,江思宏,白大明等.蒙甘新相邻(北山)地区金铜矿床时空分布特征及成矿作用[J] .矿床地质,2003,22(3) :234-245
聂凤军,屈文俊,刘妍,杜安道,江思宏.内蒙古额勒根斑岩型钼(铜)矿化区辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,2005,24(6): 638-646.
彭振安,李红红,张诗启等.内蒙古北山地区小狐狸山钼矿成矿岩体地球化学特征研究[ J].地质与勘探,2010,46(2) : 291-299
彭振安,李红红,屈文俊等.内蒙古北山地区小狐狸山钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿床地质, 2010,29(3) : 510-516
潘启宇,沈鸿章,李文国等. 1991,内蒙古自治区区域地质志[M] .地质出版社.
秦克章,方同辉,王书来等.东天山板块构造分区、演化与成矿地质背景研究[J].矿床地质,2002,20（4）
芮宗瑶,黄宗轲,齐国民. 1984.中国斑岩铜(钼)矿床[M].地质出版社
芮琮瑶.2002.国内外斑岩型铜矿研究进展[M].中国地质调查局
司雪峰,崔银亮,穆新河.甘肃北山中带变质碎屑岩型金矿地质特征及找矿前景[J].地质与勘探,2001,37（6）:5-8
孙新春等.甘蒙北山北带古生代地壳演化与成矿作用[J].甘肃地质,2011,20(2): 45-50
沈存利,张梅,于玺卿等.内蒙古钼矿找矿新进展及成矿远景分析[ J].地质与勘探, 2010, 46(4) :561-575
唐克东，邵济安.中亚褶皱区构造演化问题[ J] .现代地质，1997，11（1）∶21-27
汤中立,白云来.亚欧大陆桥北山—天山接合部构造格局[ J] .甘肃地质学报,1997,6（增刊）:13-20
王大为,邹治平,李绍雄.甘肃公婆泉铜矿成矿地质特征及矿床成因[J].西北地质科学,1995,16(1):115-122
王继春,王兢繁,许永旺等.小狐狸山钼多金属－稀有金属矿床的地质意义[J].金属矿山, 2011,418（4）:101-103
魏文中.1978年.甘肃红石山铬铁矿床基本特征和成因[J] .西北地质
夏林圻,夏祖春,徐学义等.天山古生代洋陆转化特点的几点思考[J] .西北地质,2002,4:9-19.
肖庆辉,王涛,邓晋福等.2009.中国典型造山带花岗岩与大陆地壳生长研究[M].地质出版社
肖荣阁,刘敬党,费红彩等.2008.岩石矿床地球化学[M].地质出版社
肖荣阁,彭润民,王美娟,戚开静.华北地台北缘西段主要成矿系统分析[Ｊ].地球科学——中国地质大学学报,2000,25（4）:262-268
肖渊甫,吴德超,邓江红等.新疆北山构造带西段小长山南超单元花岗岩特征[Ｊ].岩石矿物学杂志,2002，21（2）:162-168
徐备，陈斌.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构和演化[Ｊ].中国科学(Ｄ辑),1997,27(3)
姚志强，都起民，卢秉刚, 1993.多宝山铜矿床综合找矿模式,《大兴安岭及其邻区铜多金属矿床论文集》.地震出版社.
严光生,邱瑞照,连长云,Warren J·Nokleberg等.中国大陆斑岩铜矿资源潜力定量评价[Ｊ].地学前缘,2007,14（5）:584-588
颜廷杰,吕志成.磁法勘探技术在老矿区找矿中的应用及效果[Ｊ].矿产勘查,2011,2（5）:27-41
杨合群,李英,杨建国等.北山造山带的基本成矿特征[J].西北地质, 2006, 39(2) :78-95
杨帅师,李新仁,许立权,贺锋,康小龙,巩智镇等. 2003.内蒙古自治区额济纳旗甜水井地区1∶5万区域地质调查报告[R].内蒙古自治区地质调查院
杨帅师,张玉宝,郑宝军,巩智镇等. 2004.内蒙古北山成矿远景区矿产资源评价报告[R].内蒙古自治区地质调查院
杨帅师,陈志勇,康小龙,李新仁等.内蒙古西部北山地区中上二叠统双堡塘组地层古生物特征[J].地质通报,2005,24(3):272-276
杨永强,翟裕生等.沉积岩型铅锌矿床的成矿系统研究[J].地学前缘,2006,13(3): 200-205.
