新疆乌恰地区Pb-Zn资源成矿预测与评价
|
摘要
铅锌矿是国土资源“十一五”规划《矿产资源保障工程》中的主攻矿种,也是新疆主要的矿产资源。新疆乌恰地区具有巨大的成矿潜力,孕育有丰富的铅锌等多金属矿产资源,本次研究针对乌恰地区铅锌矿床的特征、成因进行深入研究,分析区域成矿背景和成矿环境,揭示成矿规律,建立找矿模型,研发具有针对性和实效性的矿产勘查评价的方法组合和最佳模式,对于乌恰地区铅锌找矿工作取得快速突破具有十分重要的意义。
本论文依托“新疆和田铜镍、哈密铜镍金、乌恰铅锌、尼勒克阿拉斯坦铜金等成矿远景地段找矿靶区圈定与综合评价”项目选择新疆乌恰地区Pb、Zn做为研究对象,总结研究区的矿床时空演化特征和成矿规律,并在此基础上,以赵鹏大院士提出的“地质异常”成矿预测理论为指导,借助GIS技术,进行矿产资源预测与评价,圈定成矿有利地段和找矿靶区。
在全面收集整理研究区以往地质矿产工作资料的基础上,结合野外、室内研究,分析了研究区地质构演化历史与成矿的关系。同时初步建立了乌拉根矿床找矿模型。
系统的分析了研究区内1∶20万水系沉积物地球化学元素的分布特征,运用因子分析等多元统计方法研究了元素的组合关系,确定了研究区内成矿元素组合为Pb-Zn-Ag-Cd,并阐述了成矿元素组合的空间分布特征。采用C-A分形方法求得元素异常下限,并确定了元素异常区。
通过岩矿光谱机理及特征研究、图像数据统计分析,选取特征主成分分析方法,进行遥感蚀变信息的增强提取,研究改进了遥感异常的分级方法,评价蚀变信息的有效性,为遥感与化探信息的综合处理分析及靶区定位预测提供准确可靠的依据。
以“地质异常”成矿预测理论为指导,利用GIS技术,对乌恰地区地质、地球化学、遥感资料进行综合分析处理,提取致矿地质异常,并以建立乌恰地区证据权重模型为基础,计算各个预测单元的成矿有利度,依据后验概率的大小,最终圈定五个一级找矿远景靶区和四个二级找矿远景靶区。
Pb and Zn minerals are the main targets of the project of mineral resources security in the 11th five year plan of homeland resources and they are also the main mineral resources of Xinjiang Autonomous Region .There are huge mineral potential in Wuqia area, Xinjiang, and Pb and Zn minerals are rich there. In this thesis, I focused on the features and genesis of these deposits, analysis of the ore-forming background, discovering of ore-forming rules, forming exploration models and the research and development of combined methods and the best model with pertinence and actual effect for mineral exploration and assessment. It is meaningful for exploration in Wuqia.
Based on the project of delineation and synthetic assessment of perspective mineralized section in Xinjiang Hetian, Hami, Wuqia, Nilekealasitan, in this thesis I selected Pb and Zn deposits in Wuqia area as main subject. And the time-spatial evolution characters and mineralization rules in the area would be investigated and summarized. Directed by geoanomaly prediction theory which is put forward by Academician Zhao Pengda, and assisted by GIS, mineral prediction and assessment were carried out and preferable mineralized area and targets were delineated.
Through the collection of geologic data in the research area and the research both in field and in doors, the relationship between geological evolution history and ore forming was analyzed. The exploration model for Wulagen deposit was formed.
The distribution characteristics of stream sediment elements in 1:200,000 scale in the area were analyzed. To study the relationship among the elements, multivariable statistical methods (e.g. factor analysis)were used and the elements combination in this area was determined as Pb,Zn,Ag and Cd. The spatial distribution of this combination was also determined. The geochemical anomaly area was delineated by C-A fractal methods.
Through the study of spectrum mechanism of rock and mineral and the statistical of image data, the alteration information was extracted by principal component analysis. The study improved the grading methods of remote sensing anomaly and evaluated the effective of alteration information, which provided reliable basis for comprehensive analysis of remote sensing and geochemical data and for positioning prediction of the targets.
Directed by the mineral prediction theory of geo-anomaly, comprehensive analysis of geological, geochemical and remote sensing data were carried out by the means of GIS; ore-caused geo-anomalies were also extracted. Based on the model of weight of evidence formed in Wuqia area, ore-forming favorability in each prediction unit was calculated. According to posterior probability, five first level targets for prospecting were delineated.
本论文依托“新疆和田铜镍、哈密铜镍金、乌恰铅锌、尼勒克阿拉斯坦铜金等成矿远景地段找矿靶区圈定与综合评价”项目选择新疆乌恰地区Pb、Zn做为研究对象,总结研究区的矿床时空演化特征和成矿规律,并在此基础上,以赵鹏大院士提出的“地质异常”成矿预测理论为指导,借助GIS技术,进行矿产资源预测与评价,圈定成矿有利地段和找矿靶区。
在全面收集整理研究区以往地质矿产工作资料的基础上,结合野外、室内研究,分析了研究区地质构演化历史与成矿的关系。同时初步建立了乌拉根矿床找矿模型。
系统的分析了研究区内1∶20万水系沉积物地球化学元素的分布特征,运用因子分析等多元统计方法研究了元素的组合关系,确定了研究区内成矿元素组合为Pb-Zn-Ag-Cd,并阐述了成矿元素组合的空间分布特征。采用C-A分形方法求得元素异常下限,并确定了元素异常区。
通过岩矿光谱机理及特征研究、图像数据统计分析,选取特征主成分分析方法,进行遥感蚀变信息的增强提取,研究改进了遥感异常的分级方法,评价蚀变信息的有效性,为遥感与化探信息的综合处理分析及靶区定位预测提供准确可靠的依据。
以“地质异常”成矿预测理论为指导,利用GIS技术,对乌恰地区地质、地球化学、遥感资料进行综合分析处理,提取致矿地质异常,并以建立乌恰地区证据权重模型为基础,计算各个预测单元的成矿有利度,依据后验概率的大小,最终圈定五个一级找矿远景靶区和四个二级找矿远景靶区。
Pb and Zn minerals are the main targets of the project of mineral resources security in the 11th five year plan of homeland resources and they are also the main mineral resources of Xinjiang Autonomous Region .There are huge mineral potential in Wuqia area, Xinjiang, and Pb and Zn minerals are rich there. In this thesis, I focused on the features and genesis of these deposits, analysis of the ore-forming background, discovering of ore-forming rules, forming exploration models and the research and development of combined methods and the best model with pertinence and actual effect for mineral exploration and assessment. It is meaningful for exploration in Wuqia.
