四川龙门山南段铜镍矿成矿地质特征及资源潜力研究
|
摘要
研究区位于都江堰市灌口以南宝山县与芦山县交界处横跨盆地北西缘和盆周山地南西缘中段,构造上该区位于龙门山褶皱带南段,受次级构造单元“宝兴复背斜”控制,构造控制方向为北东--南西向。“宝兴复背斜”核心地层为前震旦系变质岩及宝兴杂岩组成,构造两翼为古生界、中生界时代的地层组成,次级断裂构造活动十分发育,构造-岩浆活动与成矿作用关系密切。自二十世纪八十年代以来,随着基础地质工作的全面展开,研究内不断获得新的突破,如发现中元古界黄水河群的基性岩以及黄铜尖子铜矿点含矿围岩中有大量铜镍矿化说明该区有良好的铜镍矿找矿远景。
本次研究在成矿理论和地球动力学的指导下对研究区内的铜镍矿开展研究工作,研究中广泛搜集区内以往地、物、化、遥及矿产勘查等基础资料,通过综合分析对研究区铜镍矿资源开展科学的研究和评价,对龙门山南段铜、镍等矿产资源潜力开展深入的研究,为区内远景靶区预测和成矿理论研究奠定了基石出。
龙门山南段具有良好的成铜镍矿地质和地球化学背景,区域内发现多处矿点和矿化点。根据区内成矿地质条件、已知矿产分布和矿床成因类型及物化探异常,在研究区内共圈定出与基性、超基性岩有关的铜、镍矿远景区,自北东向南西依次为芦山白铜尖子铜矿成矿远景区、芦山黄铜尖子铜镍成矿远景区、宝兴天主堂铜镍成矿远景区、太平铅锌成矿远景区和芦山火石崖铜镍异常区等4个成矿潜力好的区域,并发现十余处矿点及矿化点,发现了过去曾经被认为属“含铜黄铁矿型铜矿化”均产于黄水河群的绿色变质岩系中的理论；经实地勘察和深入研究发现含矿的角闪岩原岩为基性—超基性岩,这些铜矿化均伴有不同程度的镍矿化,因此本文将从变质原岩恢复及深部找矿入手全面深入的挖掘研究铜镍矿床的成因,区内主要类型为“黄铜尖子”铜矿、“白白铜尖子”铜(镍)矿,其次为“天主堂”铜(含铂族)矿,根据成铜(镍)地质和地球化学背景,区内在岩浆型铜(镍)硫化物矿床找矿上还具有良好的成矿潜力。
Study area south of the mouth located in Dujiangyan irrigation Lushan County, Baoshan County and across the junction of the north western margin of the basin and Basin southwest edge of the middle of the mountain, construction area is located on the southern section of the Longmen Shan fold belt, constructed by the sub-unit "Baoxing complex anticline "control, construction control direction NE-SW direction."Baoxing anticlinorium" core formation for the pre-Sinian metamorphic rocks and Baoxing complex, constructed wings for the Paleozoic, Mesozoic stratigraphic age composition, activities are well developed secondary faults, tectonic-magmatic activity and mineralization are closely related. Since the1980s, along with basic geological work in full swing, the study continue to receive a new breakthrough, such as found in Yellow River Middle Proterozoic mafic group of top brass and copper ore-bearing rock in the point a large number of copper-nickel mineralization in the area have a good description of copper-nickel ore exploration vision.
In the mineralization of this study under the guidance of theory and geodynamics of the study area copper-nickel mine to carry out research work, the study collected extensive area in the past, the materials, technology, remote and mineral exploration and other basic information, through a comprehensive analysis copper-nickel mine on the study area resources to carry out scientific research and evaluation, the southern section of the Longmen copper, nickel and other mineral resource potential of in-depth study of long-term target forecast for the region and laid the foundation for forming theory.
