广东省金地球化学块体特征及资源量预测
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摘要
地球化学块体是地球上某种元素高含量的巨大岩块。由于其所具有的巨大的成矿元素供应量,为大型或巨型矿床或矿集区的形成提供必要的物质基础。本文系统介绍了地球化学块体理论及其应用于资源潜力预测的方法技术。在总结广东省区域地质特征及金矿成矿条件的基础上,利用广东省1:20万区域化探所取得的Au分析资料,根据地球化学块体的原理及方法,圈定了广东省Au地球化学块体共9个,并详细描述了Au地球化学块体的空间分布及谱系特征,以及块体内地层、岩性及构造特征,初步分析了块体演化过程及与已知矿床的空间分布关系。
研究表明,广东省内中型以上的金矿床全部产于块体内,地球化学块体中丰富的成矿元素供应量为矿床的形成,特别大中型矿床或矿集区的形成提供了物质基础。块体的规模反映了块体所在区域的成矿能力,块体规模越大,其形成的大型矿床的可能性就越大。块体中的矿床具体产出位置因不同的成因类型而有所不同:由于构造运动所形成的蚀变破碎带型矿床,其产出部位一般与块体中元素浓集中心吻合好;产于碳酸盐岩或碎屑岩中的微细粒浸染型金矿,其所在块体中元素含量层次较少且没有明显的浓集趋势,矿床在块体中的位置需要综合研究该类型矿床的成矿富集条件确定。
最后利用块体内的金属供应量与已知矿床的资源量关系,对块体的成矿率进行计算,块体或异常的成矿率为0.05%~1.07%,根据成矿率分别对全省块体按2.0ng/g、4.0 ng/g两个含量级次的潜在资源量进行了计算,其结果分别为813吨和550.97吨。
Geochemical block is defined a giant rock block with high content of one or more elements within the upper earth’s crust. It can provide large metal endowments necessary for the formation of large to giant ore deposits or ore camp. Based on the geochemical block concept and developed methodology,nine gold geological blocks are delineated by calculating the data obtained in regional geochemical mapping in Guangdong and getting 2.0 ng/g as the threshold of the blocks . In this thesis the author summarizes the regional geology and gold mineralization characteristics, describes the spatial distribution of Au geochemical blocks in Guangdong and the characteristics of hierarchically nested geochemical patterns, and analyses the spatial relationship of these blocks with known Au deposits.
The study indicates that all the large gold deposits in Guangdong are located within Au geochemical blocks. It demonstrates clearly that large gold endowment is the prerequisite to the occurrence of large gold deposits, and the large blocks indicate the high occurring possibility of large gold deposits . The studies of internal structure of the blocks also reveal that different kind of gold deposits has different spatial relationship. The faults control type gold deposits usually locate on high concentration anomalies and the type of spatial relationship is concentric. The sediment hosted microdisseminated type gold deposit locate on low concentration anomalies, the spatial relationship is uncertain.
The mineralization coefficients (Mc) is determined in some blocks on which many explorations has be carried out, the number scale from 0.05%~1.07%. By using Mc the potential Au resources in Guangdong is estimated, the total potential assessed resource of Au in Guangdong is about 813 tons and 550.97 tons.