Based on the project of delineation and synthetic assessment of perspective mineralized section in Xinjiang Hetian, Hami, Wuqia, Nilekealasitan, in this thesis I selected Pb and Zn deposits in Wuqia area as main subject. And the time-spatial evolution characters and mineralization rules in the area would be investigated and summarized. Directed by geoanomaly prediction theory which is put forward by Academician Zhao Pengda, and assisted by GIS, mineral prediction and assessment were carried out and preferable mineralized area and targets were delineated.
Through the collection of geologic data in the research area and the research both in field and in doors, the relationship between geological evolution history and ore forming was analyzed. The exploration model for Wulagen deposit was formed.
The distribution characteristics of stream sediment elements in 1:200,000 scale in the area were analyzed. To study the relationship among the elements, multivariable statistical methods (e.g. factor analysis)were used and the elements combination in this area was determined as Pb,Zn,Ag and Cd. The spatial distribution of this combination was also determined. The geochemical anomaly area was delineated by C-A fractal methods.
Through the study of spectrum mechanism of rock and mineral and the statistical of image data, the alteration information was extracted by principal component analysis. The study improved the grading methods of remote sensing anomaly and evaluated the effective of alteration information, which provided reliable basis for comprehensive analysis of remote sensing and geochemical data and for positioning prediction of the targets.
Directed by the mineral prediction theory of geo-anomaly, comprehensive analysis of geological, geochemical and remote sensing data were carried out by the means of GIS; ore-caused geo-anomalies were also extracted. Based on the model of weight of evidence formed in Wuqia area, ore-forming favorability in each prediction unit was calculated. According to posterior probability, five first level targets for prospecting were delineated.
引文
[1]赵鹏大,陈永清.地质异常矿体定位的基本途径[J]。地球科学,1998, 23(2): 111-114.
[2]赵鹏大,陈永清.基于地质异常单元金矿找矿有利地段圈定与评价[J].地球科学, 1999, 24(5) : 443- 448.
[3]赵鹏大,胡旺亮,李紫金.矿床统计预测(第二版)[M].北京:地质出版社,1994.
[4]赵鹏大,池顺都,陈永清.查明地质异常:成矿预测的基础.高校地质学报,1996, 2(4): 361-373.
[5]赵鹏大.地质异常与成矿预测[M]∥陈毓川.当代地质矿产资源勘查评价的理论与方法.北京:地震出版社, 1999: 283-292.
[6]赵鹏大,陈永清,金友渔.基于地质异常的“5P”找矿地段的定量圈定与评价[J].地质论评, 2000, 46(增刊) : 6-16.
[7]赵仁夫等.西南天山地区矿产资源综合潜力评价成果报告[R].西安地质矿产研究所,2002.
[8] Singer Donald A.Some Suggested Future Directions of Quantitative Resource Assessments[J].Journal of China University of Geosciences, 2001,12(1):40-44.
[9]翟裕生,邓军,崔彬等.成矿系统及综合地质异常[J].现代地质,1999,13(1):100-103.
[10]徐忠祥,吴国平.灰色系统理论与矿床灰色预测[M].武汉:中国地质大学出版社, 1993.
[11]杨建功等.新疆乌恰地区铅锌多金属矿资源潜力评价地质工作总结报告[R].新疆鑫汇地质矿业有限责任公司,2003.
[12]中国地质学会数学地质专业委员会.中国数学地质(第8集)[M].北京:地质出版社, 1997.
[13]李长江,麻土华,朱兴盛.矿产勘查中的分形、混沌与ANN[M].北京:地质出版社, 1999.
[14]陈守余,周梅春.人工神经网络模拟实现与应用[M].武汉:中国地质大学出版社, 2000.
[15]赵鹏大,吕新彪.长江中下游地区地质异常及成矿预测BP模型[M].武汉:中国地质大学出版社, 1999.
[16] Katsuaki Koike, Setsuro Matsuda,Toru Suzuki,et al.Neural Network-Based Estimation ofPrincipal Metal Contents in the Hokuroku District,Northern Japan, for Exploring KurokoType Deposits[J]. Natural Resources Research,2002,11(2):135-156.
[17] Gavin J Bowden,Holger R Maier,Graeme C Dandy.Optimal division of data for neural network models in water resources applications[J].Water Resources Research, 2002,38(2):2(1-11).
[18]谢贤平,柴建设,童光煦.地质数据的BP网络分析方法[J].地质与勘探, 1995,31(2): 38-42.
[19]邓建,古德生,李夕兵.可视化自适应神经网络及在矿业中的应用[J].中南工业大学学报,2000,23 (3): 205-207.
[20] Hsu K, Gupta H V,Ssorooshian.Artificial neural network modeling of the rainfall-runoff process[J].Water Resources Research, 31(10):2517-2530.
[21]胡尊国,孟宪国.第一届全国分形理论与地质科学学术讨论会论文集[M].武汉:中国地质大学出版社, 1993.
[22]毛先成.香花岭锡矿床三维数学模型及深部盲矿预测[A].中国地质大学.矿产资源统计预测国际学术讨论会论文集[C].武汉:中国地质大学出版社,1990.
[23] Jonathan M Lees. Geotouch: software for three and four dimensional GIS in the earth sciences[J]. Computers&Geosicences,2000,26:751-761.
