宁镇中段矽卡岩型铁铜多金属矿床多元信息成矿预测研究
|
摘要
宁镇中段铜多金属矿床处于长江中下游成矿带的东端,通过野外地质调查、室内地质、遥感成果研究,结合区内已有的物化探成果,取得以下几点认识：
1、本文以接触交代型矿床的成因理论为研究基础,在研究了矿体的分布特征、矿石组构特点及矿物生成顺序,明确了区内铜多金属矿床的成因类型以接触交代型为主,兼具细脉浸染型和热液脉型；
2、结合成矿系统稀土元素、稳定同位素、成矿元素等地球化学特征,认为铜多金属矿床的成矿物质来源主要受区内燕山晚期中酸性杂岩体的控制,其次是栖霞组碳酸盐岩地层的影响,区内近东西向、近南北向构造对成矿流体的迁移、富集和定位成矿提供有利的空间；
3、区内铜多金属矽卡岩矿床的成矿过程划分为两个成矿期,即矽卡岩期和热液期,成矿条件归纳为岩浆、地层、构造和物理化学条件四方面。根据矿床成因类型、控矿因素、成矿条件和成矿过程,总结出成矿规律并依此建立了综合成矿模式。
4、以多元信息成矿预测理论为指导思想,利用逻辑信息法提取获得的各类异常信息重叠最多的地段,认为是地质结构复杂的地段,也是矿床赋存的有利部位。通过地-物-化-遥多元成矿预测信息的综合,按照地质成矿条件有利程度、物化探异常强度与规模、环形构造发育程度、遥感解译蚀变显现强度与规模,构建了多元信息找矿模型,并进行综合判定成矿有利位置,在伏牛山北侧、宝华山、铜山南侧和东毛山的四个接触带部位,圈定出五个重点找矿预测靶区。经钻孔验证,伏牛山北侧接触带存在矽卡岩型铜多金属矿化,具有进一步沿接触带的有利部位找矿的前景,为该区寻找矽卡岩型矿床拓展了找矿空间,是宁镇中段铜多金属矿床采用多元信息成矿预测的有效方法。
The middle segment of Nanjing-Zhengjiang copper polymetallic deposit is in the east part of Middle_Lower Yangtze metallogenic belt. Some conclusions have been acquired by researching on geological, remote sensing, geophysical and geochemical.
1. Based on genetic theory of contact metasomatic deposits, the results suggest that contact metasomatic type is the the main metallogenic type by study on distribution characteristics of ore body, texture and structure of ores, and mineral paragenesis sequence. Meanwhile, there are veinlet disseminated type and hydrothermal vein type.
2. Combined with the geochemical characteristics in REE, stable isotope and ore-forming elements of metallogenic system, it is considered that the sources of ore-forming materials mainly are from Yanshanian intermediate-acid magma. Qixia carbonate formation is the secondary metallogenic factor. Furthermore, the structures which are nearly EW and NS trending provide advantageous space for the migration, concentration and location of metallogenic fluid.
3. The ore-forming process divides into skarn-stage and hydrothermal-stage. The metallogenic condition includes magma, strata, structure and physical chemistry. According to genetic types, controlling factors, ore-forming conditions and ore-forming process of copper polymetallic deposit, the metallogenic regularity has been summarized, and the metallogenic model has been set up by it.
4. Based on the guiding ideology of multi-information metallogenic prediction theory, it is considered that the more overlapped anomaly information on using the logical-information method to extract, the more complex geological structures are there, and are beneficial for bearing orebody. Compared with the favorable degree of geological metallogenetic conditions, intensity and sale of geophysical-geochemical anomalies, development degree of circular structure, intensity and sale of RS-interpretation alteration, the favorable position of mineralization, the prospecting model of location prediction has been built. After comprehensively determining the favorable position for ore-forming and combining with the prospecting model, five prospecting targets in the contact zones has been delineated, which are in the north of Funiushan, Baohuashan, the south of Tongshan and Dongmaoshan. Drilling verifying showed that there is skarn-type copper polymetallic mineralization in the contact zones in the north of Funiushan. It is proved that multi-information metallogenic prediction is an available method for exploration in the middle segment of Nanjing-Zhengjiang.