研究表明,广东省内中型以上的金矿床全部产于块体内,地球化学块体中丰富的成矿元素供应量为矿床的形成,特别大中型矿床或矿集区的形成提供了物质基础。块体的规模反映了块体所在区域的成矿能力,块体规模越大,其形成的大型矿床的可能性就越大。块体中的矿床具体产出位置因不同的成因类型而有所不同:由于构造运动所形成的蚀变破碎带型矿床,其产出部位一般与块体中元素浓集中心吻合好;产于碳酸盐岩或碎屑岩中的微细粒浸染型金矿,其所在块体中元素含量层次较少且没有明显的浓集趋势,矿床在块体中的位置需要综合研究该类型矿床的成矿富集条件确定。
最后利用块体内的金属供应量与已知矿床的资源量关系,对块体的成矿率进行计算,块体或异常的成矿率为0.05%~1.07%,根据成矿率分别对全省块体按2.0ng/g、4.0 ng/g两个含量级次的潜在资源量进行了计算,其结果分别为813吨和550.97吨。
Geochemical block is defined a giant rock block with high content of one or more elements within the upper earth’s crust. It can provide large metal endowments necessary for the formation of large to giant ore deposits or ore camp. Based on the geochemical block concept and developed methodology,nine gold geological blocks are delineated by calculating the data obtained in regional geochemical mapping in Guangdong and getting 2.0 ng/g as the threshold of the blocks . In this thesis the author summarizes the regional geology and gold mineralization characteristics, describes the spatial distribution of Au geochemical blocks in Guangdong and the characteristics of hierarchically nested geochemical patterns, and analyses the spatial relationship of these blocks with known Au deposits.
The study indicates that all the large gold deposits in Guangdong are located within Au geochemical blocks. It demonstrates clearly that large gold endowment is the prerequisite to the occurrence of large gold deposits, and the large blocks indicate the high occurring possibility of large gold deposits . The studies of internal structure of the blocks also reveal that different kind of gold deposits has different spatial relationship. The faults control type gold deposits usually locate on high concentration anomalies and the type of spatial relationship is concentric. The sediment hosted microdisseminated type gold deposit locate on low concentration anomalies, the spatial relationship is uncertain.
The mineralization coefficients (Mc) is determined in some blocks on which many explorations has be carried out, the number scale from 0.05%~1.07%. By using Mc the potential Au resources in Guangdong is estimated, the total potential assessed resource of Au in Guangdong is about 813 tons and 550.97 tons.
引文
[1]王淑玲.2001年世界黄金供需形势.黄金地质, 2003,9(2)
[2]李树枝,闫卫东,奚生生.2000—2001年世界矿产资源勘查开发和矿产品供需形势[A] .国土资源部信息中心.世界矿产资源年评[C] .北京:地质出版社, 2002:12-19.
[3]涂光炽.关于超大型矿床的寻找和理论研究.地球科学进展,1989,6
[4]涂光炽.关于寻找超大型金矿的问题.四川地质学报,1992,12
[5]裴荣富,熊群尧.中国特大型金属矿床成矿偏在性与成矿构造聚敛(场) .矿床地质,1999, 8(1)
[6]裴荣富等.难识别及隐伏大矿、富矿资源潜力的地质评价.北京:地质出版社,2001:97-117.
[7]王世称,陈永良.中国大型金矿床空间分布规律及找矿方向.地球科学,1999,24(5)
[8]朱炳泉.壳幔化学不均一性与块体地球化学边界研究.地学前缘,1998,5(1~2).
[9]朱炳泉,常向阳.地球化学省与地球化学边界.地球科学进展. 2001,16(2).
[11]谢学锦、刘大文、向运川等.地球化学块体—概念和方法学的发展.中国地质, 2002, 29(3).
[12]谢学锦.用新观念与新技术寻找巨型矿床.科学中国人,.[J] .1995,(5):14-16.
[13]谢学锦,向运川.巨型矿床的地球化学预测方法.走向21世纪矿勘查地球化.北京:地质出版社,1999. 63
[14]刘大文.地球化学块体的概念及其研究意义.地球化学,2002,31(6).
[15]翟裕生.中国区域成矿特征及若干值得重视的成矿环境.中国地质,2003, 30(4)
[16] Xie Xue jing. Empirical prospecting, scientific exploration and information exploration [J]. J.Geochem. Explor., 1999,76:97-108.
[17]谢学锦.勘查地球化学:发展史·现状·展望.地质与勘探, 2002,38(6)
[18]吴传璧,施俊法.矿产勘查与信息找矿[A] .走向21世纪矿产勘查地球化学[C] .北京:地质出版社,1999:48-60.
[19]奚小环,张连.地质矿产部“八五”期间物探、化探、遥感勘查若干新进展[J ] .物探与化探, 1997 , 21(1) :1-5.