[24]池顺都,吴新林.云南元江地区GIS预测时的找矿有利度和空间相关性分析[J].地球科学,1998,23 (1):75-78.
[25]池顺都,周顺平,吴新林. GIS支持下的地质异常分析及金属矿产经验预测[J].地球科学,1997,22(1).
[26]曾佐勋,周继彬,刘立林,等.陕甘川邻接区基于MAPGIS的金成矿远景区预测[J].地学前缘,2001,8(1):416-419.
[27]池顺都,赵鹏大,刘粤湘.研究矿床时间谱系的GIS途径[J].地球科学,2001,26(2):180-184
[28]金友渔,赵鹏大.分形—判别非线性数学模型及勘探线剖面致矿地质异常分析[J].地质科技情报.2000,19(2):99-102.
[29]李新中,赵鹏大,肖克炎,胡光道.矿床统计预测单元划分的方法与程序[J].矿床地质, 1998,17(4):369-375.
[30]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(自然科学版),2003,30(5):441-446.
[31]赵鹏大,陈建平.地质异常理论与遥感地质研究[J].大自然探索,1996,15(56):29-34
[32]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床预测为例[J].地球科学,1998,23(2):125-128.
[33] Harris J R, Wilkinson L, Heather K, et al.Application of GIS Processing Techniques for Producing Mineral Prospectivity Maps-A Case Study:Mesothermal Au in the Swayze Greenstone Belt, Ontario[J].Canada Natural Resources Research, 2001,10(2):91-124.
[34] Rokos D, Argialas D, Mavrantza R,et al.Structural Analysis for Gold Mineralization Using Remote Sensing and Geochemical Techniques in a GIS Environment:Island of Lesvos[J]. Hellas Natural Resources Research,2000,9(4):277-294.
[35] Gao Yu,Hu Guangdao,Ma Hongchao.Application of GIS to Geological Information Extraction[J].Journal of China University of Geosciences,2000,11(2):183-185.
[36] Xiao Keyan, Zhang Xiaohua, Chen Zhenghui, et al.GIS A Tool to Change Traditional Way of Mineral Resources Appraisal[J].Journal of China University of Geosciences,2000,11(2):138-140.
[37] Chi Shundu, Zhao Pengda, Li Jianwei.Application of GIS to Geo-anomaly-Based Delineation of Mineral Resources [J].Journal of China University of Geosciences, 2000,11(2):164-167.
[38]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):74-82.
[39] Eastman R J,Fulk M. Long sequence time series evaluation using standardized principal components[J]. Photogrammetric Engineering and Remote Sensing,1993, 59 (8) :1307-1312
[40] Fung T, LeDrew E.Application of principal components analysis to change detection[J]. Photogrammetric Engineering and Remote Sensing,1987,53(12) :1649-1658.
[41] Haiyu Gao, Pengda Zhao, Jiahua Wang, et al. Updating of population parameters and credibility of discriminant analysis[J].Mathematical Geology,1999,31(3):249-275.
[42] Taylor R B, Steven T A.Definition of mineral resource potential[J].Economic Geology, 1983, 78:1268-1270.
[43] BonhamCarter G F, Agterberg F P, Weight D F.Weights of evidence modeling:A newapproach to mapping mineral potential[C]//Agterberg F P, BonhamCarter G F (eds.). StatisticalApplications in the Earth Science.Geological Survey of Canada Paper 89-90.1989:171-183.
[44] BonhamCarter G F.Geographic Information Systems for Geoscientist:Modelling with GIS[M].1994:317-337.
[45] Scott M,Dimitrakopoulos R.Quantitative analysis of mineral resources for strategic planning : implications for Australian geological surveys[J].Natural Resource Research ,2001,10 (3):159-177.
[46]陈永清,陈建国,汪新庆.基于GIS的矿产资源综合定量评价[J].地质通报, 2007,26(2):141-149.
[47]王世称,王于天.综合信息解译的原理与方法[M].长春:吉林大学出版社,1989:164
[48] Chen Yongqing, Zhao Pengda.The delineated methods of geological anomaly units and its application in the statistical predication of gold deposits of large scale[M].Proc.30th Int'l. Geo. Congr.(Volume 25), Mathematical Geology and Geoinformatics. Zhao Pengda et al(eds). VSP1997:23-32.
[49] Chen Yongqing, Liu Hongguang. Delineation of potential mineral resources region based on geoanomaly [J].Journal of China University of Geosciences,2000,11(2):158-163.
[50] Chen Yongqing, Zhao Pengda.Application of the geo-anomaly unit concept in quantitative delineation and assessment of gold ore targets in western Shandong uplift terrain,Eastern China[J].Natural Resources Research,2001,10(1):35-49.
[51] Bonham- Carter G F.Geographic Information Systems for Geoscientists:Modelling with GIS[M].Pergamon /Elsevier Science Publications, 1996:398.
[52] Harris D P.Agterberg F P. The appraisal of mineral resources[M]/ /Skinner B J. Economic Geology.Seventy- Fifth Anniversary Volume,1981:897- 938.
[53]陈永清,刘红光.初论地质异常数字找矿模型[J].地球科学, 2001, 26(2):129-134.
[54] Singer D A. Basic concepts in three- part quantitative assessments of undiscovered mineral resources[J]. Nonrenewable Resources,1993, 2(2): 69- 81.
[55] Reed B L, Menzie W D, McDermott M.Undiscovered lode tin resources of the Seward Peninsula, Alaska[J]. Economic Geology, 1989, 84: 1936- 1947.
[56] Hu Guangdao, Chen Jianguo, Chen Shouyu. Metallic mineral resources assessment andanalysis system design[J].Journal of China University of Geosciences,2000, 11(3): 308-311.
[57]赵鹏大,池顺都.当今矿产勘探问题思考[J].地球科学,1998,23(1):70-74.
[58]赵鹏大.“三联式”资源定量预测与评价——数字找矿理论与实践探讨[J].地球科学.2002,27(5):482～489.