Longmen Mountains into the southern section has a good geological and geochemical copper-nickel mining background, found that many mine sites within the region and mineralization. According to local geological conditions, the known distribution and genesis of mineral types and geophysical and geochemical anomalies in the study area were delineated and basic, ultrabasic rocks for copper, nickel prospect, from north east to the southwest followed by copper-nickel alloy top copper mineralization prospects Lushan area, top brass, copper-nickel mineralization Lushan prospective areas, Baoxing Church copper-nickel mineralization prospect, lead and zinc ore prospect area and the Pacific Lushan fire cliffs and other4copper-nickel anomalies mineralization potential of a good area, and found more than ten points and mineralization at the mine, discovered in the past had been considered to be "copper-pyrite-type copper-based" groups are produced in the yellow River in the green metamorphic rocks theory; by field survey and in-depth study of ore-bearing amphibolite protolith mafic-ultramafic rocks, which are associated with different levels of copper nickel mineralization, this article from the metamorphic rocks to restore the original look and deep ore mining to start in-depth study of the causes of copper-nickel deposits, the main types of the region as a "top brass" copper,"copper-top vain," copper (Ni) deposit, followed by "Church" of copper (including PGE) deposit, according to copper (Ni) geological and geochemical background of the region in the magmatic Cu-(Ni) sulfide ore deposit, ore still has good potential.
本次研究在成矿理论和地球动力学的指导下对研究区内的铜镍矿开展研究工作,研究中广泛搜集区内以往地、物、化、遥及矿产勘查等基础资料,通过综合分析对研究区铜镍矿资源开展科学的研究和评价,对龙门山南段铜、镍等矿产资源潜力开展深入的研究,为区内远景靶区预测和成矿理论研究奠定了基石出。
龙门山南段具有良好的成铜镍矿地质和地球化学背景,区域内发现多处矿点和矿化点。根据区内成矿地质条件、已知矿产分布和矿床成因类型及物化探异常,在研究区内共圈定出与基性、超基性岩有关的铜、镍矿远景区,自北东向南西依次为芦山白铜尖子铜矿成矿远景区、芦山黄铜尖子铜镍成矿远景区、宝兴天主堂铜镍成矿远景区、太平铅锌成矿远景区和芦山火石崖铜镍异常区等4个成矿潜力好的区域,并发现十余处矿点及矿化点,发现了过去曾经被认为属“含铜黄铁矿型铜矿化”均产于黄水河群的绿色变质岩系中的理论；经实地勘察和深入研究发现含矿的角闪岩原岩为基性—超基性岩,这些铜矿化均伴有不同程度的镍矿化,因此本文将从变质原岩恢复及深部找矿入手全面深入的挖掘研究铜镍矿床的成因,区内主要类型为“黄铜尖子”铜矿、“白白铜尖子”铜(镍)矿,其次为“天主堂”铜(含铂族)矿,根据成铜(镍)地质和地球化学背景,区内在岩浆型铜(镍)硫化物矿床找矿上还具有良好的成矿潜力。
Study area south of the mouth located in Dujiangyan irrigation Lushan County, Baoshan County and across the junction of the north western margin of the basin and Basin southwest edge of the middle of the mountain, construction area is located on the southern section of the Longmen Shan fold belt, constructed by the sub-unit "Baoxing complex anticline "control, construction control direction NE-SW direction."Baoxing anticlinorium" core formation for the pre-Sinian metamorphic rocks and Baoxing complex, constructed wings for the Paleozoic, Mesozoic stratigraphic age composition, activities are well developed secondary faults, tectonic-magmatic activity and mineralization are closely related. Since the1980s, along with basic geological work in full swing, the study continue to receive a new breakthrough, such as found in Yellow River Middle Proterozoic mafic group of top brass and copper ore-bearing rock in the point a large number of copper-nickel mineralization in the area have a good description of copper-nickel ore exploration vision.
In the mineralization of this study under the guidance of theory and geodynamics of the study area copper-nickel mine to carry out research work, the study collected extensive area in the past, the materials, technology, remote and mineral exploration and other basic information, through a comprehensive analysis copper-nickel mine on the study area resources to carry out scientific research and evaluation, the southern section of the Longmen copper, nickel and other mineral resource potential of in-depth study of long-term target forecast for the region and laid the foundation for forming theory.