1、本文以接触交代型矿床的成因理论为研究基础,在研究了矿体的分布特征、矿石组构特点及矿物生成顺序,明确了区内铜多金属矿床的成因类型以接触交代型为主,兼具细脉浸染型和热液脉型；
2、结合成矿系统稀土元素、稳定同位素、成矿元素等地球化学特征,认为铜多金属矿床的成矿物质来源主要受区内燕山晚期中酸性杂岩体的控制,其次是栖霞组碳酸盐岩地层的影响,区内近东西向、近南北向构造对成矿流体的迁移、富集和定位成矿提供有利的空间；
3、区内铜多金属矽卡岩矿床的成矿过程划分为两个成矿期,即矽卡岩期和热液期,成矿条件归纳为岩浆、地层、构造和物理化学条件四方面。根据矿床成因类型、控矿因素、成矿条件和成矿过程,总结出成矿规律并依此建立了综合成矿模式。
4、以多元信息成矿预测理论为指导思想,利用逻辑信息法提取获得的各类异常信息重叠最多的地段,认为是地质结构复杂的地段,也是矿床赋存的有利部位。通过地-物-化-遥多元成矿预测信息的综合,按照地质成矿条件有利程度、物化探异常强度与规模、环形构造发育程度、遥感解译蚀变显现强度与规模,构建了多元信息找矿模型,并进行综合判定成矿有利位置,在伏牛山北侧、宝华山、铜山南侧和东毛山的四个接触带部位,圈定出五个重点找矿预测靶区。经钻孔验证,伏牛山北侧接触带存在矽卡岩型铜多金属矿化,具有进一步沿接触带的有利部位找矿的前景,为该区寻找矽卡岩型矿床拓展了找矿空间,是宁镇中段铜多金属矿床采用多元信息成矿预测的有效方法。
The middle segment of Nanjing-Zhengjiang copper polymetallic deposit is in the east part of Middle_Lower Yangtze metallogenic belt. Some conclusions have been acquired by researching on geological, remote sensing, geophysical and geochemical.
1. Based on genetic theory of contact metasomatic deposits, the results suggest that contact metasomatic type is the the main metallogenic type by study on distribution characteristics of ore body, texture and structure of ores, and mineral paragenesis sequence. Meanwhile, there are veinlet disseminated type and hydrothermal vein type.
2. Combined with the geochemical characteristics in REE, stable isotope and ore-forming elements of metallogenic system, it is considered that the sources of ore-forming materials mainly are from Yanshanian intermediate-acid magma. Qixia carbonate formation is the secondary metallogenic factor. Furthermore, the structures which are nearly EW and NS trending provide advantageous space for the migration, concentration and location of metallogenic fluid.
3. The ore-forming process divides into skarn-stage and hydrothermal-stage. The metallogenic condition includes magma, strata, structure and physical chemistry. According to genetic types, controlling factors, ore-forming conditions and ore-forming process of copper polymetallic deposit, the metallogenic regularity has been summarized, and the metallogenic model has been set up by it.
4. Based on the guiding ideology of multi-information metallogenic prediction theory, it is considered that the more overlapped anomaly information on using the logical-information method to extract, the more complex geological structures are there, and are beneficial for bearing orebody. Compared with the favorable degree of geological metallogenetic conditions, intensity and sale of geophysical-geochemical anomalies, development degree of circular structure, intensity and sale of RS-interpretation alteration, the favorable position of mineralization, the prospecting model of location prediction has been built. After comprehensively determining the favorable position for ore-forming and combining with the prospecting model, five prospecting targets in the contact zones has been delineated, which are in the north of Funiushan, Baohuashan, the south of Tongshan and Dongmaoshan. Drilling verifying showed that there is skarn-type copper polymetallic mineralization in the contact zones in the north of Funiushan. It is proved that multi-information metallogenic prediction is an available method for exploration in the middle segment of Nanjing-Zhengjiang.