[59] Cheng Q, Agterberg F P, Ballantyne S B.The separation of geochemical anomalies from background by fractal methods[J].Journal of Exploration Geochemistry, 1994, 51(2):109-130.
[60] Cheng Q, Xu Y, Grunsky E.Integrated spatial and spectrum method for geochemical anomaly separation[J]. Natural Resources Research, 2000, 9(1):43-51.
[61] Chen Y Q, Zhang S Y, Liu H G.Application of multi-fractal methods in extracting geochemical anomalies in western Yunnan Province,southwestern China with GeoDAS3.0 Software[M]/ /Qiuming Cheng, Graeme Bonham- Cater.Proceedings of IAMG′05 GIS and Spatial Analysis.Toronto, Canada,2005,1:487- 492.
[62] Guocheng Pan,Harris D P.Information synthesis for mineral exploration[M].Oxford University Press, 2000:461.
[63]瞿裕生,邓军,李晓波.区域成矿学[M].北京:地质出版社,1999.4-14.
[64]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):69-71.
[65]朱裕生,李纯杰.成矿地质背景分析[M].北京:地质出版社,1997: 1-143.
[66]王安建,侯增谦,李晓波,等.成矿理论与勘查技术方法现状与发展趋势[J].中国地质, 2000, 1: 30-33.
[67]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.
[68]赵鹏大,陈建平,陈建国.成矿多样性与矿床谱系[J].地球科学.2001,26(2):111～117.
[69]陈毓川,朱裕生等编著.中国矿床成矿模式.北京地质出版社, 1993.1-367.
[70]肖克炎,朱裕生,宋国耀.矿产资源GIS定量评价.中国地质,总278期2000. (7):29-32.
[71]肖克炎,张晓华,王四龙.矿产资源GIS评价系统北京:地质出版社, 2000.1-213.
[72]薛顺荣,胡光道,丁俊.成矿预测研究现状及发展趋势[J].云南地质,2001,20(4):411-416.
[73]廖崇高,陈建平.基于GIS空间分析进行多源信息成矿预测[J].物探化探计算技术,2002,24(2):146-150.
[74]杨中宝,彭省临,李朝艳.信息科学与矿产预测[J].地球科学与环境学报,2005, 17(2):39-42.
[75]朱裕生.矿产预测的基本理论[J].矿床地质,2006,25(增刊):59-62.
[76]翟裕生.论成矿系统[J].地学前缘,1999, 6(1):13-27.
[77] ZhaiY S, Deng J, Peng R M.Issues on China regional metallogeny [J].Journal of China University of Geosciences,2000,11(3):220-227.
[78]翟裕生.中国区域成矿特征的探讨[ J].地质与勘探,2002, 38(5): 1-4.
[79]翟裕生,邓军,王建平,等.深部找矿研究问题[ J].矿床地质, 2004, 23(2): 142-149.
[80] DAVID W.EATON,BERND MILKEREIT,MATTHEW SALISBURY. Seismic methods for deep mineral exploration: Mature technologies adapted to new targets. THE LEADING EDGE .2003,580～585.
[81] LAWRENCE M. GOCHIOCO , MILOVAN UROSEVIC. An introduction—Mining geophysics.The Leading edge.2003,557
[82]高珍权,刘继顺,舒广龙,匡文龙,胡江春.新疆乌恰地区中新生代盆地寻找热卤水成因的超大型铅锌矿床的地球化学证据[J].地质地球化学.2002,30(1):13-19.
[83]高珍权,刘继顺,舒广龙,匡文龙.胡江春.新疆乌恰铅锌矿床成矿的地质条件及成因[J].中南工业大学学报.2002,33(2):116-120.
[84]蔡宏渊,邓贵安,郑跃鹏.新疆乌拉根铅锌矿床成因探讨[J].矿产与地质2002,16(88):1-5.
[85]Харченков.A.Г.Принципыиметодыпрогнозированияминеральныхресурсов[M] .Москва:Изд“.Недра”,1987.
[86]Нарсеев.В.А.Прогнознаяоценкаглубокихгоризонтовифранговзолоторудныхместорождений[ M] .Москва:Изд.“Недра”, 1989.
[87]Мишнин.В.М,Истомин.И.Н,Гриненко.В.С.Перспективыглубинногоизученияпотенциальногорудоносногосуперкомплекса“ЗападноЯкутскийриф”[ M ]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.Воронеж:Изд.Воронежскогогосударственногоуниверситета,2003.
[88]Некрасов.Е.М.Ещёразозначенииучения.Кретераогеологопромышленныхтипахрудныхместорождений[ J ].ГеологияиРазведка,Изв.ВУЗов, 2006(3):32-35.
[89]Шумилин.М.В.Орискахошибочнойотбраковкиперспективныхобъектовприпоисковооценочныхработахнауранипрограммеихпроведения[J ].РазведкаиОхранаНедр,2007(4):47-49.
[90]Аристов.А.А.Метоликаяеохимическихпоисковтвердыхископаемых《.Недра》. 1984.
[91]Бакулин.Ю.И.ТипизациярудоносныхвулканотектоническихструктурконтинентальнойокраинывостокаСССРипроблемаихместорождения.Хабаровск,1989.
[92]Дергачев.А.Л.ХилиДЖ.Казаченко.Л.Д.Финансово-экономическаяоценкаминеральныхместорождений[M].Изд-ВоМГУ,2000.
[93]Авдонин.В.В.БойцовВ.Е.идр.Месторожденияметаллическихполезныхископаемых.[M] .Москва:Изд,АкадемическийПроект,Трикста,2005.
[94]КомитетгеологииинедропользованияреспубликиказахстанНИИприродныхресурсовЮГГЕО.Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов)Алматы.2004.
[95]Лось.В.Л.ГольдбергИ.С.Геохимическиепоискискрытыхрудныхобьектов:базоваямодель,технология,организация//Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов).Алматы.2004С.42-59.
[96]Колоскова.С.М.Модельно–геохимическийметодпрогнозированияскрытогозолотогооруденения,связанногоспостмагматическимирудообразующимисистемами//Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов).Алматы,2004.91-104.