叶天竺,肖克炎,严光生.矿床模型综合地质信息预测技术研究[J].地学前缘, 2007,14(5):11-19.
叶天竺,薛建玲.金属矿床深部找矿中的地质研究[J].中国地质, 2007,34(5): 855-869.
左国朝,何国琦等. 1990.北山板块构造及成矿规律[M].北京大学出版社.
左国朝,张淑玲,何国琦,张杨.北山地区早古生代板块构造特征[J].地质科学,1990,4:305-314
左国朝,刘春燕,白万成,冯永忠.北山泥盆纪碰撞造山火山一磨拉石地质构造及地球化学特征[J].甘肃地质学报,1995,4（1）:35-43
赵彦庆,刘明强,张万仁等.甘肃北山红石山地区发现早古生代奥陶纪地层[J].地质通报，2003,22（3）:215
翟裕生.长江中下游铁铜矿床成因类型及成矿系列探讨[J].地质与勘探, 1980, 16 (3):9-13.
翟裕生,姚书振,崔彬等. 1996.成矿系列研究[M].武汉:中国地质大学出版社.
翟裕生,张湖,宋鸿林等. 1997.大型构造与超大型矿床[M].北京:地质出版社.
翟裕生.成矿系统与综合地质异常. [J].现代地质, 1999, 13 (1): 1-7.
翟裕生.论成矿系统[J].地学前缘,1999, 6 (1): 13-27.
翟裕生等. 1999.区域成矿学[M] .地质出版社.
翟裕生等.成矿系统分析与新类型矿床预测[J] .地学前缘，2000，7（1）:123-132
翟裕生.成矿系统及其演化—初步实践到理论思考[J].地球科学—中国地质大学学报,2000, 25（4）:333-339
翟裕生,邓军,彭润民等.矿床变化与保存的研究内容和研究方法[J].地球科学—中国地质大学学报2000. 25（4）:340-345
翟裕生,邓军,彭润民,王建平.2002.古陆边缘成矿系统[M],北京：地质出版社.
翟裕生,苗来成,向运川,邓军,王建平.华北克拉通绿岩带型金成矿系统初析[J].地球科学—中国地质大学学报,2002,27（5）∶5 22-531
翟裕生.中国区域成矿特征探讨[J].地质与勘探, 2002, 38(5): 1-47.
翟裕生.区域构造地球化学与成矿[J].地质调查与研究,2003 ,26（1）:1-7
翟裕生.地球系统成矿系统到勘查系统[J].地学前缘，2007，14(1) :172-181
翟裕生,王建平,邓军等.成矿系统时空演化及其找矿意义[J].现代地质,2008，22(2) :143-150
翟裕生,邓军,彭润民,王建平.2010.成矿系统论[R],北京：地质出版社.
张彤,陈志勇,许立权,陈郑辉.内蒙古卓资县大苏计钼矿辉钼矿铼-锇同位素定年及其地质意义[ J].岩矿测试, 2009，28(3):279-282
郑宝军，苏世杰，樊永刚，张玉宝等. 2008.内蒙古自治区大狐狸山幅（K47E010017）矿产远景调查说明书[R].内蒙古自治区地质调查院
周文川，李聪慧，庄晓玲等. 2008.内蒙古自治区额济纳旗小狐狸山矿区铅锌钼矿详查报告[R].内蒙古地质矿产勘查院
祝新友,韦昌山,王艳丽等.广东大宝山钼钨多金属矿床成矿系统与找矿预测[ J].矿产勘查,2011，2(6):661-668
祝新友,汪东波,王书来.新疆阿克陶县塔木-卡兰古铅锌矿带成矿流体来源的矿物学论证[ J].159-165
Audetat A, Gunther D, Heinrich CA. 1998. Formation of a magmatic-hydrothermal ore deposit:Insights with LA-ICP-MS analysis of fluid inclusions. Science, 279: 2091-2094
Bouse RM, Ruiz J, Titley SR, Tosda1 RM and Wooden JL. 1999. Lead isotope compositions ofLate Cretaceous and Early Tertiary igneous rocks and sulfide minerals in ArizonaImplications for the sources of plutons and metals in porphyry copper deposits EconomicGeo1ogy, 94(2): 211-244.