[20]王学求.矿产勘查地球化学过去的成就与未来的挑战.地学前缘,2003, 10(1)
[21]谢学锦.全球地球化学填图.中国地质,2003,30(1)
[22]谢学锦.2020年的勘查地球化学—从勘查地球化学到应用地球化学.地质通报,2003,22(11-12)
[23] Potter J. F. Editorial .[J]. Environmentalist, 1990(3-4).
[24] Xie Xuejing, Mu Xuzhang, Ren Tianxiang. Geochemical mapping on Chinal. J. Geochem. Explor. , 1997, 60: 99～113.
[25]谢学锦.中国化探发展的新战略[J] .物探与化探,1992,16(2).
[26] Xie Xuejing, Yin Bingchuan. Geochemical patterns from local to global. J. Geochem. Explor. , 1993, 47: 109～129.
[27]Hawkes H.E. and Webb J. S. Geochemistry in mineral exploration [M]. New York: Harper and Row,1962:1~415.
[28] Closs L. G. .Exploration geochemistry:expanding contributions to mineral resource development.[A] In: Gubins A. G. proceedings 97C,1998:3~8.
[29]王学求.巨型矿床与大型矿集区勘查地球化学.走向21世纪矿勘查地球化.北京:地质出版社,1999:37.
[30] Wang Xueqiu . Leaching of mobile forms of metals for giant ore deposits .J.Geochem. Explor. 199 8, 61:39~55
[31] Seager R.,Meyer M. Gold distribution in supercrustal rocks from Archean greenstone bell of South Africa and complexes of European Alps: metallogenicimplication. Econ. Geo. ,1982,77(1).
[32]谢学锦.战术性与战略性的深穿透地球化学.走向21世纪矿勘查地球化.北京:地质出版社,1999:92~102
[33]翟裕生.区域成矿学.北京:地质出版社,1999.
[34] Sillitoe R. H. Giant and bonanza gold deposits in epithemal environment: Assessment of potential genetic factors. In: Whiteing B.H.,Hodgson C J, Mason R. ed, Giant ore Deposits, 1993.
[35]黄汉鼎,张振瑷,李炳荣等.广东省金矿矿产资源总量预测报告(内部资料) .1987:15.
[36] Zhou, Y. Z. .Geology and Geochemistry of the Hetai Gold Field, Southern China, Guangzhou: South China University of Technology Press, 1993:310
[37]张国恒,董玉成,谭能超等.广东省高明市富湾银矿区普查报告. 1995
[38]南颐,周国强主编.广东省岩石地层.武汉:中国地质大学出版社,1996,19~25
[40] ]周国强,郑有铭,吴安生.两广云开地区的前震旦纪地层.中国区域地质,1996,No.4.
[41]孙培基、韦永福主编.当代中国金矿地质.北京:地震出版社,1996:8-12.
[42]覃慕陶,凌井生,王正云.粤西地区金矿成矿条件及远景预测研究.当代中国金矿地质.北京:地震出版社,1996: 160-167.
[43]凌井生、陈础廷、季明均.广东省高要县河台韧性剪切带蚀变糜棱岩型金矿床地质研究. 1990:5-10孙培基、韦永福主编.当代中国金矿地质.北京:地震出版社,1996: 8-12.
[44]彭少梅.粤北新洲逆冲推覆构造及金矿成矿系列.武汉:中国地质大学出版社,1992:
[45]周永章.华南河台金矿田的地质地球化学研究(摘要).地质地球化学, 1993, No.5.
[46]栾世伟等编著.金矿床地南及找矿方法.成都:四川科学技术出版社,1987:208-211.