[97]Досанова.Б.А.Резервыминеральныхресурсовипоисковыегеохимическиетехнологии//Геологияиохрананедр.2003.№4(9)..63-67.
[98]СтаростинВ.И.,СтаростинП.А.Геологияполезныхископаемых[M].Москва.Изд. ?Академическийпроект?.2004.
[99]罗金海,周新源,邱斌,杨芝林,尹宏,尚新璐.塔里木盆地西部喀什凹陷褶皱冲断带的构造特征[J].石油与天然气地质.2004.25(2):199-203.
[100]钟大康,朱筱敏,王贵文,谢庆宾.塔里木盆地喀什凹陷侏罗纪古环境[J].古地理学报,2002,4(4):47-54.
[101]刘兆生.新疆乌恰县沙里塔什组生物地层新知[J].新疆地质,1996,14(1):86-91
[102]孙宝生,刘增仁,王招明.塔里木西南喀什凹陷几个地质问题的新认识[J].2003,21(1):78-84
[103]赵英时.遥感应用分析原理与方法[M].北京:科学出版社,2003.
[104]杨建民,张玉君,陈薇等.ETM+蚀变遥感异常技术方法在东天山戈壁地区的应用[J].矿床地质, 2003, 3: 178-284.
[105]杨建民,方洪宾,张玉君等.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, 3: 50-53.
[106]赵元洪,张福祥,陈南峰.波段比值的主成分复合在热液蚀变信息提取中的应用[J].国土资源遥感.1991,(3)12-17
[107]张守林.基于ETM数据矿化蚀变信息定量提取方法研究[D].北京:中国地质大学,2006.
[108] Andrea Z.,Salvi F,Chetta S, and et al.3D reconstruction of complex geological bodies: Examples from the Alps. Computers & Geosciences, 2009, 35: 49-69.
[109] Cengiz E, Yagmurlu F. A Satellite image approach to the study of linements, circular structures and regional geology in the Golcuk Crater District and its environs (Isparta, SW Turkey). Journal of Asian Earth Sciences, 2006, 155-163
[110] Cheng Q. M. Mapping Singularities with Stream Sediment Geochemical Data for Prediction of Undiscovered Mineral Deposits in Gejiu, Yunnan Province, China. Ore Geology Review, 2007, 32: 314–324
[111] GalleriniG., DeDonatis M. 3D modeling using geognostic data: The case of the low valley of Foglia river (Italy). Computers & Geosciences, 2009, 35:146-164
[112] Kaufmann O. Martin Th. Reprint of“3D geological modeling from boreholes, cross-sections and geological maps, application over former natural gas storages in coal mines. Computers & Geosciences, 2009, (35) 70-82
[113] Mallet J.L. Discrete modeling for nature objects. Mathematical Geology, 1997, 29(2): 199-218
[114]马建文.利用TM数据快速提取含矿蚀变带方法研究.遥感学报,1997,1(3)
[115]刘燕君.遥感找矿的原理和方法.北京:冶金工业出版社,1991
[116]丁建华,肖克炎.遥感技术在我国矿产资源预测评价中的应用.地球物理学进展,2006,21(2):588-593
[117]滕吉文,杨立强,姚敬全等..金属矿产资源的深部找矿-勘探与成矿的深层动力过程.地球物理学进展,200722(2): 317-334.
[118]高珍权,刘继顺,舒广龙,匡文龙,胡江春.新疆乌恰地区中新生代盆地寻找热卤水成因的超大型铅锌矿床的地球化学证据.地质地球化学.2002,30(1):13-19.
[119]ПоспееваЕВ.ГлубинноестроениеЮгаВосточнойСибирипорезультатаммагнитотеллурическихзондирований[M]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.Воронеж:Изд.Воронежскогогосударственногоуниверситета,2003.
[120]УаровВФ.СтроениенизовземнойкорыЮжнойчастиЯкутскойкимберлитовойпровинции[M]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.ВоронежИзд:Воронежскогогосударственногоуниверситета,2003.
[121]КороновскийН.В.,СтаростинВ.И.,АвдонинВ.В..Геологиядлягорногодела[M].Москва.Изд. ?Академия?.2007.
[2]赵鹏大,陈永清.基于地质异常单元金矿找矿有利地段圈定与评价[J].地球科学, 1999, 24(5) : 443- 448.
[3]赵鹏大,胡旺亮,李紫金.矿床统计预测(第二版)[M].北京:地质出版社,1994.
[4]赵鹏大,池顺都,陈永清.查明地质异常:成矿预测的基础.高校地质学报,1996, 2(4): 361-373.
[5]赵鹏大.地质异常与成矿预测[M]∥陈毓川.当代地质矿产资源勘查评价的理论与方法.北京:地震出版社, 1999: 283-292.
[6]赵鹏大,陈永清,金友渔.基于地质异常的“5P”找矿地段的定量圈定与评价[J].地质论评, 2000, 46(增刊) : 6-16.
[7]赵仁夫等.西南天山地区矿产资源综合潜力评价成果报告[R].西安地质矿产研究所,2002.
[8] Singer Donald A.Some Suggested Future Directions of Quantitative Resource Assessments[J].Journal of China University of Geosciences, 2001,12(1):40-44.
[9]翟裕生,邓军,崔彬等.成矿系统及综合地质异常[J].现代地质,1999,13(1):100-103.
[10]徐忠祥,吴国平.灰色系统理论与矿床灰色预测[M].武汉:中国地质大学出版社, 1993.
[11]杨建功等.新疆乌恰地区铅锌多金属矿资源潜力评价地质工作总结报告[R].新疆鑫汇地质矿业有限责任公司,2003.
[12]中国地质学会数学地质专业委员会.中国数学地质(第8集)[M].北京:地质出版社, 1997.
[13]李长江,麻土华,朱兴盛.矿产勘查中的分形、混沌与ANN[M].北京:地质出版社, 1999.
[14]陈守余,周梅春.人工神经网络模拟实现与应用[M].武汉:中国地质大学出版社, 2000.