引文
[1]薛虎,张福定,胡成荫,等.宁镇山脉是“三背两向”吗?[J].地质论评,1985,31(2)：165-171
[2]薛虎,施华生,徐国泉.宁镇山脉的推覆构造与褶皱[J].中国地科院南京地质矿产研究所所刊,1985,6(3)：1-12
[3]葛肖虹.论宁镇山脉推覆构造的特征与形成[J].长春地质学院学报,1987,17(2)：143-153
[4]张永康,孙竞雄.江苏西南部中生代断块构造的基本特征[J].中国地科院南京地质矿产研究所所刊,1982,3(4)：23-40
[5]张永康,张健,等.宁镇山脉徐—金逆掩断层前缘同生滑塌角砾岩的初步认识[J].中国地科院南京地质矿产研究所所刊,1985,6(3)：42-50
[6]邢凤鸣.宁镇山脉中段侵入岩体的初步划分及其与成矿的关系[J].华东地质,1980,(3)：88-97
[7]毛建仁,苏郁香,陈三元,等.长江中下游中酸性侵入体与成矿[M].北京：地质出版社,1990
[8]金素琴,扬培峰.江苏省宁镇地区岩浆岩侵入深度、剥蚀程度与找矿关系的研究[J].江苏地质,1988,1：18-56
[9]许继峰,王强,徐义刚,等.宁镇地区中生代安基山中酸性侵入岩的地球化学：亏损重稀土和钇的岩浆产生的限制[J].岩石学报,2001,17(4)：576-584
[10]Jifeng Xu, Shinjo R, Defant M J, et al. Origin of Mesozonic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Geology,2002.30:1111-1114
[11]翟裕生,等.长江中下游地区铁铜(金)成矿规律[M].北京：地质出版社,1992
[12]钟昆明,薛顺荣,王世称.大型超大型金属矿床综合信息预测理论与实践[M].武汉：中国地质大学出版社,2009.15-16
[13]杨洪枝、王家仁,等.勐兴铅锌矿地质与综合信息成矿预测[M].昆明：云南科技出版社,2008.1-7
[14]程裕淇.中国地区地质概论[M].北京：地质出版社,1994.165-384
[15]闵庆魁.宁镇山脉发现前震旦系—埤城群[J].地层学杂志,1987,11(2)：130-134
[16]黄英,王远坤.宁镇地区地壳运动与地质发展史分析[J].胜利油田职工大学学报,2001,15,(2)：15-16
[17]Yuanming Pan, Ping Dong. The Lower Changjiang (Yangzi/Yangtze River) metallogenic belt, east central China: intrusion- and wall rock-hosted Cu-Fe-Au, Mo, Zn, Pb, Ag deposits. Ore Geology Reviews,1999,15:177-242
[18]陈上达.论安基山铜矿热液蚀变的地球化学过程[J].江苏地质,1987,3：17-120
[19]张术根,王大伟.长江中下游地区铜金矿床矿石稀土元素地球化学特征研究[J].湖南地质,1992,S1：61-169
[20]Xuexiang Gu, Oskar Schulz, Franz Vavtar, et al. Rare earth element geochemistry of the Woxi W-Sb-Au deposit, Hunan Province, South China. Ore Geology Reviews,2007,31:319-336
[21]Hanson G N. Rare earth elements in petrogenetic studies of igneous systems. Ann. Rev. Earth & Planet Sci.,1980,8:371-1406.