Longmen Mountains into the southern section has a good geological and geochemical copper-nickel mining background, found that many mine sites within the region and mineralization. According to local geological conditions, the known distribution and genesis of mineral types and geophysical and geochemical anomalies in the study area were delineated and basic, ultrabasic rocks for copper, nickel prospect, from north east to the southwest followed by copper-nickel alloy top copper mineralization prospects Lushan area, top brass, copper-nickel mineralization Lushan prospective areas, Baoxing Church copper-nickel mineralization prospect, lead and zinc ore prospect area and the Pacific Lushan fire cliffs and other4copper-nickel anomalies mineralization potential of a good area, and found more than ten points and mineralization at the mine, discovered in the past had been considered to be "copper-pyrite-type copper-based" groups are produced in the yellow River in the green metamorphic rocks theory; by field survey and in-depth study of ore-bearing amphibolite protolith mafic-ultramafic rocks, which are associated with different levels of copper nickel mineralization, this article from the metamorphic rocks to restore the original look and deep ore mining to start in-depth study of the causes of copper-nickel deposits, the main types of the region as a "top brass" copper,"copper-top vain," copper (Ni) deposit, followed by "Church" of copper (including PGE) deposit, according to copper (Ni) geological and geochemical background of the region in the magmatic Cu-(Ni) sulfide ore deposit, ore still has good potential.
引文
[1]肖克炎,张晓华,王四龙,等.矿产资源GIS评价系统[M].北京：地质出版社,2000.1-124.
[2]吴信才.地理信息系统的基本技术与发展动态[J].地球科学—中国地质大学学报,1998,23(4)：329-333.
[3]周成虎,鲁学军.对地球信息科学的思考[J].地理学报,1998,53(4)：372-380.
[4]张洪岩,王软敏,周成虎,等.“数字地球”与地理信息科学[J].地球信息科学,2001,(4)：1-4.
[5]Tor Bernhardsen. Geographic Information Systems—An Intro-duct ion[M]. New York:John Wiley &Sons Inc,2002.1-408.
[6]Anne Vernez Moudon, Michael Huber. Monitoring Land Sup-ply with Geographic Information Systems—Theory, Practice, and Parcel-Based Approaches [M]. Canada:John Wiley &Sons, Inc. 2000.1-327.
[7]Andrew C Millington, Stephen J Walsh, Patrick E Osborne. GIS and Remote Sensing Applications in Biogeography and E-cology[M]. USA:Kluwer Academic Publishers,2001.1-328.
[8]Keith C Clarke, Bradley 0 Parks, Michael P Crane. Geograph-ic Information Systems and Environmental Modeling[M]. NJ:Prelntice Hall,2002.1-298.
[9]赵俊三,赵耀龙.GIS发展的最新趋势及其应用前景[J].测绘工程,2000,9(2)：21-25.
[10]吴信才,白玉琪,郭玲玲.地理信息系统(GIS)发展现状及展望[J].计算机工程与应用,2000,(4)：8-9.
[11]方裕,周成虎,景贵飞,等.第四代GIS软件研究[J].中国图像图形学报,2001,6(9)：817-823.
[12]孟鲁闽,朱庆伟.互联网上地理信息系统的发展[J].测绘通报,2000,(7)：9-10.
[13]郑贵洲.地理信息系统(GIs)在地质学中的应用[J].地球科学——中国地质大学学报,1998,23(4)：420423.
[14]Mejia M, Navarro M, Wohl E E. Geological hazard and riskevaluation using GIS[J]. Bulletin of the Association of Engi-neering Geologists,1994,(4):21-30.
[15]姜作勤.新一代地质填图所面临的挑战[J].中国地质,1996,(2)：29-30.
[16]赵文吉,张松梅,晋佩东.GIS技术在区域地质调查中的应用[J].贵金属地质,2000,9(3)：170-173.
[17]Chi Shundu, Zhao Pengda, Li Jianwei. Application of GIS toGeo-anomaly-Based Delineation of Mineral Resources [J]. Journal of China University of Geosciences,2000,11(2):164-167.
[18]池顺都,赵鹏大.应用GIS圈定找矿可行地段和有利地段——以云南元江地区大红山群铜矿产为例[J].地球科学,1998,23(2)：125-128.
[19]Wu Xinlin,Chi Shundu. A GIS Approach to Prediction ofCopper Deposits [J]. Journal of China University of Geo-sciences,2000,11(2):180-182.
[20]曹瑜,胡光道.圈定“5P”找矿地段的GIS成矿预测空间模型及应用[J].地球科学——中国地质大学学报,1999,24(4)：409-412.
[21]陈华慧.遥感地质学[M].北京：地质出版社,1984
[22]Cao Yu, Hu Guangdao, Ma Hongchao. Application of GIS toGeological Information Extraction[J]. Journal of China Uni-versity of Geosciences,2000,11(2):183-185.