Candela PA and Holland HD. 1986. A mass transfer model for copper and molybdenum inmagmatic hydrothermal system: The origin of porphyry-type ore deposits. EconomicGeology, 81 (1): 1-19.
Cooke D R, Hollings P. 2005. Giant porphyry deposits: characteris, distribution, and tectoniccontrols. Economic Geology, 100: 801-818
Force ER, 1998. Laramide alteration of Proterozoic diabase: a likely contributor of copper toporphyry systems in the Dripping Spring mountains area, southeastem Arizona. EconomicGeo1ogy, 93(2): 171-183.
Hedenquist JW, Arribas AJ and Reynolds TJ. 1998. Evolution of an intrusion-centeredhydrothermal system: Far Southeast-Lepanto porphyry and epithermal Cu-Au deposits,Philippines. Economic Geology, 93: 373-404.
Heinrich CA. 2005. The physical and chemical evolution of low-salinity magmatic fluids at theporphyry to epithermal transition: A thermodynamic study. Mineralium Deposita, 39:864-889
Klemm LM, Pettke T, Heinrich CA, Campos E. 2007. Hydrothermal Evolution of the El TenienteDeposit, Chile: Porphyry Cu-Mo Ore Deposition from Low-Salinity Magmatic Fluids.Economic Geology, 102(6): 1021-1045
Lowell JD and Guilbert JM. 1970. Lateral and vertical alteration-mineralization zoning inporphyry ore deposits. Economic Geology, 65: 373-404.
Mungall JE. 2002. Roasting the mantle: slab melting and the genesis of major Au and Au-rich Cudeposits. Geology, 30: 915-918.
Nagaseki H, Hayashi K. 2008. Experimental study of the behavior of copper and zinc in a boilinghydrothermal system. Geology, 36(1): 27-30
Pokrovski GS, Roux J, Harrichoury JC. 2005. Fluid density control on vapor-liquid partitioning ofmetals in hydrothermal systems. Geology, 33(8): 657-660
Pokrovski GS, Zakirov IV, Roux J, Testemale D, Hazemann JL, Bychkov AY, Golikova GV. 2002.Experimental study of arsenic speciation in vapor phase to 500°C: implications for Astransport and fractionation in low-density crustal fluids and volcanic gases. Geochimica etCosmochimica Acta, 66 (19): 3453-3480
Robb L. 2005. Introduction to ore-forming process. Oxford: Blackwell.1-166.
Seedorff E, Dilles JH, Proffett JM, Einaudi M, Zurcher L, Stavast WJA, Johnson DA, Barton MD.2005. Porphyry deposits: charcdteristics and origin of hypogene features. Economic Geology100th Anniversary Volume: 251-298
Seo JH, Guillong M, Heinrich CA. 2009. The role of sulfur in the formation ofmagmatic-hydrothermal copper-gold deposits. Earth and Planetary Science Letters, 282(1-4):323-328
Sillitoe RH. 1972. A plate tectonic model for the origin of porphyry copper deposits. EconomicGeology, 67: 184-197.
Sillitoe RH. 1972. A plate tectonic model for the origin of porphyrycopper deposits. EconomicGeology, 67(2): 184-197
Sillitoe RH. 1997. Characteristics and controls of the largest porphyry copper- gold and epithermalgold deposits in the circum-Pacific region: Australian Journal of Earth Sciences, 44: 373-388.