[22]赵振华.某些常用稀土元素地球化学参数的计算方法及其地球化学意义[J].地质地球化学,1985,S1(3)：11-14
[23]袁峰,周涛发,刘晓东,等.安徽安庆铜矿床稀土元素地球化学研究[J].中国稀土学报,2002,20(6)：199-202
[24]Taofa Zhou, Feng Yuan, Shucang Yue, et al. Geochemistry and evolution of ore-forming fluids of the Yueshan Cu-Au skarn- and vein-type deposits, Anhui Province, South China. Ore Geology Reviews.2007,31:279-303
[25]邱瑞龙.贵池铜山铜矿矽卡岩稀土元素地球化学特征[J].地质学报,1987,6(1)：91-100
[26]徐晓春,赵丽丽,谢巧勤,等,铜陵狮子山矿田金矿床和铜矿床矿石稀土元素地球化学[J],高校地质学报,2009,15(1)：35-47
[27]田世洪,丁悌平,侯增谦,等.安徽铜陵小铜官山铜矿床稀土元素和稳定同位素地球化学研究[J].中国地质,2005,32(4)：604-611
[28]Runxing Jia, Weixuan Fang, Ruizhong Hu. Geochemical characteristics and significance of major elements, trace elements and REE of NM copper polymetal deposit in Laos. Journal of rare earths,2010,28(2):305-311
[29]赵振华,钱汉东,黄晟.多元统计分析在金川铜镍矿床两类矿石中的应用[J].高校地质学报,2007,13(1)：127-136
[30]胡以铿.地球化学中的多元分析[M].武汉：中国地质大学出版社,1991：19-20
[31]王中刚,等.稀土元素地球化学[M].北京：科学出版社,1989
[32]邢凤鸣.宁镇山脉中段侵入岩体的初步划分及其与成矿关系.华东地质, 1980,(3)：88-108
[33]王立本,季克剑,陈东.安基山和铜山铜(钼)矿床中辉钼矿的铼—锇同位素年龄及其意义[J].岩石矿物学杂志,1997,16(2)：154-159
[34]叶水泉.江苏宁镇伏牛山岩体的铷锶等时线年龄[J].江苏地质,1999,23(3)：148-150
[35]陈福鑫,唐建华.宁镇地区内生矿产找矿标志及找矿方向[J].江苏地质,1993,17(3-4)：148-153.
[36]Habib Mollai, Rajesh Sharma, Georgia Pe-Piper. Copper mineralization around the Ahar batholith, north of Ahar (NW Iran):Evidence for fluid evolution and the origin of the skarn ore deposit. Ore Geology Reviews.2009,35:401-414
[37]Galal H. El Habaak. Pan-African skarn deposits related to banded iron formation, Um Nar area, central Eastern Desert, Egypt. Journal of African Earth Sciences, 2004,38:199-221
[38]袁见齐,朱上庆,翟裕生,等.矿床学[M].北京：地质出版社,1985.104-130
[39]华东有色地质研究所,宁镇地区区域地球化学资料,1988
[40]张建.安基山铜矿床沉积地球化学特征及其与成矿的关系[J].江苏地质,1987,1：8-14
[41]赵一鸣,吴良士,等.中国主要金属矿床成矿规律[M].北京：地质出版社,2004.63-99
[42]常印佛、刘湘培、吴言昌.长江中下游铜铁成矿带[M].北京：地质出版社.1991,138-197.