[15]赵鹏大,吕新彪.长江中下游地区地质异常及成矿预测BP模型[M].武汉:中国地质大学出版社, 1999.
[16] Katsuaki Koike, Setsuro Matsuda,Toru Suzuki,et al.Neural Network-Based Estimation ofPrincipal Metal Contents in the Hokuroku District,Northern Japan, for Exploring KurokoType Deposits[J]. Natural Resources Research,2002,11(2):135-156.
[17] Gavin J Bowden,Holger R Maier,Graeme C Dandy.Optimal division of data for neural network models in water resources applications[J].Water Resources Research, 2002,38(2):2(1-11).
[18]谢贤平,柴建设,童光煦.地质数据的BP网络分析方法[J].地质与勘探, 1995,31(2): 38-42.
[19]邓建,古德生,李夕兵.可视化自适应神经网络及在矿业中的应用[J].中南工业大学学报,2000,23 (3): 205-207.
[20] Hsu K, Gupta H V,Ssorooshian.Artificial neural network modeling of the rainfall-runoff process[J].Water Resources Research, 31(10):2517-2530.
[21]胡尊国,孟宪国.第一届全国分形理论与地质科学学术讨论会论文集[M].武汉:中国地质大学出版社, 1993.
[22]毛先成.香花岭锡矿床三维数学模型及深部盲矿预测[A].中国地质大学.矿产资源统计预测国际学术讨论会论文集[C].武汉:中国地质大学出版社,1990.
[23] Jonathan M Lees. Geotouch: software for three and four dimensional GIS in the earth sciences[J]. Computers&Geosicences,2000,26:751-761.
[24]池顺都,吴新林.云南元江地区GIS预测时的找矿有利度和空间相关性分析[J].地球科学,1998,23 (1):75-78.
[25]池顺都,周顺平,吴新林. GIS支持下的地质异常分析及金属矿产经验预测[J].地球科学,1997,22(1).
[26]曾佐勋,周继彬,刘立林,等.陕甘川邻接区基于MAPGIS的金成矿远景区预测[J].地学前缘,2001,8(1):416-419.
[27]池顺都,赵鹏大,刘粤湘.研究矿床时间谱系的GIS途径[J].地球科学,2001,26(2):180-184
[28]金友渔,赵鹏大.分形—判别非线性数学模型及勘探线剖面致矿地质异常分析[J].地质科技情报.2000,19(2):99-102.
[29]李新中,赵鹏大,肖克炎,胡光道.矿床统计预测单元划分的方法与程序[J].矿床地质, 1998,17(4):369-375.
[30]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(自然科学版),2003,30(5):441-446.
[31]赵鹏大,陈建平.地质异常理论与遥感地质研究[J].大自然探索,1996,15(56):29-34
[32]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床预测为例[J].地球科学,1998,23(2):125-128.
[33] Harris J R, Wilkinson L, Heather K, et al.Application of GIS Processing Techniques for Producing Mineral Prospectivity Maps-A Case Study:Mesothermal Au in the Swayze Greenstone Belt, Ontario[J].Canada Natural Resources Research, 2001,10(2):91-124.
[34] Rokos D, Argialas D, Mavrantza R,et al.Structural Analysis for Gold Mineralization Using Remote Sensing and Geochemical Techniques in a GIS Environment:Island of Lesvos[J]. Hellas Natural Resources Research,2000,9(4):277-294.
[35] Gao Yu,Hu Guangdao,Ma Hongchao.Application of GIS to Geological Information Extraction[J].Journal of China University of Geosciences,2000,11(2):183-185.
[36] Xiao Keyan, Zhang Xiaohua, Chen Zhenghui, et al.GIS A Tool to Change Traditional Way of Mineral Resources Appraisal[J].Journal of China University of Geosciences,2000,11(2):138-140.
[37] Chi Shundu, Zhao Pengda, Li Jianwei.Application of GIS to Geo-anomaly-Based Delineation of Mineral Resources [J].Journal of China University of Geosciences, 2000,11(2):164-167.
[38]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):74-82.
[39] Eastman R J,Fulk M. Long sequence time series evaluation using standardized principal components[J]. Photogrammetric Engineering and Remote Sensing,1993, 59 (8) :1307-1312
[40] Fung T, LeDrew E.Application of principal components analysis to change detection[J]. Photogrammetric Engineering and Remote Sensing,1987,53(12) :1649-1658.
[41] Haiyu Gao, Pengda Zhao, Jiahua Wang, et al. Updating of population parameters and credibility of discriminant analysis[J].Mathematical Geology,1999,31(3):249-275.
[42] Taylor R B, Steven T A.Definition of mineral resource potential[J].Economic Geology, 1983, 78:1268-1270.
[43] BonhamCarter G F, Agterberg F P, Weight D F.Weights of evidence modeling:A newapproach to mapping mineral potential[C]//Agterberg F P, BonhamCarter G F (eds.). StatisticalApplications in the Earth Science.Geological Survey of Canada Paper 89-90.1989:171-183.
[44] BonhamCarter G F.Geographic Information Systems for Geoscientist:Modelling with GIS[M].1994:317-337.
[45] Scott M,Dimitrakopoulos R.Quantitative analysis of mineral resources for strategic planning : implications for Australian geological surveys[J].Natural Resource Research ,2001,10 (3):159-177.
[46]陈永清,陈建国,汪新庆.基于GIS的矿产资源综合定量评价[J].地质通报, 2007,26(2):141-149.
[47]王世称,王于天.综合信息解译的原理与方法[M].长春:吉林大学出版社,1989:164
[48] Chen Yongqing, Zhao Pengda.The delineated methods of geological anomaly units and its application in the statistical predication of gold deposits of large scale[M].Proc.30th Int'l. Geo. Congr.(Volume 25), Mathematical Geology and Geoinformatics. Zhao Pengda et al(eds). VSP1997:23-32.
[49] Chen Yongqing, Liu Hongguang. Delineation of potential mineral resources region based on geoanomaly [J].Journal of China University of Geosciences,2000,11(2):158-163.