[23]陈述彭.从地质遥感迈向地质调查[J].遥感学报.2005,9(2)：113-116.
[24]陈石羡.地理信息系统在金属矿产预测中的应用[J].地质找矿论丛,1998,13(1)：74-83.
[25]Zhou Yunxuan,Wang Lei, Liu Wangsong, et al. A Review ofMineral Resources and GIS Application in Mineral ResourceAssessment in Northeast China[J]. Jour. Geosci. Res. NE Asi-a,2000,3(2): 169-180.
[26]李春霞.GIS在地质勘查找矿应用中的关键问题探讨[J].矿产与地质,2000,(6)：362-364.
[27]吴堑虹.利用GIS编制矿产预测图[J].地质与勘探,2000,36(3)：48-50.
[28]张振飞.GIS支持的矿产预测单元簇法[M].西安：陕西科学技术出版社,2001.6-8.
[29]向运川,任天祥,杨竹溪.开发利用地理信息系统(GIS)综合分析地学信息进行矿产预测[J].物探与化探,1996,20(1)：1-13.
[30]苏红旗,葛艳,刘冬林,等.基于GIS的证据权重法矿产预测系统(EWM)[J].地质与勘探,1999,35(1)：4446.
[31]周军,梁云.地理信息系统及其在地质矿产勘查中的应用[J].西安工程学院学报,2002,24(2)：47-50.
[32]袁峰,周涛发,岳书仓.GIS矿产资源预测中的证据权重法[J].黄金地质,2003,9(3)：75-77.
[33]宋国耀,张晓华等.矿产资源潜力评价的若干问题[J].中国地质,1999,(8)：17-19.
[34]徐翠玲等.GIS在矿产资源评价中的应用[J].西安文理学院学报,2006,9(4)：104-107.
[35]唐宾.GIS支持下的金属矿产成矿预测简介[J].广西地质,2000,13(1)：69-72.
[36]袁峰,周涛发,李湘凌等.基于GIS的矿产资源预测现状及关键问题[J].合肥工业大学学报,2004,27(5)：486-489.
[37]赵鹏大.“三联式”资源定量预测与评价一数字找矿理论与实践探讨[J].地球科学一中国地质大学学报,2002,27(5)：482-489.
[38]赵鹏大,陈建平,张寿庭.“三联式”成矿预测新进展[J].地学前缘,2003,10(2)：455-463.
[39]王世称、陈永良、夏立显,综合信息矿产预测理论与方法[M],北京：科学出版社,2000,1-200。
[40]黄杏元,马劲松,汤勤,等.地理信息系统概论[M]北京：高等教育出版社,1990,1-200。
[41]梅安新,彭望路,秦其明,等.遥感导论[M],高等教育出版社,2001,1一324.
[42]傅文杰.遥感矿化蚀变信息提取中两种新方法的应用研究[D].长沙：中南大学,2006,1-108.
[43]张廷斌.西藏谢通门县铜金矿带遥感图像蚀变信息提取及多源数据融合在成矿预测中的应用[D].成都：成都理工大学,2006,1-50.
[44]廖崇高,陈建平,刘登中.兰坪盆地遥感地质及化探综合分析在成矿预测中的应用[J].国土资源遥感,1999,42(4)：17一18.
[45]王四龙,王西华.北京地区遥感环形构造信息提取与金矿预测[J].地质与勘探,1996,32(4)：36-39
[46]常青.甘肃北山南带岩(矿)石波谱特征的初步研究(J].甘肃地质学报,1999,8(1)：49-55.
[47]刘莉.基于于ENVI青海茫崖地区遥感数据矿化信息提取[D].长沙：中南大学,2006,1-91.
[48]赵鹏大,胡旺亮,李紫金,等.矿产统计预测[M].北京：地质出版社,1983,1-115.
[49]王世称,范继璋,杨永华,等.矿产资源评价[M].吉林：吉林科学技术出版社,1987,151-157.
[50]高辉,JH ronsky,曹殿华,等.金川铜镍矿床成矿模式、控矿因素分析与找矿[J].地质与勘探.2009,45(3)：218-227.
[51]汤中立,任端进,薛增瑞,等.中国矿床.中国镍矿床[M].北京：地质出版社,1989,205-266.