[43]翟裕生,等.长江中下游地区铁铜(金)成矿规律[J],北京：地质出版社,1992
[44]毛建仁,苏郁香,陈三元,等.长江中下游中酸性侵入岩与成矿[M],北京：地质出版社,1990
[45]翟裕生,等.长江中下游地区铁铜矿床类型、形成条件和成矿演化[J],地球科学,1983,(4)：95-105
[46]王道华,等.长江中下游地区铜、金、铁、硫矿床基本特征及成矿规律[M],北京：地质出版社,1989
[47]裴荣富,中国矿床模式[M],北京：地质出版社,1995.265-267,271-273
[48]刘湘培.长江中下游地区矿床系列和成矿模式[J],地质论评,1989,35(5)：398-408
[49]程裕淇,陈毓川.再论矿床成矿系列问题[J].中国地质科学院院刊,1993
[50]陈毓川,朱裕生.中国矿床成矿模式[M].北京：地质出版社,1993
[51]陈国达,黄瑞华.成矿构造学[J].地球科学进展,1991,6(1)：60-62
[52]丁存根,张术根,马春,等.宁镇中段矽卡岩型矿床的闪锌矿及其地质压力计应用讨论[J].地质学刊,2009,33(2)：124-129
[53]刘燕君.遥感找矿的原理和方法[M].北京：冶金工业出版社,1991
[54]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
[55]赵鹏大,池顺都,李志德,等.矿产勘查理论与方法[M].北京：中国地质大学出版社,2001
[56]朱裕生,肖克炎,等.成矿预测方法[M].北京：地质出版社,1997
[57]赵鹏大,胡旺亮,李紫金.矿床统计预测[M].北京：地质出版社,1994
[58]王世称,王於天.综合信息解译原理与矿产预测图编制方法[M].长春：吉林大学出版社,1989
[59]吴堑虹.利用GIS编制矿产预测图[J].地质与勘探,2000,36(3)：48-66
[60]黄旭钊.利用MAPINFO综合分析多源地学信息进行矿产预测[J].地球科学,2001,26(2)：189-191
[61]曹新志,王燕.成矿预测方法的理论基础及分类[J].地质科技情报,1993,12(1)：69-72
[62]卢作祥,范永香,刘辅臣.成矿规律和成矿预测学[M].武汉：中国地质大学出版社,1988
[63]李继宏.应用边缘成矿理论综合多源地学信息进行成矿预测[J].地质找矿论丛,2006,21：107-112
[64]Liangming Liu, Shenlin Peng. Prediction of hidden ore bodies by synthesis of geological, geophysical and geochemical information based on dynamic model in Fenghuangshan ore field, Tongling district, China. Journal of Geochemical Exploration,2003,81:81-98
[65]Mansour Ziaii, Ali A. Pouyan, Mahdi Ziaei. Neuro-fuzzy modelling in mining geochemistry: Identification of geochemical anomalies. Journal of Geochemical Exploration,2009,100:25-36
[66]Gongwen Wang, Jianping Chen. Mineral resource prediction and assessment of copper multi-mineral deposit based on GIS technology in the north of Sanjiang Region, China. Earth Science Frontiers,2008,15(4):27-32.
[67]Qingmou Li, Qiuming Cheng. VisualAnomaly: A GIS-based multifractal method for geochemical and geophysical anomaly separation in Walsh domain. Computers & Geosciences,2006,32:663-672
[68]叶水盛.综合信息矿产预测系统在内蒙古大兴安岭东南部多金属矿床密集区预测应用研究：[博士学位论文].长春：吉林大学,2007
[69]于文修.安徽月山岩体成因及其与成矿关系探讨：[硕士学位论文].贵阳：中国科学院地球化学研究所,2006
[70]廖莉萍.贵州西部地区铅锌矿成矿地质条件及综合信息成矿预测研究：[博士学位论文].长春：吉林大学,2006
[71]李津.区域地球化学在长江中下游铜矿产资源预测中的应用研究：[硕士学位论文].北京：中国地质大学,2005
[72]唐永成,何义权,王永敏,等.GIS应用于安徽东部地区金矿资源评价研究[M].北京：地质出版社,2000
[73]池顺都,吴新林.云南元江地区铜矿GIS预测找矿有利度和空间相关性分析[J].地球科学,1998,23(1)：75-78
[74]肖克炎.试论综合找矿模型[J].地质与勘探,1994,30(1)：41-45
[75]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)：99-104
[76]赵鹏大,池顺都,陈永清.查明地质异常：成矿预测的基础[J].高校地质学报,1996,2(4)：361-372
[77]Shouting Zhang, Pengda Zhao, Qinglin Xia, et al. Discussion on the theories and practice of regional multi-objective mineral prediction and assessment - a case study of mineral deposits related to Himalayan alkali-rich porphyry in northwestern Yunnan Province, China. Earth Science Frontiers,2007,14(5): 104-115.
