用户名: 密码: 验证码:
广西南丹大厂锡矿长坡—高峰矿床(山)数字化与综合信息成矿预测
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
本博士论文“广西南丹大厂锡矿长坡-高峰矿床(山)数字化与综合信息成矿预测”是结合国土资源部下达的2005年度危机矿山接替资源勘查项目,即“广西南丹铜坑锡矿接替资源勘查”项目(项目编码200545022)的科研需要而选题。
     改革开放以来,随着经济的飞速发展,我国对矿产资源的需求与日俱增,而目前我们国家各主要矿种的资源保证程度相当低,矿产资源的形势非常严峻,严重威胁着国家的经济安全和社会稳定。为了改变这种形势,我们必须依赖于科技进步,积极探索新的、更有效的现代成矿预测理论与高新技术有机结合的矿产资源预测体系,整体提升我国矿产资源勘查评价水平和科学预测能力,寻找和发现新的矿产资源品种和类型,增加矿产资源的储备,为我国经济安全、高效、持续发展提供资源保证。
     本博士论文结合课题的研究需要,瞄准我国矿业和地质勘探行业发展的前沿,从近期在铜坑成矿区火山岩—次火山岩的重要发现入手,研究分析火山岩—次火山岩的地质特征。其次,在鉴于国内外矿山数字化信息系统软件现状分析的基础上,取长补短,通过深化改造自行开发的“矿床数学-经济模型”软件包,同时以国内外软件Surpac, Micrmine和Mapgis为辅助,作为长坡—高峰矿床(山)数字化信息系统的软件平台,建立长坡—高峰矿区的矿山数字化信息系统,建立三维数字地学模型,通过模型综合分析研究,提出三维异常地段。第三,在成矿理论的指导下,对矿区控矿因素与成矿信息进行空间分析研究,建立综合信息找矿模型,开展综合信息成矿预测研究。
     在对前人研究成果的充分借鉴和吸收的前提下,我们开展了广泛的野外及井下地质调查和室内的综合研究工作,主要包括矿床的宏观和微观地质特征研究,典型矿床的解剖,地球化学特征和矿床类型的厘定及成因模式的探讨,矿山数字化信息系统研究,矿床地物化遥多源地学信息特征的分析和综合信息找矿模型的研究、控矿因素和找矿标志分析、基于GIS空间分析的综合信息成矿预测研究,及矿床(山)数字化的靶区优选等,通过上述研究主要得到以下成果:
     1、通过铜坑矿区火山岩—次火山岩及其与成矿关系的初步研究,取得矿床成因理论上的新认识。研究表明:在长坡—高峰矿区,除了存在传统的燕山晚期花岗岩成矿作用外,至少还存在海西早期海底基性火山—喷流沉积成矿作用和海底沉积—喷流成矿作用,取得了该区成矿理论上的突破。
     2、通过区域成矿地学背景和矿床地质特征研究,认为本区的成矿物质具有多来源性,提供物源的地质体主要有前寒武系的古老基底、寒武纪、泥盆纪地层、基性火山岩和燕山晚期构造岩浆热液等。长坡—高峰锡多金属矿床的成矿作用经历了多期次多阶段,为“多因复成”矿床。
     3、运用系统论的观点,详尽地研究了长坡—高峰矿区的大地构造演化,矿体产出位置和形态产状、矿物组合及矿石组构、控矿规律,及成矿作用、成矿时代和矿床成因模式。指出在长坡—高峰矿区进行火山喷流沉积矿床成矿理论的研究,不仅可以取得矿床成因理论上的突破,而且对于指导矿山的找矿勘探具有明显的现实意义。这一结论已得到了生产勘探实践的证实。
     4、根据矿区地层、岩浆岩和矿床的宏观和微观资料的综合分析研究,认为长坡—高峰矿区成矿与南北向同构造岩浆带(东岩墙)演化关系密切。“东岩墙”在泥盆纪是南北向的同生断裂带,控制了泥盆纪基性火山作用和喷流沉积成矿作用。整个矿区成矿与南北向同构造岩浆带的海底火山—沉积热水沉积成矿作用、喷流—热水沉积和后期构造岩浆叠加改造有关的热液成矿作用有密切关系,具有成岩成矿多阶段,形成矿种多的特点。这从而为综合信息成矿模型的建立提供了理论依据。
     5、通过矿床(山)数字化研究,对长坡—高峰矿区矿体、地形、地层、构造、岩浆岩、钻孔原生晕和探采工程等信息进行全方位立体建模,建立三维数字地学信息模型。通过模型的三维综合空间分析研究,提出三个三维异常地段,为综合信息找矿靶区优选提供依据。
     6、通过分析长坡—高峰矿区成矿地质背景入手,在火山喷流沉积成矿理论认识的指导下,对各种控矿因素(基底、地层、岩浆岩和构造)与成矿信息(矿床、矿点、矿化点、物探异常、化探异常和遥感地质)在空间分布上的相关关系进行研究,并用控矿因素对各种成矿信息在空间分布上的控制规律,确定各种控矿因素与成矿作用的密切程度,建立综合信息矿产资源找矿模型,提出了找矿靶区10个。
     7、通过数字化三维异常地段与综合信息找矿靶区空间分析,结合已有探矿工程见矿信息,优选出找矿靶区3个。分别是:长坡南-巴里-高峰深部靶区(Ⅰ-3)、长坡区大厂断裂下盘一带深部叠瓦状构造带靶区(Ⅰ-2)和V号盲矿体以北及东岩墙以东靶区(Ⅱ-2)。它们将为矿山扩建及下一步的地质找矿和资源评价工作提供依据。
The doctoral dissertation, The Digital Mine and Comprehensive Information Minerogenetic Prognosis of Dachang Changpo-Gaofeng Area, is based on the scientific research requirements for the project, The Resources Exploration in Tongkeng Tin Deposit of Guangxi Nadan(Serial number:200545022), a sub-project of The Resources Exploration of The Crisis Mine in 2005 sponsored the Ministry of Land and Resources, P.R.C.