Sillitoe RH. 1997. Characteristics and controls of the largest porphyry copper- gold and epithermalgold deposits in the circum-Pacific region: Australian Journal of Earth Sciences, 44:373-388.
Sillitoe RH. 2010. Porphyry copper systems. Economic Geology, 105: 3-41
Simon AC, Pettke T, Candela PA, Piccoli PM, Heinrich CA. 2006. Copper partitioning in amelt-vapor-brine-magnetite-pyrrhotite assemblage. Geochimica et Cosmochimica Acta,70(22): 5583-5600
Solomon M. 1990. Subduction, arc reversal, and the origin of porphyry copper-gold deposits inisland arcs. Geology, 18(7): 630-633.
Ulrich T, Gunther D, and Heinrich CA. 1999. Gold concentrations of magmatic brines and themetal budget of porphyry copper deposits. Nature, 399: 676-679
Urich T. 2002. Evolution of a porphyry Cu-Au deposit, based on LA-ICP-MS analysis of fluidinclusions, Bajo de la Alumbrera, Argentina. Economic Geology, 97: 1888-1920
Webster J and Mandeville C. 2007. Fluid immiscibility in volcanic environments. Review MineralGeochemistry. 65: 313-362
陈富文,李华芹,蔡红等.新疆东部金窝子金矿床成因讨论—同位素地质年代学证据[J].地质论评,1999,45（3）:247-254
陈毓川,裴荣富,宋天锐. 1998.年中国矿床成矿系列初论[M].北京,地质出版社
陈毓川主编. 1999.中国主要成矿区带矿产资源远景评价[M].北京,地质出版社
陈祖伊,张学权,张昭明等著.北山区域地质发展史和金矿区域成矿模式[Ｊ] .铀矿地质,1993,9（2）:65-75
程小珍,杨伦,张晓.内蒙古小东沟钼矿成矿地质条件分析[J].地质与勘探,2007,43(05),11-16
程裕淇,陈毓川等.初论矿床的成矿系列问题.中国地质科学院院报,1979,第1号
崔惠文,陈祖伊. 1996.甘肃北山地区金矿地质[Ｍ] .北京:地质出版社.
崔惠文.甘肃北山古岛弧期后张裂带[J].贵金属地质,1996,5（4）:306-314
杜安道,何红蓼,殷宁万等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347
冯铁全,左国朝,金松桥.北山窑洞努如—公婆泉岛弧火山岩岩石地球化学特征（摘要）[Ｊ].甘肃地质学报,1997,6（增刊）:23-24
龚全胜,刘明强,梁明宏等.北山造山带大地构造相及构造演化[Ｊ].西北地质,2003,36（1）:11-17
龚全胜,刘明强,李海林等.甘肃北山造山带类型及基本特征[Ｊ].西北地质,2002,35（3）:28-34
葛肖虹著.中亚大陆一次重要的板内会聚事件[Ｊ].地学前缘,1999,6(4):330
洪大卫,黄怀曾,肖宜君等.内蒙中部二叠纪碱性花岗岩及其地球动力学意义[Ｊ].地质学报,1994,68(3):219-230
洪大卫,王式光,谢锡林等.试析地幔来源物质成矿域—以中亚造山带为例[J].矿床地质,2003,22（1）:41-55
何建坤,刘金朝.下地壳流变与造山带同挤压期地壳伸展的动力学关系[J].地球物理学报,2002,45（4）:502-516
何国琦,李茂松,刘德权著. 1994.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社
黄崇轲,白冶,朱裕生等著. 2001.中国铜矿床[Ｍ].北京地质出版社
江思宏,聂凤军,陈文等著.北山明水地区花岗岩时代的确定及其地质意义[J].岩石矿物学杂志,2003,22（2）:107-111
雷洪平,徐玉麟著. 1984.内蒙古自治区额济纳旗流沙山钼矿区详细普查地质报告[R].甘肃省地质矿产局第四地质队.