[47]张敬陆.从闪长岩与金矿的关系谈金矿的岩浆成矿机理.黄金地质科技,1989,No.2
[48]涂光炽.几个金矿地质传统认识的质疑―涂光炽教授在“中国花岗岩-绿岩地体的金矿”项目第二次工作会议上的报告.国外前寒武纪地质. 1994,No.1
[49]申玉科,邓军,徐叶兵.煌斑岩在玲珑金矿田形成过程中的地质意义.地质与勘探,2005,41(3)
[50]王联魁,张绍立,黄智龙.华南金矿二元混合成矿模式.矿床地质,1995,14(1).
[51]王祖伟.蚀变构造岩型银金矿床地质地球化学及资源潜力,博士论文,1998:65-67.
[52]王祖伟、周永章、张海华、周汉文.云开基底演化与成矿作用.前寒武纪研究进展, 1998,21(1):45-53
[53]武汉地质学院地球化学教研室.地球化学.北京:地质出版社,1979:32-34.
[54] Tayor, H.P. and Mcdenna, S.M.. The continental crust: Its composition and evolution, Blackwell Scientific Publications, 1985.
[55]黎彤.中国陆壳及其沉积层和上陆壳的化学元素丰度.地球化学, 1994,23(2).
[56]鄢明才,迟清华,顾铁新等.中国东部上地壳化学组成.中国科学(D辑),1997,27(3).
[57]段嘉瑞,何绍勋,张曾荣.广东吴川—四会断裂构造综合体.中国大陆构造论文集.武汉:中国地质大学出版社,1992.
[58]周永章,E.H. Chown, J. Guha.地质热场中微量元素迁移的方向性和分维结构图象.中国科学,1994,24(12):1308-1313.
[59]凌井生,赵士杰,肖鸿群等.广东省河台金矿区高村矿床地质勘查报告,1987.
[60]凌井生,裘有守,陈础廷等.云开大山及其外围金矿远景区成矿条件.北京:地质出版社,1992:91-96.
[61]杜均恩,马超槐,张国恒.广东长坑金、银矿成矿特征.广东地质,1993, 8 (3) : 1-8
[62]张生,李统锦,王联魁.广东长坑大型-超大型金银矿床的地球化学与成因.矿床地质,1998,17(2):125-134.
[63]关康,裘有守,颜竹筠.长坑金矿床地质特征与成因探讨.贵金属地质,1997,6(1).
[64]张湖,李锦统.微细浸染型金矿床的一种新的亚类———硅质岩型金矿.地学前缘, 2004,11(2):364-371.
[65]梁化英,夏萍,王秀璋等.长坑矿田金、银矿床地球化学特征及形成差异分析.地质评论,1998,34(2):131-133
[66].毛晓冬,刘云华.广东长坑金、银矿床成矿模式.地质科技情报,2004,23(2):82-85.
[67]孙晓明,陈炳辉.粤中长坑金银矿热泉成因及其地质意义.中山大学学报(自然科学版),1995,34(2):131-133.
[68] Cargill S.M., Meyer R.F.,Picklyk D.D..Urguidi F.. Summary of resource assement methods resulting from the international geologocal correlation program project 98. J.Int. Assoc. Math. Geol., 1977,9(3).
[69]中国地质科学院.矿产资源评价的理论和实践.1982:35-45
[70] Erickson R. L.. Crustal abundance of elements and mineral reserves and resoueces [A]. U.S. Geol. Surv. Profess paper 820[C],1973,21-25.
[71]中国科学院地球化学研究所.高等地球化学[M] .北京:科学出版社,2000:1~491.
[72]谢学锦.区域化探[M] .北京:地质出版社,1979.
[73] Meyer, W. T., Theobald, P.K. and Bloom,H.. Stream sediment geochemistry [A] In: Peter J. Hood(Ed). Geophysics and geochemistry in the search for metallic ores [C],Proceedings of exploration 77, Economic Geology Report 31. Geological Survey of Canada, Ottawa, Canada,1979: 411-434.
[74] Xie Xuejing, Liu Dawen, Xiang Yunchun et al. Geochemical blocks for predicting large ore deposits- concept and mathodology. J. Geochem. Explor. 2004, 84: 77-91.