     With the rapid economic development since the reform and opening up in China, We are demanding for increasing mineral resources. But at present our country's major mineral resources to guarantee is in a very low level, which is very serious. Mineral resources serious throated to the country's economic security and social stability. In order to change this situation, we must rely on scientific and technological progress, and actively explore new, more effective modern metallogenic prediction theory and high-tech combination of mineral resources, projections system and enhancing the overall level of exploration and evaluation of mineral resources, and scientific prediction capabilities, search for and discovery of new varieties and types of mineral resources to increase the reserves of mineral resources for China's economic security, efficient and provide resources to ensure sustainable development.
     In the paper, connecting with the thesis research, targeting China's forefront mining and geological exploration development, we research and analysis of geological features based on the recent lava-sub lava discovery in Tongkeng deposit. Secondly, in view of domestic and international mining digital information system software, based on the own development "mathematical deposits-Economic Model" package, Surpac, Micrmine and Mapgis, we have created a Digital Mine Information System for the comprehensive information miner genetic prognosis and achieved three-dimensional digital geo-information model which gave anomaly bodies. Thirdly, under the guidance of the metallogenic theory, we established the information prospecting model, that can launch a comprehensive information metallogenic prediction by spatial analysis between mining geological characteristics and metallogenic information.
     In previous research results and to draw on the full context, we have carried out extensive field and mine geological survey and comprehensive study of indoor work, mainly including deposits geological characteristics of macro and micro studies, the typical anatomy of deposits, geochemical the determination of characteristics and deposit types and causes of patterns to explore mining of digital information systems research, DEPOSIT Physical characteristics of multi-source geo-information analysis and synthesis of information prospecting model studies, ore-controlling factors and prospecting criteria analysis, GIS-based spatial Analysis of integrated information metallogenic prediction, based on the digital deposit ore deposit deep edge prediction and so on, through the above-mentioned study is mainly supported by the following results:
     1.In Tongkeng area, we investigated through lava-sub lava and mineralization in the preliminary study of the relationship to obtain a new theoretical understanding of deposit mode of origin. Research shows that:In Changpo -Gaofeng diggings, in addition there is the traditional late Yanshan granite mineralization, the existence of at least the early Hercynian mafic submarine volcanic and sedimentary-exhalative mineralization and submarine exhalative hot water-the role of sedimentary mineralization and made a theoretical breakthrough in the area mineralization.
     2. Through the regional geological background and metallogenic geological characteristics of mining deposits that the district into a multi-source minerals, provide the source material of geological bodies are mainly the ancient pre-Cambrian basement, Cambrian, Devonian Department of carbonate rocks, basalt and mafic magmatic hydrothermal structures such as the late Yanshan. Changpo -Gaofeng diggings of the tin-polymetallic ore deposits in the role of experienced multi-stage multi-period, in order to "polygenetic" deposit.
     3. The use of system theory point of view, a detailed study of Changpo -Gaofeng diggings geotectonic evolution, occurrence condition and morphologic occurrence, mineral association, ore texture, metallotect, mineralization, metallogenetic epoch and deposit mode of origin. Pointed out that Changpo -Gaofeng diggings mining for volcanic exhalative sedimentary deposit, theoretical research, not only can obtain a theoretical breakthrough in ore genesis, but also for guiding the exploration of deposits of mines has obvious practical significance. This conclusion has been confirmed by the production of exploration.
     4. According to the study area strata, rocks and deposits of a comprehensive macro and micro data analysis and research that Changpo-Gaofeng diggings and North-South Summit to the synkinematic magmatic belt (east rock wall) evolution closely. In Devonian east rock wall was north-south contemporaneous fault, which controlled the devonian basic volcanic rock metallogenic mineralization and spout-sedimentary metallogenic mineralization.The ore-forming and North-South as a whole to the synkinematic magmatic belt of submarine volcanic-sedimentary hydrothermal sedimentary mineralization, jet stream-hot water deposition and post-structural transformation of magma-related hydrothermal superimposed mineralization is closely related with the rock-forming multi-stage, characterized by the formation of minerals and more. This is thus the establishment of integrated information metallogenic model provides a theoretical basis.