[52]ZHAOPengda. "Three2step" quantitativeforeeastingandassessmentofresouree--theory of digitalexPlorationanddiseussiononPractiee[J]. EarthScience,2002,27(5):482-489
[53]CHENJianPing, ZHANGShouting, TANGJun, etal. Theoreticaleonsiderationtoquantitative foreeastingofnontraditionalmineralresouree[J]. ProgresslnGeophysies,2002,17(2):342-348.
[54]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
[55]姚敬金,张素兰,曹落华,等.中国土要大7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
[56]何政伟,孙传敏,朱章森.搜索法一一种无模型矿产预测的方法[J].矿物岩石,2000,20(3)：81-37.
[57]翟裕生,邓军,王建平,等.2004.深部找矿研究问题[J].矿床地质,23(2)：141-149.
[58]杨金中,方洪宾.中国西部重要成矿带遥感找矿异常提取的方法研究[J].国土资源遥感,2003,57(3)：50-53
[59]翟裕生,邓军,彭润民,等.2002.成矿系统研究及其资源、环境意义[J].高效地质学报,8(1)：1-8.
[60]甘甫平,王润生,马蔼乃,等.遥感地质信息提取集成与矿物遥感地质分析模型.遥感学报,2003,7(3)：208-213
[61]高亚林,汤中立,宋谢炎.金川铜镍矿隐伏富铜矿体成因研究及其深部找矿意义[J].岩石学报,2009,25(12)：3379-3395
[62]裴荣富.中国矿床模式[M].北京：地质出版社,1995：1-200.
[63]吴承烈,徐外生,刘崇民.中国主要类型铜矿勘查地球化学模刑[M].北京：地质出版社,1998：1-200.
[64]李文渊.岩浆Cu-Ni-PGE矿床研究现状及发展趋势[J].西北地质,2007,(2)：1-28.
[65]吕林素,刘裙,张作衡,等.中国岩浆型Ni-Cu-(PGE)硫化物矿床的时空分布及其地球动力学背景[J].岩石学报,2007,23(10)：2561-2594.
[66]汤中立,闫海卿,焦建刚,等.中国小岩体镍铜(铂族)矿床的区域成矿规律[J].地学前缘,2007,14(5)：92-103.
[67]成秋明.成矿过程奇异性与矿床多重分形分布[J].矿物岩石地球化学通报,2001,27(3)：298-305.
[68]陈毓川.中国主要成矿区带矿产资源远景评价[M].北京：地质出版社,1999.
[69]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.
[70]肖克炎,张晓华,李景朝.全国重要矿产总量预测方法[J].地学前缘,2007,14(5)：20-26.
[71]叶玉丰.基于GIS技术的矿产资源规划管理信息系统[J].地质与资源,2004,13(1)：52-64.
[72]肖克炎,丁建华,刘锐.美国“三步式”固体矿产资源潜力评价方法评述[J].地质论评,2006,52(6)：793-798.
[73]尹建忠.多源信息综合分析在矿产资源潜力评价中的应用[D].成都理工大学,2004.
[74]林茂炳、苟宗海.四川龙门山造山带造山模式研究[M],成都：成都科技大学出版社,1996,33-62。
[75]高怀忠.新疆坡北镁铁-超镁铁岩带1号岩体地质特征及其含矿性研究[J].地球科学：中国地质大学学报,1992,17(4)：391-401.
[76]李鸿儒.新疆坡北镁铁-超镁铁岩带控岩构造及成矿专属性[J].中国区域地质,1994,3：227-233.
[77]杨甲全,钟莉,邓刚.北山地区坡北1号、10号基性-超基性岩体成矿预测及找矿方向[J].新疆地质,2002,20(3)：214-218.
[78]孙赫,秦克章,李金祥,徐兴旺,三金柱,丁奎首,惠卫尔,许英霞.2006.尔天山图拉尔根铜镍钴硫化物矿床岩相、岩石地球化学特征及其形成的构造背景[J].中国地质,33(3)：157-168.
[79]肖骑彬,蔡新平,徐兴旺.浅层地震与MT联合技术在隐伏金属矿定位预测中的应用[J].矿床地质,24
[80]詹艳,赵国泽,汤吉.1999.新疆玛纳斯大震区地壳深部的电性结构[J].地震地质,21(2)159-166.
[81]朱建军.浅谈东天山镜尔泉铜镍矿的成因及成矿规律[J].新疆有色金属2011,20(3)1-3.