[2]薛虎,施华生,徐国泉.宁镇山脉的推覆构造与褶皱[J].中国地科院南京地质矿产研究所所刊,1985,6(3)：1-12
[3]葛肖虹.论宁镇山脉推覆构造的特征与形成[J].长春地质学院学报,1987,17(2)：143-153
[4]张永康,孙竞雄.江苏西南部中生代断块构造的基本特征[J].中国地科院南京地质矿产研究所所刊,1982,3(4)：23-40
[5]张永康,张健,等.宁镇山脉徐—金逆掩断层前缘同生滑塌角砾岩的初步认识[J].中国地科院南京地质矿产研究所所刊,1985,6(3)：42-50
[6]邢凤鸣.宁镇山脉中段侵入岩体的初步划分及其与成矿的关系[J].华东地质,1980,(3)：88-97
[7]毛建仁,苏郁香,陈三元,等.长江中下游中酸性侵入体与成矿[M].北京：地质出版社,1990
[8]金素琴,扬培峰.江苏省宁镇地区岩浆岩侵入深度、剥蚀程度与找矿关系的研究[J].江苏地质,1988,1：18-56
[9]许继峰,王强,徐义刚,等.宁镇地区中生代安基山中酸性侵入岩的地球化学：亏损重稀土和钇的岩浆产生的限制[J].岩石学报,2001,17(4)：576-584
[10]Jifeng Xu, Shinjo R, Defant M J, et al. Origin of Mesozonic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Geology,2002.30:1111-1114
[11]翟裕生,等.长江中下游地区铁铜(金)成矿规律[M].北京：地质出版社,1992
[12]钟昆明,薛顺荣,王世称.大型超大型金属矿床综合信息预测理论与实践[M].武汉：中国地质大学出版社,2009.15-16
[13]杨洪枝、王家仁,等.勐兴铅锌矿地质与综合信息成矿预测[M].昆明：云南科技出版社,2008.1-7
[14]程裕淇.中国地区地质概论[M].北京：地质出版社,1994.165-384
[15]闵庆魁.宁镇山脉发现前震旦系—埤城群[J].地层学杂志,1987,11(2)：130-134
[16]黄英,王远坤.宁镇地区地壳运动与地质发展史分析[J].胜利油田职工大学学报,2001,15,(2)：15-16
[17]Yuanming Pan, Ping Dong. The Lower Changjiang (Yangzi/Yangtze River) metallogenic belt, east central China: intrusion- and wall rock-hosted Cu-Fe-Au, Mo, Zn, Pb, Ag deposits. Ore Geology Reviews,1999,15:177-242
[18]陈上达.论安基山铜矿热液蚀变的地球化学过程[J].江苏地质,1987,3：17-120
[19]张术根,王大伟.长江中下游地区铜金矿床矿石稀土元素地球化学特征研究[J].湖南地质,1992,S1：61-169
[20]Xuexiang Gu, Oskar Schulz, Franz Vavtar, et al. Rare earth element geochemistry of the Woxi W-Sb-Au deposit, Hunan Province, South China. Ore Geology Reviews,2007,31:319-336
[21]Hanson G N. Rare earth elements in petrogenetic studies of igneous systems. Ann. Rev. Earth & Planet Sci.,1980,8:371-1406.