     5. By the digital mine study on Changpo -Gaofeng diggings mining geological characteristics (topography, stratigraphy, structure, igneous rock, drilling of the original halo and exploration and developing engineering) for full three-dimensional modeling, to achieve three-dimensional digital geo-information model. According to space geology analysis, it gave three anomaly bodies, which can optimize the comprehensive information targets.
     6. Based on volcanogenic sedimentary hypothesis in Changpo-Gaofeng diggings metalloginic geology, I compared in space between controlling ore factors (basement, strata, magmatic rock and structure) and metallogenic information (deposit, ore spot, mineralized spot, geophysical prospecting, geochemical exploration and remote sensing).I confirmed the affinity and found the comprehensive information prospecting model between controlling ore factors and metallogenic information by space analysis, which gave 10 targets.
     7. According to information correspondence analysis between three-dimensional target bodies and comprehensive information prospecting model, we gived 3 optimized prospecting targets combined with information of Mine Exploration Project. The south of Changpo-Bali-Deep Gaofeng target (Ⅰ-3), The Dachang fracture footwall of Changpo in deep Imbricate belt (Ⅰ-2)and The north of number V underground ore body and east of "east rock wall" target (Ⅱ-2),they provide a guarantee for the mine expansion and evaluation of geological prospecting.
引文
[1]秦德先.近年在我国三个特大型锡矿床中相继发现的火山(成矿)作用及其科学意义[J].昆明理工大学学报:理工版-2008年1期
    [2]夏湘蓉等.中国古代矿业开发史[M].北京:地质出版社,1980
    [3]广西大厂矿田成矿作用和物质成分研究报告[M].中国科学院地球化学研究所.1976.
    [4]李锡林,庄东臣.广西215矿区锡石硫化物矿床中硫岩矿物的初步研究[J].地质科学,1959,(8):236-240.
    [5]陈毓川.一个锡石多金属矿带中闪锌矿的成矿期与成矿特征[J].地质论评,1964,20(2):111-128.
    [6]陈毓川.广西某矿带原生带状分布[J].地质论评,1965,23(1):29-40.
    [7]杨凤筠,邱纯一等.硫同位素分析方法(在某热液型锡石—硫化物矿床中的应用)[J].地质科学,1966,(3):217-235.
    [8]章振根,李锡林,陈国玺.广西某锡石硫化物矿床磁黄铁矿的研究及其区别特征[J].地球化学,1976,(1):54-63.
    [9]陈毓川,黄民智等.大厂锡矿[M].北京:地质出版社,1997
    [10]叶俊,周怀阳等.大厂矿田锡石—硫化物矿床成矿机理[J].矿产与地质,1985,(3):40-45
    [11]叶绪孙.大厂锡多金属矿田成矿规律与成矿预测[J].地质与勘探,1983(6)
    [12]尹国栋.广西锡矿成矿规律及预测[J].桂林冶金地质学院学报,1985,5(3):231-237
    [13]刘元镇,钟铿,马林清.广西锡矿地质特征和成矿规律.(《锡矿地质讨论会论文集》),北京:地质出版社,1987:74-83
    [14]杨冀民.略论广西原生锡矿成矿特征及成矿条件[J].广西地质,1989,2(2):167-175
    [15]涂光炽.广西大厂矿床成因并兼论锡石硫化物矿床形成条件. (《锡矿地质讨论会论文集》),北京:地质出版社,1987:105-109
    [16]蔡宏渊,张国林.试论广西大厂锡多金属矿床海底火山热泉(喷气)成矿作用[J].冶金矿产地质研究院学报,1983,(4):13-21
    [17]雷良奇.大厂长坡锡多金属矿床成因刍议[J].矿床地质,1986,5(3):87-96
    [18]周怀阳,徐克勤,叶俊等.广西大厂层控锡石—硫化物多金属矿床的地质特征及形成机制探讨[J].南京大学学报(自然科学版),1987,23(3):533-541
    [19]张国林,蔡宏渊.广西大厂锡多金属矿床成因探讨[J].地质论评,1987,33(5):426-436
    [20]陈骏,周怀阳等.广西大厂沉积—热液叠加型锡矿床的成矿模拟实验[J].桂林冶金地质学院学报,1989,9(4):380-386
    [21]韩发,R.W.哈钦森.大厂锡-多金属矿床热液喷气沉积成因的证据——容矿岩石的微量元素及稀土元素地球化学[J].矿床地质,1989,8(3):33-41
    [22]韩发,R.W.哈钦森.大厂锡多金属矿床热液喷气沉积成因的证据——含矿建造及热液沉积岩[J].矿床地质,1989,8(3):25-37
    [23]韩发,R.W.哈钦森.大厂锡-多金属矿床喷气沉积成因的证据——矿床地质、地球化学特征[J].矿床地质,1990,9(4):309-324
    [24]徐新煌,蔡建明,陈洪德等.广西丹池矿带锡多金属矿床地质地球化学特征及成矿作用[J].成都地质学院学报,1991,(4):12-25
    [25]毛景文,陈晴勋,杨开泰等.桂北地区中元古代层纹状锡矿化的发现及其意义[J].矿床地质,1988,(1):46
    [26]广西大厂铜坑矿东岩墙以东成矿规律研究.昆明理工大学矿产地质研究所,2009.6
    [27]翟裕生.论成矿系统[J].地学前缘,1999,6(1):13-27
    [28]郭文魁.金属矿床地质的发展[J].矿床地质,1991,10(1):1-9
    [29]Zhu B-Q. The mapping of geochemical provinces in China based on pb isotopes, J. Geochem. Exploration.1995,55,171-181.