李人澍.成矿系统分析的理论与实践. [M].地质出版社, 1996.
李述靖,张维杰,耿明山著.1998.蒙古弧地质构造特征及形成演化概论[M].北京:地质出版社.
李双林,欧阳自远.兴蒙造山带及邻区的构造格局与构造演化[J].海洋地质与第四纪地质,1998,18(3):45-54
李文国,姜万德,王惠等. 1996.内蒙古岩石地层[M].中国地质大学出版社
李景春,赵安生,崔惠文.北山北带地质构造特征[J].贵金属地质，1965（1）:59-68
李华芹,谢才富,常海亮. 1998 .新疆北部有色贵金属矿床成矿作用年代学[Ｍ].北京地质出版社
李奋其,王成善.甘肃公婆泉铜矿田地质特征和控矿因素分析[J].成都理工大学学报(自然科学版),2003,30（2）:120-125
梁明宏,龚全胜,李海林等.造山带花岗岩类型及填图方法的实践—以甘肃北山造山带为例.岩石矿物学杂志,2002,21（2）:174-178
刘明强,党引业,龚全胜.甘肃北山平头山逆冲推覆构造的特征.西北地质,2002,35（1）:22-27
刘雪亚,王荃.中国西部北山造山带的大地构造及其演化[Ｊ] .地学研究,1995,28:37-48
刘益康,徐叶兵.蒙古Oyu Tolgoi斑岩铜金矿的勘查[J].地质与勘探,2003,39 (1),1-4
吕志成.与危机矿山接替资源勘查有关的成矿找矿模式[J].矿床地质,2006,25 (增刊),439-442
吕志成,戴自希,蔺志永,彦廷杰.危机矿山接替资源找矿勘查相关成矿理论与技术方法[J].矿物岩石地球化学通报,23卷增刊,132-133.
毛景文,杨建民,屈文俊等.新疆黄山东铜镍硫化物矿床Ｒｅ-Ｏｓ同位素测定及其地球动力学意义[Ｊ] .矿床地质,2002,21(4),323-330
穆治国,刘驰,黄宝玲,侯贵廷,左国朝等.甘肃北山古生代造山带地壳演化的同位素和稀土元素地球化学特征[J] .北京大学学报(自然科学版),1994,30（2）:202-214
聂凤军,江思宏,白大明等. 2002.北山地区金属矿床成矿规律及找矿方向[M].地质出版社
聂凤军,江思宏,赵省民.内蒙古流沙山金(钼)矿床地质特征及矿床类型划分[J].地质地球化学,2002,30(1):1-7
聂凤军,江思宏,白大明等.北山中南带海西-印支期岩浆活动与金的成矿作用[J].地球学报，2003,24(5):415-422
聂凤军,江思宏,白大明等.蒙甘新相邻(北山)地区金铜矿床时空分布特征及成矿作用[J] .矿床地质,2003,22(3) :234-245
聂凤军,屈文俊,刘妍,杜安道,江思宏.内蒙古额勒根斑岩型钼(铜)矿化区辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,2005,24(6): 638-646.
彭振安,李红红,张诗启等.内蒙古北山地区小狐狸山钼矿成矿岩体地球化学特征研究[ J].地质与勘探,2010,46(2) : 291-299
彭振安,李红红,屈文俊等.内蒙古北山地区小狐狸山钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿床地质, 2010,29(3) : 510-516
潘启宇,沈鸿章,李文国等. 1991,内蒙古自治区区域地质志[M] .地质出版社.