[22]赵振华.某些常用稀土元素地球化学参数的计算方法及其地球化学意义[J].地质地球化学,1985,S1(3)：11-14
[23]袁峰,周涛发,刘晓东,等.安徽安庆铜矿床稀土元素地球化学研究[J].中国稀土学报,2002,20(6)：199-202
[24]Taofa Zhou, Feng Yuan, Shucang Yue, et al. Geochemistry and evolution of ore-forming fluids of the Yueshan Cu-Au skarn- and vein-type deposits, Anhui Province, South China. Ore Geology Reviews.2007,31:279-303
[25]邱瑞龙.贵池铜山铜矿矽卡岩稀土元素地球化学特征[J].地质学报,1987,6(1)：91-100
[26]徐晓春,赵丽丽,谢巧勤,等,铜陵狮子山矿田金矿床和铜矿床矿石稀土元素地球化学[J],高校地质学报,2009,15(1)：35-47
[27]田世洪,丁悌平,侯增谦,等.安徽铜陵小铜官山铜矿床稀土元素和稳定同位素地球化学研究[J].中国地质,2005,32(4)：604-611
[28]Runxing Jia, Weixuan Fang, Ruizhong Hu. Geochemical characteristics and significance of major elements, trace elements and REE of NM copper polymetal deposit in Laos. Journal of rare earths,2010,28(2):305-311
[29]赵振华,钱汉东,黄晟.多元统计分析在金川铜镍矿床两类矿石中的应用[J].高校地质学报,2007,13(1)：127-136
[30]胡以铿.地球化学中的多元分析[M].武汉：中国地质大学出版社,1991：19-20
[31]王中刚,等.稀土元素地球化学[M].北京：科学出版社,1989
[32]邢凤鸣.宁镇山脉中段侵入岩体的初步划分及其与成矿关系.华东地质, 1980,(3)：88-108
[33]王立本,季克剑,陈东.安基山和铜山铜(钼)矿床中辉钼矿的铼—锇同位素年龄及其意义[J].岩石矿物学杂志,1997,16(2)：154-159
[34]叶水泉.江苏宁镇伏牛山岩体的铷锶等时线年龄[J].江苏地质,1999,23(3)：148-150
[35]陈福鑫,唐建华.宁镇地区内生矿产找矿标志及找矿方向[J].江苏地质,1993,17(3-4)：148-153.
[36]Habib Mollai, Rajesh Sharma, Georgia Pe-Piper. Copper mineralization around the Ahar batholith, north of Ahar (NW Iran):Evidence for fluid evolution and the origin of the skarn ore deposit. Ore Geology Reviews.2009,35:401-414
[37]Galal H. El Habaak. Pan-African skarn deposits related to banded iron formation, Um Nar area, central Eastern Desert, Egypt. Journal of African Earth Sciences, 2004,38:199-221
[38]袁见齐,朱上庆,翟裕生,等.矿床学[M].北京：地质出版社,1985.104-130
[39]华东有色地质研究所,宁镇地区区域地球化学资料,1988
[40]张建.安基山铜矿床沉积地球化学特征及其与成矿的关系[J].江苏地质,1987,1：8-14
[41]赵一鸣,吴良士,等.中国主要金属矿床成矿规律[M].北京：地质出版社,2004.63-99
[42]常印佛、刘湘培、吴言昌.长江中下游铜铁成矿带[M].北京：地质出版社.1991,138-197.