    [30]程裕淇,陈毓川,赵一鸣.初论矿床的成矿系列问题[J].中国地质科学院院报,1979,1(1):32-57
    [31]程裕淇,陈毓川,赵一鸣,宋人锐.再论矿床的成矿系列问题[J].中国地质科学院院报,1983,5(6):1-14
    [32]翟裕生,姚书振,崔彬等.成矿系列研究[M].武汉:中国地质大学出版社,1996
    [33]Zhu B Q. Discussion on geochemical division and affinity of East Asia blocks:Implications for tectonic framework[J], In:Metcalfe I, ed. Condwana Dispersion and Asian Accretion-Final Result of IUGS IGCP 321 [C], Netherland, A A Balkema Pub,1998,211~227.
    [34]程裕淇.中国大百科全书(地质卷)[M].北京:中国大百科全书出版社,1993,343-344
    [35]陈毓川,裴荣富,宋天锐.中国矿床成矿系列初论[M].北京:地质出版社,1998
    [36]广西南丹县铜坑锡矿资源潜力调查报告.柳州华锡集团有限责任公司,2005
    [37]Zhu B Q, Chang X Y, Qiu H N et al. Characteristics of Proterozoic basements on the geochemical steep zones in the continent of China and their implications for setting of super large deposits[J], Science in China(D),1998,41(Supp.):54~64.
    [38]Zhu B-Q, Dong Y-P, Chang X-Y, et al. Relation of isotopic geochemical steep zones with geophysical fields tectonics in the junction area of the Cathaysian, Yangtze and Indochia plates[J].Acta Geol Sinica,2000,74(2):236-240.
    [39]谢登科.我国将实施危机矿山接替资源找矿.新华社,2004年10月6日
    [40]翟裕生.成矿系列研究问题[J].现代地质,1992,6(3):301-308
    [41]Wang Yuwang, Jiang Fuzhi, Zhu Xinyou etal. The metallogenesis series of massive sulfide deposits related to marine volcanic rocks in Northwest China.9th, LAGOD, Abstracts, Beijing, China,1994:566-567
    [42]吕志成,段国正,刘丛强等.大兴安岭地区银矿床类型、成矿系列及成矿地球化学特征[J].矿物岩石地球化学通报,2000,19(4):305-309
    [43]翟裕生,熊永良.关于成矿系列的结构[J].地球科学-中国地质大学学报,1988.12(4):375-380
    [44]毛景文,王平安,毕承恩.矿床成矿系列在地质历史中的空间叠加、复合、并列和迁移[A].中国地质学会矿床地质专业委员会.第五届全国矿床会议论文集[C].北京:地质出版社,1993,25-27
    [45]毛德宝,王克卓,钟长汀等.阿尔金成矿带主要成矿系列及其地质特征[J].地质与勘探,2003,39(5):1-5
    [46]王登红,陈毓川.与海相火山作用有关的铁-铜-铅-锌矿床成矿系列类型及成因初探[J].矿床地质,2001,20(2):112-118
    [47]秦德先,洪托,田毓龙等.广西大厂锡矿92号矿体矿床地质与技术经济[M].地质出版社.2001
    [48]Japues L A, Wyborn L A I, Gallagbe R. The role of geographic information system, empirical modeling and expert systems in metallogenic research [A].12th Australian Geological Convention, Geological Society of Australia Abstract (No.37) [s.1.]:Perth, 1994,196-197
    [49]毛景文.桂北九万大山元宝山地区锡多金属矿床地质特征和成矿系列[J].矿床地质,1987(4)
    [50]方维萱,胡瑞忠,苏文超等.扬子地块南缘及邻区大陆动力成矿系统、成矿系列特征与找矿方向[J].矿物学报,2001,21(4):561-570
    [51]秦德先,谈树成,范柱国等.个旧-大厂地区地质构造演化及锡多金属成矿[J].矿物学报,2004, 24(2):117-122
    [52]陶维屏.中国非金属矿床的成矿系列[J].地质学报.1989,4:324-337
    [53]吴立新,史文中,Christopher Gold等.3DGIS与3DGMS中的空间构模技术[J].地理与地理信息科学,2003,(19)
    [54]吴立新,张瑞新.三维地学模拟与虚拟矿山系统[J].测绘学,2002,(31)
    [55]吴立新.论数字矿山及其基本特征与关键技术.http://www.dcoal.com.cn
    [56]罗周全,刘晓明,刘望平等.数字矿山的技术基础[J].中国钨业,2005,(20)
    [57]B. E. Hobbs and S. Henley. Computing For Exploration And Mining Industries To The Year 2000".25th APCOM,1995
    [58]Surpac Vision软件用户使用手册[M].4版.北京:Surpac SoftWare International国际软件公司.2000
    [59]张金山.计算机技术在采矿工业中应用现状与展望[J].中国矿业,2000.01
    [60]Wellian R. sharp. Design of an Underground Mine Layout.11th APCOM,1973
    [61]昆明理工大学矿产地质研究所.Micromine用户使用说明书1-5册,2002
    [62]Surpac用户手册,2000.7以及www.surpac.com.cn网站下载的培训资料,2005.03
    [63]翟裕生.金属成矿学的若干进展[J].地质与勘探,1997,33(1):13-18