秦克章,方同辉,王书来等.东天山板块构造分区、演化与成矿地质背景研究[J].矿床地质,2002,20（4）
芮宗瑶,黄宗轲,齐国民. 1984.中国斑岩铜(钼)矿床[M].地质出版社
芮琮瑶.2002.国内外斑岩型铜矿研究进展[M].中国地质调查局
司雪峰,崔银亮,穆新河.甘肃北山中带变质碎屑岩型金矿地质特征及找矿前景[J].地质与勘探,2001,37（6）:5-8
孙新春等.甘蒙北山北带古生代地壳演化与成矿作用[J].甘肃地质,2011,20(2): 45-50
沈存利,张梅,于玺卿等.内蒙古钼矿找矿新进展及成矿远景分析[ J].地质与勘探, 2010, 46(4) :561-575
唐克东，邵济安.中亚褶皱区构造演化问题[ J] .现代地质，1997，11（1）∶21-27
汤中立,白云来.亚欧大陆桥北山—天山接合部构造格局[ J] .甘肃地质学报,1997,6（增刊）:13-20
王大为,邹治平,李绍雄.甘肃公婆泉铜矿成矿地质特征及矿床成因[J].西北地质科学,1995,16(1):115-122
王继春,王兢繁,许永旺等.小狐狸山钼多金属－稀有金属矿床的地质意义[J].金属矿山, 2011,418（4）:101-103
魏文中.1978年.甘肃红石山铬铁矿床基本特征和成因[J] .西北地质
夏林圻,夏祖春,徐学义等.天山古生代洋陆转化特点的几点思考[J] .西北地质,2002,4:9-19.
肖庆辉,王涛,邓晋福等.2009.中国典型造山带花岗岩与大陆地壳生长研究[M].地质出版社
肖荣阁,刘敬党,费红彩等.2008.岩石矿床地球化学[M].地质出版社
肖荣阁,彭润民,王美娟,戚开静.华北地台北缘西段主要成矿系统分析[Ｊ].地球科学——中国地质大学学报,2000,25（4）:262-268
肖渊甫,吴德超,邓江红等.新疆北山构造带西段小长山南超单元花岗岩特征[Ｊ].岩石矿物学杂志,2002，21（2）:162-168
徐备，陈斌.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构和演化[Ｊ].中国科学(Ｄ辑),1997,27(3)
姚志强，都起民，卢秉刚, 1993.多宝山铜矿床综合找矿模式,《大兴安岭及其邻区铜多金属矿床论文集》.地震出版社.
严光生,邱瑞照,连长云,Warren J·Nokleberg等.中国大陆斑岩铜矿资源潜力定量评价[Ｊ].地学前缘,2007,14（5）:584-588
颜廷杰,吕志成.磁法勘探技术在老矿区找矿中的应用及效果[Ｊ].矿产勘查,2011,2（5）:27-41
杨合群,李英,杨建国等.北山造山带的基本成矿特征[J].西北地质, 2006, 39(2) :78-95
杨帅师,李新仁,许立权,贺锋,康小龙,巩智镇等. 2003.内蒙古自治区额济纳旗甜水井地区1∶5万区域地质调查报告[R].内蒙古自治区地质调查院
杨帅师,张玉宝,郑宝军,巩智镇等. 2004.内蒙古北山成矿远景区矿产资源评价报告[R].内蒙古自治区地质调查院
杨帅师,陈志勇,康小龙,李新仁等.内蒙古西部北山地区中上二叠统双堡塘组地层古生物特征[J].地质通报,2005,24(3):272-276
杨永强,翟裕生等.沉积岩型铅锌矿床的成矿系统研究[J].地学前缘,2006,13(3): 200-205.
叶天竺,肖克炎,严光生.矿床模型综合地质信息预测技术研究[J].地学前缘, 2007,14(5):11-19.
叶天竺,薛建玲.金属矿床深部找矿中的地质研究[J].中国地质, 2007,34(5): 855-869.
左国朝,何国琦等. 1990.北山板块构造及成矿规律[M].北京大学出版社.
左国朝,张淑玲,何国琦,张杨.北山地区早古生代板块构造特征[J].地质科学,1990,4:305-314
左国朝,刘春燕,白万成,冯永忠.北山泥盆纪碰撞造山火山一磨拉石地质构造及地球化学特征[J].甘肃地质学报,1995,4（1）:35-43
赵彦庆,刘明强,张万仁等.甘肃北山红石山地区发现早古生代奥陶纪地层[J].地质通报，2003,22（3）:215
翟裕生.长江中下游铁铜矿床成因类型及成矿系列探讨[J].地质与勘探, 1980, 16 (3):9-13.