[82]毛德宝等.阿尔金成矿带成矿规律与找矿预测[J].西北地质,2006,39(2)：114-127.
[83]姚凤良,孙丰月.矿床学教程[M].北京：地质出版社,2006.
[84]汤中立,钱壮志,姜常义.中国镍铜铂岩浆硫化物矿床与成矿预测[M].北京：地质出版社,2006.
[85]李文渊.中国硫化物铜镍矿床成矿系列与地球化学[M].西安：西安地图出版社,1996.
[2]吴信才.地理信息系统的基本技术与发展动态[J].地球科学—中国地质大学学报,1998,23(4)：329-333.
[3]周成虎,鲁学军.对地球信息科学的思考[J].地理学报,1998,53(4)：372-380.
[4]张洪岩,王软敏,周成虎,等.“数字地球”与地理信息科学[J].地球信息科学,2001,(4)：1-4.
[5]Tor Bernhardsen. Geographic Information Systems—An Intro-duct ion[M]. New York:John Wiley &Sons Inc,2002.1-408.
[6]Anne Vernez Moudon, Michael Huber. Monitoring Land Sup-ply with Geographic Information Systems—Theory, Practice, and Parcel-Based Approaches [M]. Canada:John Wiley &Sons, Inc. 2000.1-327.
[7]Andrew C Millington, Stephen J Walsh, Patrick E Osborne. GIS and Remote Sensing Applications in Biogeography and E-cology[M]. USA:Kluwer Academic Publishers,2001.1-328.
[8]Keith C Clarke, Bradley 0 Parks, Michael P Crane. Geograph-ic Information Systems and Environmental Modeling[M]. NJ:Prelntice Hall,2002.1-298.
[9]赵俊三,赵耀龙.GIS发展的最新趋势及其应用前景[J].测绘工程,2000,9(2)：21-25.
[10]吴信才,白玉琪,郭玲玲.地理信息系统(GIS)发展现状及展望[J].计算机工程与应用,2000,(4)：8-9.
[11]方裕,周成虎,景贵飞,等.第四代GIS软件研究[J].中国图像图形学报,2001,6(9)：817-823.
[12]孟鲁闽,朱庆伟.互联网上地理信息系统的发展[J].测绘通报,2000,(7)：9-10.
[13]郑贵洲.地理信息系统(GIs)在地质学中的应用[J].地球科学——中国地质大学学报,1998,23(4)：420423.
[14]Mejia M, Navarro M, Wohl E E. Geological hazard and riskevaluation using GIS[J]. Bulletin of the Association of Engi-neering Geologists,1994,(4):21-30.
[15]姜作勤.新一代地质填图所面临的挑战[J].中国地质,1996,(2)：29-30.
[16]赵文吉,张松梅,晋佩东.GIS技术在区域地质调查中的应用[J].贵金属地质,2000,9(3)：170-173.
[17]Chi Shundu, Zhao Pengda, Li Jianwei. Application of GIS toGeo-anomaly-Based Delineation of Mineral Resources [J]. Journal of China University of Geosciences,2000,11(2):164-167.
[18]池顺都,赵鹏大.应用GIS圈定找矿可行地段和有利地段——以云南元江地区大红山群铜矿产为例[J].地球科学,1998,23(2)：125-128.
[19]Wu Xinlin,Chi Shundu. A GIS Approach to Prediction ofCopper Deposits [J]. Journal of China University of Geo-sciences,2000,11(2):180-182.
[20]曹瑜,胡光道.圈定“5P”找矿地段的GIS成矿预测空间模型及应用[J].地球科学——中国地质大学学报,1999,24(4)：409-412.
[21]陈华慧.遥感地质学[M].北京：地质出版社,1984
[22]Cao Yu, Hu Guangdao, Ma Hongchao. Application of GIS toGeological Information Extraction[J]. Journal of China Uni-versity of Geosciences,2000,11(2):183-185.
[23]陈述彭.从地质遥感迈向地质调查[J].遥感学报.2005,9(2)：113-116.
[24]陈石羡.地理信息系统在金属矿产预测中的应用[J].地质找矿论丛,1998,13(1)：74-83.
[25]Zhou Yunxuan,Wang Lei, Liu Wangsong, et al. A Review ofMineral Resources and GIS Application in Mineral ResourceAssessment in Northeast China[J]. Jour. Geosci. Res. NE Asi-a,2000,3(2): 169-180.