    [64]王世称,陈永良,夏立显.综合信息矿产预测理论与方法[M].第一版.北京:科学出版社,2000.3
    [65]赵鹏大,池顺都,李志德等.矿产勘查理论与方法[M].第一版.北京:中国地质大学出版社,2001.7
    [66]陈永清,王世称.综合信息成矿系列预测的基本原理和方法[J].山东地质,1995,11(1):55-62
    [67]侯德义,刘鹏鄂,李守义等.矿产勘查学[M].第二版.北京:地质出版社,1997.11
    [68]王世称、陈永清.成矿系列预测的基本原则及特点[J].地质找矿论丛,1994,9(4):79-85
    [69]王世称,陈永清.金矿综合信息成矿系列预测理论体系[J].黄金地质,1995,1(1):1-7
    [70]Richard BM, Joseph MB, Rlchard SL, Roger WB. Characteristic Analysis-1981:Final program and a possible discobery. Math. Geol,1983,15(1):59-83
    [71]Jay Hodgson C. The case for upper crustal control on mineralization of some hydrothermal ore deposits:aspeculative genetic model. Queen's University
    [72]杨永华,赵善付.区域金矿成矿系列综合信息预测原理和方法[J].有色金属矿产与勘查,1995,4(6):361-364
    [73]Ohmoto II. Formation of volcanigentic massive sulfide deposits:The Kuroko perspective, Ore Geol-Rev,1996. No.10
    [74]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
    [75]C. M. Knox-Robinson, L. A. I. Wybom. Towards a holistic exploration strategy:Using geographic information systems as a tool to enhance exploration[J]. Australian journal of earth sciences,1997,44:453-463
    [76]马淑珍.综合信息矿产预测回顾与展望[J].世界地质,1995,14(4):75-78
    [77]Woodall R. Empiricism and concept in successful mineral exploration[J]. Australian Journal of Earth Sciences,1994,41(1):1-10
    [78]曹新志,孙华山,徐伯骏.关于成矿预测研究的若干进展[J].黄金,2003,24(4):11-14
    [79]Dilles J H, Solomon G C, Taylor H P, et al. Oxygen and hydrogen isotope characteristics of hydrothermal alteration at the Ann-Mason porphyry copper deposit, Yerington, Nevada[J]. Economic Geology,1992,87:44-63.
    [80]Hekinian R, Fevrive et al. Sulful deposits from the East Pacific Rise 21° N.Science,1980,207
    [81]CYAMEX Scientific Team:First manned submersible dives on the East Pacific Rise at 21 °N (Project RITA):General results. Marine Geologys Res,1981, (4)
    [82]肖克炎.应用综合信息法研究成矿规律及成矿预测的新进展[J].地球科学进展,1994,9(2):18-23
    [83]肖克炎.大比例尺综合信息成矿预测的研究问题及途径[J].黄金地质科技,1993,38(4):34-39
    [84]陈洪德,曾云孚,李考全.丹池晚古生代盆地的沉积和构造演化[J].沉积学报,1989,7(4):85-96
    [85]陈洪德,曾云孚.右江沉积盆地的性质及演化讨论[J].岩相古地理,1990,第一辑:28-37
    [86]杨建宇,秦德先,胡志军等.Surpac在大厂92号矿体经济评价中的应用[J].昆明理工大学学报:理工版-2007年2期
    [87]P. A. Rona. Hydrotermal mineralization at oceanic ridges, Journal of the mineralogical association of Canada,1988,266, part 3
    [88]秦德先,陈建文,田毓龙.广西大厂长坡锡矿床地质及成因[J].有色金属矿产与勘查,1998,7(3):146-151
    [89]韩发.孙海田.Sedex型矿床成矿系统[J].地学前缘,1999,6(1)
    [90]韩发等.大厂锡多金属矿床地质及成因[M].北京:地质出版社,1997:122-131.
    [91]中国有色金属工业总公司广西地质勘查局.广西锡矿[M].北京:地质出版社,1993.20-79
    [92]秦德先.广西大厂锡矿92号矿体地质特征及富集规律.研究报告,1994
    [93]黄有德,俞开基,高志斌.个旧—大厂及其外围地区锡矿成矿条件、找矿方法及找矿远景.研究报告,1985.1-95
    [94]翟裕生.同生断层对层控超大型矿床的控制[J].中国科学(D集),1998,28(3)
    [95]赵汝松.丹池地区构造系统及其对岩矿的控制[J].锡矿地质讨论会论文集.北京:地质出版社,1987.176-180
    [96]V. Marching, J. Erzinger, H. Rosch.. Sediments from a hydrothermal field in the central valley of the Galapagos Rift spreading center.Marine Geology,1987,86:243-251
    [97]Fouquet Y., Stackelberg U. V., et al., Metallogenesis in back-arc environments:the Lau basin example. Econ. geol.,1993,88:2154-2181
    [98]秦德先,陈健文.广西大厂长坡锡矿地质与成因[J].有色金属矿产与勘查,1998,7(3):P146-152.