翟裕生,姚书振,崔彬等. 1996.成矿系列研究[M].武汉:中国地质大学出版社.
翟裕生,张湖,宋鸿林等. 1997.大型构造与超大型矿床[M].北京:地质出版社.
翟裕生.成矿系统与综合地质异常. [J].现代地质, 1999, 13 (1): 1-7.
翟裕生.论成矿系统[J].地学前缘,1999, 6 (1): 13-27.
翟裕生等. 1999.区域成矿学[M] .地质出版社.
翟裕生等.成矿系统分析与新类型矿床预测[J] .地学前缘，2000，7（1）:123-132
翟裕生.成矿系统及其演化—初步实践到理论思考[J].地球科学—中国地质大学学报,2000, 25（4）:333-339
翟裕生,邓军,彭润民等.矿床变化与保存的研究内容和研究方法[J].地球科学—中国地质大学学报2000. 25（4）:340-345
翟裕生,邓军,彭润民,王建平.2002.古陆边缘成矿系统[M],北京：地质出版社.
翟裕生,苗来成,向运川,邓军,王建平.华北克拉通绿岩带型金成矿系统初析[J].地球科学—中国地质大学学报,2002,27（5）∶5 22-531
翟裕生.中国区域成矿特征探讨[J].地质与勘探, 2002, 38(5): 1-47.
翟裕生.区域构造地球化学与成矿[J].地质调查与研究,2003 ,26（1）:1-7
翟裕生.地球系统成矿系统到勘查系统[J].地学前缘，2007，14(1) :172-181
翟裕生,王建平,邓军等.成矿系统时空演化及其找矿意义[J].现代地质,2008，22(2) :143-150
翟裕生,邓军,彭润民,王建平.2010.成矿系统论[R],北京：地质出版社.
张彤,陈志勇,许立权,陈郑辉.内蒙古卓资县大苏计钼矿辉钼矿铼-锇同位素定年及其地质意义[ J].岩矿测试, 2009，28(3):279-282
郑宝军，苏世杰，樊永刚，张玉宝等. 2008.内蒙古自治区大狐狸山幅（K47E010017）矿产远景调查说明书[R].内蒙古自治区地质调查院
周文川，李聪慧，庄晓玲等. 2008.内蒙古自治区额济纳旗小狐狸山矿区铅锌钼矿详查报告[R].内蒙古地质矿产勘查院
祝新友,韦昌山,王艳丽等.广东大宝山钼钨多金属矿床成矿系统与找矿预测[ J].矿产勘查,2011，2(6):661-668
祝新友,汪东波,王书来.新疆阿克陶县塔木-卡兰古铅锌矿带成矿流体来源的矿物学论证[ J].159-165
Audetat A, Gunther D, Heinrich CA. 1998. Formation of a magmatic-hydrothermal ore deposit:Insights with LA-ICP-MS analysis of fluid inclusions. Science, 279: 2091-2094
Bouse RM, Ruiz J, Titley SR, Tosda1 RM and Wooden JL. 1999. Lead isotope compositions ofLate Cretaceous and Early Tertiary igneous rocks and sulfide minerals in ArizonaImplications for the sources of plutons and metals in porphyry copper deposits EconomicGeo1ogy, 94(2): 211-244.
Candela PA and Holland HD. 1986. A mass transfer model for copper and molybdenum inmagmatic hydrothermal system: The origin of porphyry-type ore deposits. EconomicGeology, 81 (1): 1-19.
Cooke D R, Hollings P. 2005. Giant porphyry deposits: characteris, distribution, and tectoniccontrols. Economic Geology, 100: 801-818
Force ER, 1998. Laramide alteration of Proterozoic diabase: a likely contributor of copper toporphyry systems in the Dripping Spring mountains area, southeastem Arizona. EconomicGeo1ogy, 93(2): 171-183.