[26]李春霞.GIS在地质勘查找矿应用中的关键问题探讨[J].矿产与地质,2000,(6)：362-364.
[27]吴堑虹.利用GIS编制矿产预测图[J].地质与勘探,2000,36(3)：48-50.
[28]张振飞.GIS支持的矿产预测单元簇法[M].西安：陕西科学技术出版社,2001.6-8.
[29]向运川,任天祥,杨竹溪.开发利用地理信息系统(GIS)综合分析地学信息进行矿产预测[J].物探与化探,1996,20(1)：1-13.
[30]苏红旗,葛艳,刘冬林,等.基于GIS的证据权重法矿产预测系统(EWM)[J].地质与勘探,1999,35(1)：4446.
[31]周军,梁云.地理信息系统及其在地质矿产勘查中的应用[J].西安工程学院学报,2002,24(2)：47-50.
[32]袁峰,周涛发,岳书仓.GIS矿产资源预测中的证据权重法[J].黄金地质,2003,9(3)：75-77.
[33]宋国耀,张晓华等.矿产资源潜力评价的若干问题[J].中国地质,1999,(8)：17-19.
[34]徐翠玲等.GIS在矿产资源评价中的应用[J].西安文理学院学报,2006,9(4)：104-107.
[35]唐宾.GIS支持下的金属矿产成矿预测简介[J].广西地质,2000,13(1)：69-72.
[36]袁峰,周涛发,李湘凌等.基于GIS的矿产资源预测现状及关键问题[J].合肥工业大学学报,2004,27(5)：486-489.
[37]赵鹏大.“三联式”资源定量预测与评价一数字找矿理论与实践探讨[J].地球科学一中国地质大学学报,2002,27(5)：482-489.
[38]赵鹏大,陈建平,张寿庭.“三联式”成矿预测新进展[J].地学前缘,2003,10(2)：455-463.
[39]王世称、陈永良、夏立显,综合信息矿产预测理论与方法[M],北京：科学出版社,2000,1-200。
[40]黄杏元,马劲松,汤勤,等.地理信息系统概论[M]北京：高等教育出版社,1990,1-200。
[41]梅安新,彭望路,秦其明,等.遥感导论[M],高等教育出版社,2001,1一324.
[42]傅文杰.遥感矿化蚀变信息提取中两种新方法的应用研究[D].长沙：中南大学,2006,1-108.
[43]张廷斌.西藏谢通门县铜金矿带遥感图像蚀变信息提取及多源数据融合在成矿预测中的应用[D].成都：成都理工大学,2006,1-50.
[44]廖崇高,陈建平,刘登中.兰坪盆地遥感地质及化探综合分析在成矿预测中的应用[J].国土资源遥感,1999,42(4)：17一18.
[45]王四龙,王西华.北京地区遥感环形构造信息提取与金矿预测[J].地质与勘探,1996,32(4)：36-39
[46]常青.甘肃北山南带岩(矿)石波谱特征的初步研究(J].甘肃地质学报,1999,8(1)：49-55.
[47]刘莉.基于于ENVI青海茫崖地区遥感数据矿化信息提取[D].长沙：中南大学,2006,1-91.
[48]赵鹏大,胡旺亮,李紫金,等.矿产统计预测[M].北京：地质出版社,1983,1-115.
[49]王世称,范继璋,杨永华,等.矿产资源评价[M].吉林：吉林科学技术出版社,1987,151-157.
[50]高辉,JH ronsky,曹殿华,等.金川铜镍矿床成矿模式、控矿因素分析与找矿[J].地质与勘探.2009,45(3)：218-227.
[51]汤中立,任端进,薛增瑞,等.中国矿床.中国镍矿床[M].北京：地质出版社,1989,205-266.
[52]ZHAOPengda. "Three2step" quantitativeforeeastingandassessmentofresouree--theory of digitalexPlorationanddiseussiononPractiee[J]. EarthScience,2002,27(5):482-489
[53]CHENJianPing, ZHANGShouting, TANGJun, etal. Theoreticaleonsiderationtoquantitative foreeastingofnontraditionalmineralresouree[J]. ProgresslnGeophysies,2002,17(2):342-348.
[54]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
[55]姚敬金,张素兰,曹落华,等.中国土要大7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
[56]何政伟,孙传敏,朱章森.搜索法一一种无模型矿产预测的方法[J].矿物岩石,2000,20(3)：81-37.