    [99]广西地质勘查二一五队.大厂锡多金属矿田地质测量报告.1990
    [100]毛景文等.桂北地区火成岩系列和锡多金属矿床成矿系列[J].北京:北京科技出版社,1988
    [101]叶俊等.广西大厂锡矿田泥盆系蚀变海相火山岩[J].地质论评,1989,35(3)
    [102]苏亚汝,黎应书,秦德先等.广西大厂锡矿田100号矿体成矿模型的建立[J].有色金属:矿山部分-2007年2期
    [103]Yamamoto K. Geochemical characteristics and deposition environment of cherts and associated rocks in the Franciscan and Shimena terranes. Sediment Geology,1987,52:65-108
    [104]Adach5 M., Yamamoto R., Suigiski R.. Hydrothermal chert and associated siliceous rocks from the Northern Pacific:Their Geological significance as indication of ocean ridge activity. Sedimentary Geology,1986,47 (1-2):125-148
    [105]王思源,潘其云,赵兴元等.芒场层控型锡多金属矿[M].北京:中国地质大学出版社.1990:132-150
    [106]G.福尔.同位素地质学原理(中译本)[M].北京:科学出版社.1986:302-315
    [107]张科,曹新志,孙华山.粤西北庞西垌银矿床化探元素多元统计分析[J].黄金.2004,25(6): P16-19
    [108]程光耀等.试论锡的原始富集[J].地质与勘探,1984, (6):29-35
    [109]郭文魁.现代海洋地壳的成矿作用及其意义[J].地质论评,1987,33(4):372-377
    [110]罗德宣,张起钻,廖宗廷.大厂锡矿田海底热水沉积、后期岩浆热液叠加改造成矿的依据[J].矿产与地质,1993,7(5):313-319
    [111]侯增谦,艾永德,曲晓明等.岩浆流体对冲绳海槽海底成矿热水系统的可能贡献[J].地质学报,1999,73(1):57-65
    [112]韩发,沈建忠,R.W.哈钦森.冰长石——大厂锡-多金属矿床同生成因的标志矿物[J].矿床地质,1993,12(4):330-337
    [113]Qin Dexian, Chen Jianwen, Zhao Rusong. Geology and geochemistry of the super-large modified emanated-sedimenrary Dachang TinDeposit in Guanxi provice[A]. Papers to 30thIGC[C].1996:495-498
    [114]Bostrom K.. Genesis of ferromanganese deposits-diagnostic criteria for recent and old deposits. In:Rona P. A. et al. ed. Hydrothermal process at seafloor spreading centers. New York:Plrnum Press,1983:473-483
    [115]叶俊等.华南某些锡石硫化物矿床成矿机制的探讨[M].地质出版社.1987:66-74
    [116]冼柏琪.试论广西锡矿的成矿条件及分布规律[J].地质学报.1984(1):49-61
    [117]秦德先.近年在我国三个特大型锡矿床中相继发现的火山(成矿)作用及其科学意义[J].昆明理工大学学报.2008(1)
    [118]涂光炽.关于超大型矿床的寻找和理论研究[J].地球科学进展,1989, (6)
    [119]祁思敬,李英.热水沉积岩及其后生变化[J].1994
    [120]芮宗瑶.海底喷气沉积矿床研究的新进展[J].国外矿床地质,1989, (2)
    [121]侯增谦,浦边辙郎.古代与现代海底黑矿型块状硫化物矿床矿石地球化学比较研究[J].地球化学,1996,25(3):228-240
    [122]陈先沛等.热水沉积作用的概念和几个岩石学标志[J].沉积学报,1992,10(3):124-131
    [123]宋春晖,武安斌,周少平.西成矿田海底喷溢沉积成因硅质岩及其与矿化关系[J].沉积学报,1992,10(4):61-67
    [124]田毓龙,秦德先等.三家厂铜矿地质地球化学[J].矿物学报,2000(1)
    [125]杨志华.边缘转换盆地的构造岩相与成矿[M].北京:科学出版社,1991
    [126]R.W.哈钦森.层控矿床在地质历史中的地位.国外矿床地质,1988, (3):1-81
    [127]Large R. R.. Australia volcanic hosted massive sulphide deposits:features, style, and genetic models. Econ. Geol.,1992,87:471~510
    [128]容铃聪.三维地质模型软件[J].中国矿业,1999.03
    [129]南格利.矿体线框模型及其建立方法[J].有色矿山,2001.09,30(5)
    [130]朱良峰,吴信才,刘修国等.基于钻孔数据的三维地层模型的构建[J].地理与地理信息科学,2004,(5)
    [131]南格利.采矿CAD在冬瓜山铜矿设计中的应用研究[J].北京:中国矿业大学,2000
    [132]]丁悌平.大厂锡石—硫化物多金属矿带地质特征,成矿系列和找矿方向.地质矿产部矿床地质研究所.1985.