[75]刘大文,谢学锦.基于地球化学块体概念的中国锡资源潜力评价.中国地质, 2005, Vol.32
[76]刘大文,向运川,连长云等.水系沉积物中的金属元素在中国东部不同构造单元的分布特征[J].地质与勘探,2002, 38:156~163.
[77]迟清华.岩石化学元素丰度在地球化学块体研究中的意义.物探与化探,2003,27(6).
[78]鄢明才,迟清华.中国东部地壳与岩石的化学组成[M] .北京:科学出版社,1997:11 - 155.
[79]严已宽,张振瑗.中国东部地区地球化学块体内矿产资源潜力预测成果报告(广东部分).广东省地质调查院,2001.
[80]广东省地质矿产局.广东省金矿矿产卡片集,1986.
[81]王祖伟、周永章.粤桂云开地区庞西垌-金山银金矿床地球化学特征与资源潜力.北京:地质出版社,2003:95p.
[2]李树枝,闫卫东,奚生生.2000—2001年世界矿产资源勘查开发和矿产品供需形势[A] .国土资源部信息中心.世界矿产资源年评[C] .北京:地质出版社, 2002:12-19.
[3]涂光炽.关于超大型矿床的寻找和理论研究.地球科学进展,1989,6
[4]涂光炽.关于寻找超大型金矿的问题.四川地质学报,1992,12
[5]裴荣富,熊群尧.中国特大型金属矿床成矿偏在性与成矿构造聚敛(场) .矿床地质,1999, 8(1)
[6]裴荣富等.难识别及隐伏大矿、富矿资源潜力的地质评价.北京:地质出版社,2001:97-117.
[7]王世称,陈永良.中国大型金矿床空间分布规律及找矿方向.地球科学,1999,24(5)
[8]朱炳泉.壳幔化学不均一性与块体地球化学边界研究.地学前缘,1998,5(1~2).
[9]朱炳泉,常向阳.地球化学省与地球化学边界.地球科学进展. 2001,16(2).
[11]谢学锦、刘大文、向运川等.地球化学块体—概念和方法学的发展.中国地质, 2002, 29(3).
[12]谢学锦.用新观念与新技术寻找巨型矿床.科学中国人,.[J] .1995,(5):14-16.
[13]谢学锦,向运川.巨型矿床的地球化学预测方法.走向21世纪矿勘查地球化.北京:地质出版社,1999. 63
[14]刘大文.地球化学块体的概念及其研究意义.地球化学,2002,31(6).
[15]翟裕生.中国区域成矿特征及若干值得重视的成矿环境.中国地质,2003, 30(4)
[16] Xie Xue jing. Empirical prospecting, scientific exploration and information exploration [J]. J.Geochem. Explor., 1999,76:97-108.
[17]谢学锦.勘查地球化学:发展史·现状·展望.地质与勘探, 2002,38(6)
[18]吴传璧,施俊法.矿产勘查与信息找矿[A] .走向21世纪矿产勘查地球化学[C] .北京:地质出版社,1999:48-60.
[19]奚小环,张连.地质矿产部“八五”期间物探、化探、遥感勘查若干新进展[J ] .物探与化探, 1997 , 21(1) :1-5.
[20]王学求.矿产勘查地球化学过去的成就与未来的挑战.地学前缘,2003, 10(1)
[21]谢学锦.全球地球化学填图.中国地质,2003,30(1)
[22]谢学锦.2020年的勘查地球化学—从勘查地球化学到应用地球化学.地质通报,2003,22(11-12)
[23] Potter J. F. Editorial .[J]. Environmentalist, 1990(3-4).
[24] Xie Xuejing, Mu Xuzhang, Ren Tianxiang. Geochemical mapping on Chinal. J. Geochem. Explor. , 1997, 60: 99～113.
[25]谢学锦.中国化探发展的新战略[J] .物探与化探,1992,16(2).
[26] Xie Xuejing, Yin Bingchuan. Geochemical patterns from local to global. J. Geochem. Explor. , 1993, 47: 109～129.