[50] Chen Yongqing, Zhao Pengda.Application of the geo-anomaly unit concept in quantitative delineation and assessment of gold ore targets in western Shandong uplift terrain,Eastern China[J].Natural Resources Research,2001,10(1):35-49.
[51] Bonham- Carter G F.Geographic Information Systems for Geoscientists:Modelling with GIS[M].Pergamon /Elsevier Science Publications, 1996:398.
[52] Harris D P.Agterberg F P. The appraisal of mineral resources[M]/ /Skinner B J. Economic Geology.Seventy- Fifth Anniversary Volume,1981:897- 938.
[53]陈永清,刘红光.初论地质异常数字找矿模型[J].地球科学, 2001, 26(2):129-134.
[54] Singer D A. Basic concepts in three- part quantitative assessments of undiscovered mineral resources[J]. Nonrenewable Resources,1993, 2(2): 69- 81.
[55] Reed B L, Menzie W D, McDermott M.Undiscovered lode tin resources of the Seward Peninsula, Alaska[J]. Economic Geology, 1989, 84: 1936- 1947.
[56] Hu Guangdao, Chen Jianguo, Chen Shouyu. Metallic mineral resources assessment andanalysis system design[J].Journal of China University of Geosciences,2000, 11(3): 308-311.
[57]赵鹏大,池顺都.当今矿产勘探问题思考[J].地球科学,1998,23(1):70-74.
[58]赵鹏大.“三联式”资源定量预测与评价——数字找矿理论与实践探讨[J].地球科学.2002,27(5):482～489.
[59] Cheng Q, Agterberg F P, Ballantyne S B.The separation of geochemical anomalies from background by fractal methods[J].Journal of Exploration Geochemistry, 1994, 51(2):109-130.
[60] Cheng Q, Xu Y, Grunsky E.Integrated spatial and spectrum method for geochemical anomaly separation[J]. Natural Resources Research, 2000, 9(1):43-51.
[61] Chen Y Q, Zhang S Y, Liu H G.Application of multi-fractal methods in extracting geochemical anomalies in western Yunnan Province,southwestern China with GeoDAS3.0 Software[M]/ /Qiuming Cheng, Graeme Bonham- Cater.Proceedings of IAMG′05 GIS and Spatial Analysis.Toronto, Canada,2005,1:487- 492.
[62] Guocheng Pan,Harris D P.Information synthesis for mineral exploration[M].Oxford University Press, 2000:461.
[63]瞿裕生,邓军,李晓波.区域成矿学[M].北京:地质出版社,1999.4-14.
[64]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):69-71.
[65]朱裕生,李纯杰.成矿地质背景分析[M].北京:地质出版社,1997: 1-143.
[66]王安建,侯增谦,李晓波,等.成矿理论与勘查技术方法现状与发展趋势[J].中国地质, 2000, 1: 30-33.
[67]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.
[68]赵鹏大,陈建平,陈建国.成矿多样性与矿床谱系[J].地球科学.2001,26(2):111～117.
[69]陈毓川,朱裕生等编著.中国矿床成矿模式.北京地质出版社, 1993.1-367.
[70]肖克炎,朱裕生,宋国耀.矿产资源GIS定量评价.中国地质,总278期2000. (7):29-32.
[71]肖克炎,张晓华,王四龙.矿产资源GIS评价系统北京:地质出版社, 2000.1-213.
[72]薛顺荣,胡光道,丁俊.成矿预测研究现状及发展趋势[J].云南地质,2001,20(4):411-416.
[73]廖崇高,陈建平.基于GIS空间分析进行多源信息成矿预测[J].物探化探计算技术,2002,24(2):146-150.
[74]杨中宝,彭省临,李朝艳.信息科学与矿产预测[J].地球科学与环境学报,2005, 17(2):39-42.
[75]朱裕生.矿产预测的基本理论[J].矿床地质,2006,25(增刊):59-62.
[76]翟裕生.论成矿系统[J].地学前缘,1999, 6(1):13-27.
[77] ZhaiY S, Deng J, Peng R M.Issues on China regional metallogeny [J].Journal of China University of Geosciences,2000,11(3):220-227.
[78]翟裕生.中国区域成矿特征的探讨[ J].地质与勘探,2002, 38(5): 1-4.
[79]翟裕生,邓军,王建平,等.深部找矿研究问题[ J].矿床地质, 2004, 23(2): 142-149.
[80] DAVID W.EATON,BERND MILKEREIT,MATTHEW SALISBURY. Seismic methods for deep mineral exploration: Mature technologies adapted to new targets. THE LEADING EDGE .2003,580～585.
[81] LAWRENCE M. GOCHIOCO , MILOVAN UROSEVIC. An introduction—Mining geophysics.The Leading edge.2003,557
[82]高珍权,刘继顺,舒广龙,匡文龙,胡江春.新疆乌恰地区中新生代盆地寻找热卤水成因的超大型铅锌矿床的地球化学证据[J].地质地球化学.2002,30(1):13-19.
[83]高珍权,刘继顺,舒广龙,匡文龙.胡江春.新疆乌恰铅锌矿床成矿的地质条件及成因[J].中南工业大学学报.2002,33(2):116-120.
[84]蔡宏渊,邓贵安,郑跃鹏.新疆乌拉根铅锌矿床成因探讨[J].矿产与地质2002,16(88):1-5.
[85]Харченков.A.Г.Принципыиметодыпрогнозированияминеральныхресурсов[M] .Москва:Изд“.Недра”,1987.
[86]Нарсеев.В.А.Прогнознаяоценкаглубокихгоризонтовифранговзолоторудныхместорождений[ M] .Москва:Изд.“Недра”, 1989.
[87]Мишнин.В.М,Истомин.И.Н,Гриненко.В.С.Перспективыглубинногоизученияпотенциальногорудоносногосуперкомплекса“ЗападноЯкутскийриф”[ M ]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.Воронеж:Изд.Воронежскогогосударственногоуниверситета,2003.