    [133]孙华山,赵朋大,张寿庭等.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(自然版).2005,32(1):P82-86
    [134]I. R. Plimer. Exhalative Sn and W deposits associated with mafic volcanism as precursors to Sn and W associated with granites. Mineralium Deposite,1980,15:275~289
    [135]倪春中,秦德先,范柱国等.广西大厂92号矿体节理裂隙与矿化及岩体稳定性关系[J].昆明 理工大学学报:理工版-2005年4期
    [136]杨学善,秦德先,邓家凤等.广西大厂锡多金属矿田找金条件分析[J].矿床地质-2005年2期
    [137]秦来勇,秦德先,余阳先等.广西大厂细脉带锡矿体富集规律及隐伏矿体预测[J].华南地质与矿产-2005年1期
    [138]余阳先,秦德先,秦来勇等.大厂长坡-铜坑锡多金属矿床地质特征及其层控性[J].矿产与地质-2004年5期
    [139]夏既胜,秦德先,谈树成等.广西大厂X矿体数字化研究及其意义[J].地质与勘探-2004年4期
    [140]Fleet A. J. Hydrothermal and hydrogeneous ferromanganes deposits. In:Rona P. A., et al. eds. Hydrothermal process at sea floor spreading centers. Amsterdam:Elsevier Science Publishers B V.,1983:537-570.
    [141]Huston D. L.,. Sie S. H., Surer C. F., et. al, Trace elements. in sulphide minerals from eastern Australia volcanic-hosted massive sulphide deposit. Econ. Geol.1995,90:1167-1196
    [142]矫东风,吕新彪.基于GIS空间分析的成矿预测[J].地质找矿论丛,2003,18(4):269-274
    [143]张建龙,游丽君,秦举礼等.利用GIS空间分析功能进行矿产资源评价的方法研究[J].物探化探计算技术,1997,19(3):283-286
    [144]肖克炎,朱裕生,张晓华等.矿产资源评价中的成矿信息提取与综合技术[J].矿床地质,1999,18(4):379-384
    [145]王全明,方一平.矿产资源评价中的GIS[J].中国地质,2001,28(4):3844
    [146]鲍光淑,刘斌.基于空间分析的矿产资源评价方法[J].中南工业大学学报,2001,32(1):1-4
    [147]杨学善,秦德先,陈耀光等.地理信息系统(GIS)支撑下的综合信息成矿预测[J].地质与勘探,2004,40(2):71-76
    [148]朱思才,吴加齐,刘和发.GIS技术在区域矿产资源勘查评价中的应用[J].有色金属矿产与勘查,1999,8(6):615-619
    [149]高志斌.广西丹池地区锡多金属成矿带控矿因素及成矿预测[J].地质与勘探,1988,24(8):18-24
    [150]赵鹏大,池顺都.初论地质异常[J].地球科学—中国地质大学学报,1991,(3):241-248
    [151]赵鹏大,陈永清.地质异常矿体定位的基本途径[J].地球科学—中国地质大学学报,1998,23(2):111-114
    [152]赵鹏大,陈永清,刘吉平等.地质异常成矿预测理论与实践[M].武汉:中国地质大学出版社,1999:1-138
    [153]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):1-12
    [154]赵鹏大,孟宪国.地质异常与矿产预测[J].地球科学—中国地质大学学报,1993,18(1):39-46
    [155]赵鹏大,王京贵,饶明辉.中国地质异常[J].地球科学—中国地质大学学报1995,20(2):117-127
    [156]陈永清,刘红光.初论地质异常数字找矿模型[J].地球科学—中国地质大学学报,2001,126(2):129-134
    [157]王世称,范继璋,杨永华.矿产资源评价[M].长春,吉林科技出版社,1990
    [158]张均,陈守余,张玉香.隐伏矿体定位预测中的几个关键问题[J].贵金属地质,1998,7(4):293-301
    [159]G. P. Watson, A. N. Rencz and G. F. Bonham-Carte, Geographic information system are being applied to mineral resource assessment in Northern New Brunswick[J] GEOS1989,18(1)
    [160]张均.矿体定位预测的研究现状与趋势[J].地球科学进展,1997,12(3):242-246
    [161]张均.隐伏矿体定位预测的方法学基础及方法论[J].贵金属地质,2000,9(2)::101-105
    [162]Cox D.P., Singer D.A.Mineral Deposit Models. U S Geological SurveyBulletin 1963, 1986,379,143-161
    [163]Cox D.P.The Development and Use of Mineral Deposit Models in the United States Geological Survey. Geological Association of Canada Special Pager,40,1993, (1995):15-19
    [164]Drew L. J. Revising U S Geological Survey Mineral Resource Assessment Method. http:/ /pubs.usgs.gov/info-handout/revision,1998