[27]Hawkes H.E. and Webb J. S. Geochemistry in mineral exploration [M]. New York: Harper and Row,1962:1~415.
[28] Closs L. G. .Exploration geochemistry:expanding contributions to mineral resource development.[A] In: Gubins A. G. proceedings 97C,1998:3~8.
[29]王学求.巨型矿床与大型矿集区勘查地球化学.走向21世纪矿勘查地球化.北京:地质出版社,1999:37.
[30] Wang Xueqiu . Leaching of mobile forms of metals for giant ore deposits .J.Geochem. Explor. 199 8, 61:39~55
[31] Seager R.,Meyer M. Gold distribution in supercrustal rocks from Archean greenstone bell of South Africa and complexes of European Alps: metallogenicimplication. Econ. Geo. ,1982,77(1).
[32]谢学锦.战术性与战略性的深穿透地球化学.走向21世纪矿勘查地球化.北京:地质出版社,1999:92~102
[33]翟裕生.区域成矿学.北京:地质出版社,1999.
[34] Sillitoe R. H. Giant and bonanza gold deposits in epithemal environment: Assessment of potential genetic factors. In: Whiteing B.H.,Hodgson C J, Mason R. ed, Giant ore Deposits, 1993.
[35]黄汉鼎,张振瑷,李炳荣等.广东省金矿矿产资源总量预测报告(内部资料) .1987:15.
[36] Zhou, Y. Z. .Geology and Geochemistry of the Hetai Gold Field, Southern China, Guangzhou: South China University of Technology Press, 1993:310
[37]张国恒,董玉成,谭能超等.广东省高明市富湾银矿区普查报告. 1995
[38]南颐,周国强主编.广东省岩石地层.武汉:中国地质大学出版社,1996,19~25
[40] ]周国强,郑有铭,吴安生.两广云开地区的前震旦纪地层.中国区域地质,1996,No.4.
[41]孙培基、韦永福主编.当代中国金矿地质.北京:地震出版社,1996:8-12.
[42]覃慕陶,凌井生,王正云.粤西地区金矿成矿条件及远景预测研究.当代中国金矿地质.北京:地震出版社,1996: 160-167.
[43]凌井生、陈础廷、季明均.广东省高要县河台韧性剪切带蚀变糜棱岩型金矿床地质研究. 1990:5-10孙培基、韦永福主编.当代中国金矿地质.北京:地震出版社,1996: 8-12.
[44]彭少梅.粤北新洲逆冲推覆构造及金矿成矿系列.武汉:中国地质大学出版社,1992:
[45]周永章.华南河台金矿田的地质地球化学研究(摘要).地质地球化学, 1993, No.5.
[46]栾世伟等编著.金矿床地南及找矿方法.成都:四川科学技术出版社,1987:208-211.
[47]张敬陆.从闪长岩与金矿的关系谈金矿的岩浆成矿机理.黄金地质科技,1989,No.2
[48]涂光炽.几个金矿地质传统认识的质疑―涂光炽教授在“中国花岗岩-绿岩地体的金矿”项目第二次工作会议上的报告.国外前寒武纪地质. 1994,No.1
[49]申玉科,邓军,徐叶兵.煌斑岩在玲珑金矿田形成过程中的地质意义.地质与勘探,2005,41(3)
[50]王联魁,张绍立,黄智龙.华南金矿二元混合成矿模式.矿床地质,1995,14(1).
[51]王祖伟.蚀变构造岩型银金矿床地质地球化学及资源潜力,博士论文,1998:65-67.
[52]王祖伟、周永章、张海华、周汉文.云开基底演化与成矿作用.前寒武纪研究进展, 1998,21(1):45-53
[53]武汉地质学院地球化学教研室.地球化学.北京:地质出版社,1979:32-34.
[54] Tayor, H.P. and Mcdenna, S.M.. The continental crust: Its composition and evolution, Blackwell Scientific Publications, 1985.