[57]翟裕生,邓军,王建平,等.2004.深部找矿研究问题[J].矿床地质,23(2)：141-149.
[58]杨金中,方洪宾.中国西部重要成矿带遥感找矿异常提取的方法研究[J].国土资源遥感,2003,57(3)：50-53
[59]翟裕生,邓军,彭润民,等.2002.成矿系统研究及其资源、环境意义[J].高效地质学报,8(1)：1-8.
[60]甘甫平,王润生,马蔼乃,等.遥感地质信息提取集成与矿物遥感地质分析模型.遥感学报,2003,7(3)：208-213
[61]高亚林,汤中立,宋谢炎.金川铜镍矿隐伏富铜矿体成因研究及其深部找矿意义[J].岩石学报,2009,25(12)：3379-3395
[62]裴荣富.中国矿床模式[M].北京：地质出版社,1995：1-200.
[63]吴承烈,徐外生,刘崇民.中国主要类型铜矿勘查地球化学模刑[M].北京：地质出版社,1998：1-200.
[64]李文渊.岩浆Cu-Ni-PGE矿床研究现状及发展趋势[J].西北地质,2007,(2)：1-28.
[65]吕林素,刘裙,张作衡,等.中国岩浆型Ni-Cu-(PGE)硫化物矿床的时空分布及其地球动力学背景[J].岩石学报,2007,23(10)：2561-2594.
[66]汤中立,闫海卿,焦建刚,等.中国小岩体镍铜(铂族)矿床的区域成矿规律[J].地学前缘,2007,14(5)：92-103.
[67]成秋明.成矿过程奇异性与矿床多重分形分布[J].矿物岩石地球化学通报,2001,27(3)：298-305.
[68]陈毓川.中国主要成矿区带矿产资源远景评价[M].北京：地质出版社,1999.
[69]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.
[70]肖克炎,张晓华,李景朝.全国重要矿产总量预测方法[J].地学前缘,2007,14(5)：20-26.
[71]叶玉丰.基于GIS技术的矿产资源规划管理信息系统[J].地质与资源,2004,13(1)：52-64.
[72]肖克炎,丁建华,刘锐.美国“三步式”固体矿产资源潜力评价方法评述[J].地质论评,2006,52(6)：793-798.
[73]尹建忠.多源信息综合分析在矿产资源潜力评价中的应用[D].成都理工大学,2004.
[74]林茂炳、苟宗海.四川龙门山造山带造山模式研究[M],成都：成都科技大学出版社,1996,33-62。
[75]高怀忠.新疆坡北镁铁-超镁铁岩带1号岩体地质特征及其含矿性研究[J].地球科学：中国地质大学学报,1992,17(4)：391-401.
[76]李鸿儒.新疆坡北镁铁-超镁铁岩带控岩构造及成矿专属性[J].中国区域地质,1994,3：227-233.
[77]杨甲全,钟莉,邓刚.北山地区坡北1号、10号基性-超基性岩体成矿预测及找矿方向[J].新疆地质,2002,20(3)：214-218.
[78]孙赫,秦克章,李金祥,徐兴旺,三金柱,丁奎首,惠卫尔,许英霞.2006.尔天山图拉尔根铜镍钴硫化物矿床岩相、岩石地球化学特征及其形成的构造背景[J].中国地质,33(3)：157-168.
[79]肖骑彬,蔡新平,徐兴旺.浅层地震与MT联合技术在隐伏金属矿定位预测中的应用[J].矿床地质,24
[80]詹艳,赵国泽,汤吉.1999.新疆玛纳斯大震区地壳深部的电性结构[J].地震地质,21(2)159-166.
[81]朱建军.浅谈东天山镜尔泉铜镍矿的成因及成矿规律[J].新疆有色金属2011,20(3)1-3.
[82]毛德宝等.阿尔金成矿带成矿规律与找矿预测[J].西北地质,2006,39(2)：114-127.
[83]姚凤良,孙丰月.矿床学教程[M].北京：地质出版社,2006.
[84]汤中立,钱壮志,姜常义.中国镍铜铂岩浆硫化物矿床与成矿预测[M].北京：地质出版社,2006.
[85]李文渊.中国硫化物铜镍矿床成矿系列与地球化学[M].西安：西安地图出版社,1996.