[43]翟裕生,等.长江中下游地区铁铜(金)成矿规律[J],北京：地质出版社,1992
[44]毛建仁,苏郁香,陈三元,等.长江中下游中酸性侵入岩与成矿[M],北京：地质出版社,1990
[45]翟裕生,等.长江中下游地区铁铜矿床类型、形成条件和成矿演化[J],地球科学,1983,(4)：95-105
[46]王道华,等.长江中下游地区铜、金、铁、硫矿床基本特征及成矿规律[M],北京：地质出版社,1989
[47]裴荣富,中国矿床模式[M],北京：地质出版社,1995.265-267,271-273
[48]刘湘培.长江中下游地区矿床系列和成矿模式[J],地质论评,1989,35(5)：398-408
[49]程裕淇,陈毓川.再论矿床成矿系列问题[J].中国地质科学院院刊,1993
[50]陈毓川,朱裕生.中国矿床成矿模式[M].北京：地质出版社,1993
[51]陈国达,黄瑞华.成矿构造学[J].地球科学进展,1991,6(1)：60-62
[52]丁存根,张术根,马春,等.宁镇中段矽卡岩型矿床的闪锌矿及其地质压力计应用讨论[J].地质学刊,2009,33(2)：124-129
[53]刘燕君.遥感找矿的原理和方法[M].北京：冶金工业出版社,1991
[54]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
[55]赵鹏大,池顺都,李志德,等.矿产勘查理论与方法[M].北京：中国地质大学出版社,2001
[56]朱裕生,肖克炎,等.成矿预测方法[M].北京：地质出版社,1997
[57]赵鹏大,胡旺亮,李紫金.矿床统计预测[M].北京：地质出版社,1994
[58]王世称,王於天.综合信息解译原理与矿产预测图编制方法[M].长春：吉林大学出版社,1989
[59]吴堑虹.利用GIS编制矿产预测图[J].地质与勘探,2000,36(3)：48-66
[60]黄旭钊.利用MAPINFO综合分析多源地学信息进行矿产预测[J].地球科学,2001,26(2)：189-191
[61]曹新志,王燕.成矿预测方法的理论基础及分类[J].地质科技情报,1993,12(1)：69-72
[62]卢作祥,范永香,刘辅臣.成矿规律和成矿预测学[M].武汉：中国地质大学出版社,1988
[63]李继宏.应用边缘成矿理论综合多源地学信息进行成矿预测[J].地质找矿论丛,2006,21：107-112
[64]Liangming Liu, Shenlin Peng. Prediction of hidden ore bodies by synthesis of geological, geophysical and geochemical information based on dynamic model in Fenghuangshan ore field, Tongling district, China. Journal of Geochemical Exploration,2003,81:81-98
[65]Mansour Ziaii, Ali A. Pouyan, Mahdi Ziaei. Neuro-fuzzy modelling in mining geochemistry: Identification of geochemical anomalies. Journal of Geochemical Exploration,2009,100:25-36
[66]Gongwen Wang, Jianping Chen. Mineral resource prediction and assessment of copper multi-mineral deposit based on GIS technology in the north of Sanjiang Region, China. Earth Science Frontiers,2008,15(4):27-32.
[67]Qingmou Li, Qiuming Cheng. VisualAnomaly: A GIS-based multifractal method for geochemical and geophysical anomaly separation in Walsh domain. Computers & Geosciences,2006,32:663-672
[68]叶水盛.综合信息矿产预测系统在内蒙古大兴安岭东南部多金属矿床密集区预测应用研究：[博士学位论文].长春：吉林大学,2007
[69]于文修.安徽月山岩体成因及其与成矿关系探讨：[硕士学位论文].贵阳：中国科学院地球化学研究所,2006
[70]廖莉萍.贵州西部地区铅锌矿成矿地质条件及综合信息成矿预测研究：[博士学位论文].长春：吉林大学,2006
[71]李津.区域地球化学在长江中下游铜矿产资源预测中的应用研究：[硕士学位论文].北京：中国地质大学,2005
[72]唐永成,何义权,王永敏,等.GIS应用于安徽东部地区金矿资源评价研究[M].北京：地质出版社,2000
[73]池顺都,吴新林.云南元江地区铜矿GIS预测找矿有利度和空间相关性分析[J].地球科学,1998,23(1)：75-78
[74]肖克炎.试论综合找矿模型[J].地质与勘探,1994,30(1)：41-45
[75]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)：99-104
[76]赵鹏大,池顺都,陈永清.查明地质异常：成矿预测的基础[J].高校地质学报,1996,2(4)：361-372
[77]Shouting Zhang, Pengda Zhao, Qinglin Xia, et al. Discussion on the theories and practice of regional multi-objective mineral prediction and assessment - a case study of mineral deposits related to Himalayan alkali-rich porphyry in northwestern Yunnan Province, China. Earth Science Frontiers,2007,14(5): 104-115.
© 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 |