[55]黎彤.中国陆壳及其沉积层和上陆壳的化学元素丰度.地球化学, 1994,23(2).
[56]鄢明才,迟清华,顾铁新等.中国东部上地壳化学组成.中国科学(D辑),1997,27(3).
[57]段嘉瑞,何绍勋,张曾荣.广东吴川—四会断裂构造综合体.中国大陆构造论文集.武汉:中国地质大学出版社,1992.
[58]周永章,E.H. Chown, J. Guha.地质热场中微量元素迁移的方向性和分维结构图象.中国科学,1994,24(12):1308-1313.
[59]凌井生,赵士杰,肖鸿群等.广东省河台金矿区高村矿床地质勘查报告,1987.
[60]凌井生,裘有守,陈础廷等.云开大山及其外围金矿远景区成矿条件.北京:地质出版社,1992:91-96.
[61]杜均恩,马超槐,张国恒.广东长坑金、银矿成矿特征.广东地质,1993, 8 (3) : 1-8
[62]张生,李统锦,王联魁.广东长坑大型-超大型金银矿床的地球化学与成因.矿床地质,1998,17(2):125-134.
[63]关康,裘有守,颜竹筠.长坑金矿床地质特征与成因探讨.贵金属地质,1997,6(1).
[64]张湖,李锦统.微细浸染型金矿床的一种新的亚类———硅质岩型金矿.地学前缘, 2004,11(2):364-371.
[65]梁化英,夏萍,王秀璋等.长坑矿田金、银矿床地球化学特征及形成差异分析.地质评论,1998,34(2):131-133
[66].毛晓冬,刘云华.广东长坑金、银矿床成矿模式.地质科技情报,2004,23(2):82-85.
[67]孙晓明,陈炳辉.粤中长坑金银矿热泉成因及其地质意义.中山大学学报(自然科学版),1995,34(2):131-133.
[68] Cargill S.M., Meyer R.F.,Picklyk D.D..Urguidi F.. Summary of resource assement methods resulting from the international geologocal correlation program project 98. J.Int. Assoc. Math. Geol., 1977,9(3).
[69]中国地质科学院.矿产资源评价的理论和实践.1982:35-45
[70] Erickson R. L.. Crustal abundance of elements and mineral reserves and resoueces [A]. U.S. Geol. Surv. Profess paper 820[C],1973,21-25.
[71]中国科学院地球化学研究所.高等地球化学[M] .北京:科学出版社,2000:1~491.
[72]谢学锦.区域化探[M] .北京:地质出版社,1979.
[73] Meyer, W. T., Theobald, P.K. and Bloom,H.. Stream sediment geochemistry [A] In: Peter J. Hood(Ed). Geophysics and geochemistry in the search for metallic ores [C],Proceedings of exploration 77, Economic Geology Report 31. Geological Survey of Canada, Ottawa, Canada,1979: 411-434.
[74] Xie Xuejing, Liu Dawen, Xiang Yunchun et al. Geochemical blocks for predicting large ore deposits- concept and mathodology. J. Geochem. Explor. 2004, 84: 77-91.
[75]刘大文,谢学锦.基于地球化学块体概念的中国锡资源潜力评价.中国地质, 2005, Vol.32
[76]刘大文,向运川,连长云等.水系沉积物中的金属元素在中国东部不同构造单元的分布特征[J].地质与勘探,2002, 38:156~163.
[77]迟清华.岩石化学元素丰度在地球化学块体研究中的意义.物探与化探,2003,27(6).
[78]鄢明才,迟清华.中国东部地壳与岩石的化学组成[M] .北京:科学出版社,1997:11 - 155.
[79]严已宽,张振瑗.中国东部地区地球化学块体内矿产资源潜力预测成果报告(广东部分).广东省地质调查院,2001.
[80]广东省地质矿产局.广东省金矿矿产卡片集,1986.
[81]王祖伟、周永章.粤桂云开地区庞西垌-金山银金矿床地球化学特征与资源潜力.北京:地质出版社,2003:95p.