    [165]Hodgson C. J. Uses (and Abuses) of Ore Deposit Models in Mineral Exploration. Geosciences Canada,1990,17
    [166]Mc Cammon R. B.PROSPECTOR II-an expert system for mineral deposit models. Geological Association of Canada Special Pager,40,1993, (1995):679-684
    [167]Klaus J Schulz, Joseph A Briskey. A cooperative International Project to Assess the World Undiscovered Non-fuel Mineral Resources:Status and Schedule of Activities. Workshop on Assessment Undiscovered Mineral Resources, Beijing, China,2002,1-6
    [168]Singer D A.Basic concepts in three quantitative assessments of undiscovered mineral resources. Nonrenewable Resources,1993a,2(2):69-81
    [169]Simger D A. Development of grade and tonnage models for different deposit types. Geological Association of Canada Special Pager,40,1993b, (1995):21-30
    [170]Singer D A. Some Suggested Future Directions of Quantitative Resource Assessments. Journal of China University of Geosciences,2001,40-44
    [171]陈述彭,鲁学军,周成虎.地理信息系统导论[M].北京:科学出版社,1999
    [172]吴信才.地理信息系统的基本技术与发展动态[J].地球科学,1998,23(4):329-333
    [173]郭秋英.当前GIS发展的几个特点[J].测绘通报,1998(5):43-48
    [174]朱光,季晓燕,戌只.地理信息系统基本原理及应用[M].北京:测绘出版社,1997
    [175]陈军,杜道先.试论地理信息产业的发展方向与对策[J].测绘通报,1994(6):13-17
    [176]徐翠生.地理信息系统应用现状及相应技术发展趋势[J].中国地质,1998
    [177]Graem F, Bonham-Carter. Geographic Information System for Geo-Scientist Modeling with GIS.1994
    [178]方维萱,刘方杰,程顺有.初论信息技术有我国有色金属矿产勘查与开发[J].岩土工程界,1999,8(6):627-632
    [179]李裕伟.空间信息技术的发展及其在地球科学中的应用[J].地学前缘,1998,5(1-2):335-347
    [180]宋国耀,张晓华,肖克炎等.矿产资源潜力评价的理论和GIS技术[J].物化探计算技术,1999,21(3):199-205
    [181]周凯锋,秦德先,李云霞等.变异函数在广西大厂锡矿田X号矿体中的应用[J].金属矿山.2009年1期
    [182]杨晓坤,秦德先,冯美丽等.广西大厂矿田钻孔化探元素多元统计分析研究[J].金属矿山.2008年7期
    [183]刘晓玮,秦德先,黎应书等.数字矿床模型在广西大厂91号矿体中的应用[J].矿业研究与开发.2008年1期
    [184]伍伟,秦德先,周凯锋等.广西大厂细脉带矿体基于Surpac的数学经济模型研究[J].矿冶工程.2008年1期
    [185]杨晓坤,秦德先,冯美丽等.广西大厂矿田三维地球化学模型的研究及应用[J].金属矿山-2007年1期
    [186]杨晓坤,秦德先,冯美丽等.大厂100号矿体深部和外围三维地球化学模型及在找矿中的应用 [J].有色金属:矿山部分-2006年6期
    [187]伍伟,秦德先,黎应书等.广西大厂矿田细脉带锌矿体三维矿床数学模型[J].中国矿业-2006年9期
    [188]夏既胜,秦德先,曾红云等.MAPGIS在广西大厂锡矿成矿预测中的应用[J].矿产与地质-2006年1期
    [189]林小平,秦德先,黎应书等.广西大厂锡矿田92号矿体数学经济模型研究[J].昆明理工大学学报:理工版-2005年6期
    [190]黎应书,秦德先,党玉涛等.广西大厂锡矿田某矿体三维矿床数学模型[J].矿业研究与开发-2005年6期
    [191]杨晓坤,秦德先,冯美丽等.都龙锡锌矿区曼家寨矿段13号矿体化探元素统计[J].物探与化探-2009年3期
    [192]曾敏,秦德先,杨晓坤等.基于MapGIS的综合信息成矿预测[J].矿业工程-2008年5期
    [193]杨晓坤,秦德先,冯美丽等.基于Surpac的矿山三维地学模型及综合信息成矿预测研究[J].地质与资源-2008年1期
    [194]胡志军,秦德先,黎应书等.变异函数在大厂锡矿田92号矿体中的应用[J].有色金属:矿山部分-2007年6期
    [195]伍伟,秦德先,任卓隽等.基于Surpac的坑道与采空区模型建立及其应用[J].有色金属:矿山部分-2009年4期
    [196]杨晓坤,秦德先,冯美丽等.广西大厂矿田三维地学模型及综合信息找矿预测研究[J].地质找矿论丛.2009年1期
    [197]黄薰德,吴郁彦等.地球化学找矿[M].北京:地质出版社,1986,5.
    [198]蔡明海,梁婷等.广西大厂矿田花岗岩地球化学特征及其构造环境[J].地质科技情报,2004,23(2):57-62.
    [199]李业辉.大厂矿田105号矿体开发面临的问题及对策[J].采矿技术,2002,2(4):9-11.
    [200]郜兆典.大厂锡多金属矿床成矿模式及找矿远景[J].广西地质,2002,15(3):25-32.

© 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