[88]Некрасов.Е.М.Ещёразозначенииучения.Кретераогеологопромышленныхтипахрудныхместорождений[ J ].ГеологияиРазведка,Изв.ВУЗов, 2006(3):32-35.
[89]Шумилин.М.В.Орискахошибочнойотбраковкиперспективныхобъектовприпоисковооценочныхработахнауранипрограммеихпроведения[J ].РазведкаиОхранаНедр,2007(4):47-49.
[90]Аристов.А.А.Метоликаяеохимическихпоисковтвердыхископаемых《.Недра》. 1984.
[91]Бакулин.Ю.И.ТипизациярудоносныхвулканотектоническихструктурконтинентальнойокраинывостокаСССРипроблемаихместорождения.Хабаровск,1989.
[92]Дергачев.А.Л.ХилиДЖ.Казаченко.Л.Д.Финансово-экономическаяоценкаминеральныхместорождений[M].Изд-ВоМГУ,2000.
[93]Авдонин.В.В.БойцовВ.Е.идр.Месторожденияметаллическихполезныхископаемых.[M] .Москва:Изд,АкадемическийПроект,Трикста,2005.
[94]КомитетгеологииинедропользованияреспубликиказахстанНИИприродныхресурсовЮГГЕО.Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов)Алматы.2004.
[95]Лось.В.Л.ГольдбергИ.С.Геохимическиепоискискрытыхрудныхобьектов:базоваямодель,технология,организация//Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов).Алматы.2004С.42-59.
[96]Колоскова.С.М.Модельно–геохимическийметодпрогнозированияскрытогозолотогооруденения,связанногоспостмагматическимирудообразующимисистемами//Поисковаягеохимия:теоретическиеосновы,технологии,результаты(Сборникнаучныхдокладов).Алматы,2004.91-104.
[97]Досанова.Б.А.Резервыминеральныхресурсовипоисковыегеохимическиетехнологии//Геологияиохрананедр.2003.№4(9)..63-67.
[98]СтаростинВ.И.,СтаростинП.А.Геологияполезныхископаемых[M].Москва.Изд. ?Академическийпроект?.2004.
[99]罗金海,周新源,邱斌,杨芝林,尹宏,尚新璐.塔里木盆地西部喀什凹陷褶皱冲断带的构造特征[J].石油与天然气地质.2004.25(2):199-203.
[100]钟大康,朱筱敏,王贵文,谢庆宾.塔里木盆地喀什凹陷侏罗纪古环境[J].古地理学报,2002,4(4):47-54.
[101]刘兆生.新疆乌恰县沙里塔什组生物地层新知[J].新疆地质,1996,14(1):86-91
[102]孙宝生,刘增仁,王招明.塔里木西南喀什凹陷几个地质问题的新认识[J].2003,21(1):78-84
[103]赵英时.遥感应用分析原理与方法[M].北京:科学出版社,2003.
[104]杨建民,张玉君,陈薇等.ETM+蚀变遥感异常技术方法在东天山戈壁地区的应用[J].矿床地质, 2003, 3: 178-284.
[105]杨建民,方洪宾,张玉君等.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, 3: 50-53.
[106]赵元洪,张福祥,陈南峰.波段比值的主成分复合在热液蚀变信息提取中的应用[J].国土资源遥感.1991,(3)12-17
[107]张守林.基于ETM数据矿化蚀变信息定量提取方法研究[D].北京:中国地质大学,2006.
[108] Andrea Z.,Salvi F,Chetta S, and et al.3D reconstruction of complex geological bodies: Examples from the Alps. Computers & Geosciences, 2009, 35: 49-69.
[109] Cengiz E, Yagmurlu F. A Satellite image approach to the study of linements, circular structures and regional geology in the Golcuk Crater District and its environs (Isparta, SW Turkey). Journal of Asian Earth Sciences, 2006, 155-163
[110] Cheng Q. M. Mapping Singularities with Stream Sediment Geochemical Data for Prediction of Undiscovered Mineral Deposits in Gejiu, Yunnan Province, China. Ore Geology Review, 2007, 32: 314–324
[111] GalleriniG., DeDonatis M. 3D modeling using geognostic data: The case of the low valley of Foglia river (Italy). Computers & Geosciences, 2009, 35:146-164
[112] Kaufmann O. Martin Th. Reprint of“3D geological modeling from boreholes, cross-sections and geological maps, application over former natural gas storages in coal mines. Computers & Geosciences, 2009, (35) 70-82
[113] Mallet J.L. Discrete modeling for nature objects. Mathematical Geology, 1997, 29(2): 199-218
[114]马建文.利用TM数据快速提取含矿蚀变带方法研究.遥感学报,1997,1(3)
[115]刘燕君.遥感找矿的原理和方法.北京:冶金工业出版社,1991
[116]丁建华,肖克炎.遥感技术在我国矿产资源预测评价中的应用.地球物理学进展,2006,21(2):588-593
[117]滕吉文,杨立强,姚敬全等..金属矿产资源的深部找矿-勘探与成矿的深层动力过程.地球物理学进展,200722(2): 317-334.
[118]高珍权,刘继顺,舒广龙,匡文龙,胡江春.新疆乌恰地区中新生代盆地寻找热卤水成因的超大型铅锌矿床的地球化学证据.地质地球化学.2002,30(1):13-19.
[119]ПоспееваЕВ.ГлубинноестроениеЮгаВосточнойСибирипорезультатаммагнитотеллурическихзондирований[M]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.Воронеж:Изд.Воронежскогогосударственногоуниверситета,2003.
[120]УаровВФ.СтроениенизовземнойкорыЮжнойчастиЯкутскойкимберлитовойпровинции[M]∥Проблемыпрогнозирования,поисковиизученияместорожденийполезныхископаемыхнапорогеXXIвека.ВоронежИзд:Воронежскогогосударственногоуниверситета,2003.
[121]КороновскийН.В.,СтаростинВ.И.,АвдонинВ.В..Геологиядлягорногодела[M].Москва.Изд. ?Академия?.2007.