Hedenquist JW, Arribas AJ and Reynolds TJ. 1998. Evolution of an intrusion-centeredhydrothermal system: Far Southeast-Lepanto porphyry and epithermal Cu-Au deposits,Philippines. Economic Geology, 93: 373-404.
Heinrich CA. 2005. The physical and chemical evolution of low-salinity magmatic fluids at theporphyry to epithermal transition: A thermodynamic study. Mineralium Deposita, 39:864-889
Klemm LM, Pettke T, Heinrich CA, Campos E. 2007. Hydrothermal Evolution of the El TenienteDeposit, Chile: Porphyry Cu-Mo Ore Deposition from Low-Salinity Magmatic Fluids.Economic Geology, 102(6): 1021-1045
Lowell JD and Guilbert JM. 1970. Lateral and vertical alteration-mineralization zoning inporphyry ore deposits. Economic Geology, 65: 373-404.
Mungall JE. 2002. Roasting the mantle: slab melting and the genesis of major Au and Au-rich Cudeposits. Geology, 30: 915-918.
Nagaseki H, Hayashi K. 2008. Experimental study of the behavior of copper and zinc in a boilinghydrothermal system. Geology, 36(1): 27-30
Pokrovski GS, Roux J, Harrichoury JC. 2005. Fluid density control on vapor-liquid partitioning ofmetals in hydrothermal systems. Geology, 33(8): 657-660
Pokrovski GS, Zakirov IV, Roux J, Testemale D, Hazemann JL, Bychkov AY, Golikova GV. 2002.Experimental study of arsenic speciation in vapor phase to 500°C: implications for Astransport and fractionation in low-density crustal fluids and volcanic gases. Geochimica etCosmochimica Acta, 66 (19): 3453-3480
Robb L. 2005. Introduction to ore-forming process. Oxford: Blackwell.1-166.
Seedorff E, Dilles JH, Proffett JM, Einaudi M, Zurcher L, Stavast WJA, Johnson DA, Barton MD.2005. Porphyry deposits: charcdteristics and origin of hypogene features. Economic Geology100th Anniversary Volume: 251-298
Seo JH, Guillong M, Heinrich CA. 2009. The role of sulfur in the formation ofmagmatic-hydrothermal copper-gold deposits. Earth and Planetary Science Letters, 282(1-4):323-328
Sillitoe RH. 1972. A plate tectonic model for the origin of porphyry copper deposits. EconomicGeology, 67: 184-197.
Sillitoe RH. 1972. A plate tectonic model for the origin of porphyrycopper deposits. EconomicGeology, 67(2): 184-197
Sillitoe RH. 1997. Characteristics and controls of the largest porphyry copper- gold and epithermalgold deposits in the circum-Pacific region: Australian Journal of Earth Sciences, 44: 373-388.
Sillitoe RH. 1997. Characteristics and controls of the largest porphyry copper- gold and epithermalgold deposits in the circum-Pacific region: Australian Journal of Earth Sciences, 44:373-388.
Sillitoe RH. 2010. Porphyry copper systems. Economic Geology, 105: 3-41
Simon AC, Pettke T, Candela PA, Piccoli PM, Heinrich CA. 2006. Copper partitioning in amelt-vapor-brine-magnetite-pyrrhotite assemblage. Geochimica et Cosmochimica Acta,70(22): 5583-5600
Solomon M. 1990. Subduction, arc reversal, and the origin of porphyry copper-gold deposits inisland arcs. Geology, 18(7): 630-633.
Ulrich T, Gunther D, and Heinrich CA. 1999. Gold concentrations of magmatic brines and themetal budget of porphyry copper deposits. Nature, 399: 676-679
Urich T. 2002. Evolution of a porphyry Cu-Au deposit, based on LA-ICP-MS analysis of fluidinclusions, Bajo de la Alumbrera, Argentina. Economic Geology, 97: 1888-1920
Webster J and Mandeville C. 2007. Fluid immiscibility in volcanic environments. Review MineralGeochemistry. 65: 313-362