海南省儋州市南江铅锌多金属矿成矿规律与成矿预测研究
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摘要
海南省儋州市南江铅锌多金属矿区位于海南岛中北部,处于岭南褶皱系五指山褶皱带北缘,王五-文教深大断裂带的南侧。本文结合生产实际,通过区域成矿地质背景、矿区地质特征和物化探工作的研究,首次全面系统地论述了矿区铅锌矿和褐铁矿矿体地质特征,明确了矿床成因和成矿规律,提出了本区成矿模式,总结了找矿标志并对矿区找矿远景区和资源量进行预测。
研究发现,矿区出露地层为志留系下统空列村组(S1k)和石炭系下统南好组(Cn-q)及第四系(Q)；矿区褶皱构造不发育,为一单斜地层；断裂和节理较发育,共发育有7条断裂,走向北北东向、北西向及近东西向；矿区南部和西北角可见海西-印支期黑云母二长花岗岩侵入,脉岩发育。矿区发育有铅锌矿和褐铁矿体,铅锌矿呈透镜状、脉状产出；新发现褐铁矿(化)体由四个矿段组成,分别标为Ⅰ号矿段、Ⅱ号矿段、Ⅲ号矿段、Ⅳ号矿段,矿(化)体走向北北东向,倾向南东,倾角40°-70°,断续长达800m,地表出露宽度10-100m左右,呈脉状、透镜状产出,规模较大,矿体品位很高质量较好。根据物化探异常分析,圈出物探异常极化率异常带一处,视电阻率低阻带两处,化探异常发现三处较明显,物化探异常与地质工作成果相同。
研究认为,矿区成矿物质来源主要为地层沉积和岩浆热液来源,铅锌和褐铁矿主要受地层、断裂和岩浆岩控制。铅锌矿赋矿围岩为志留系空列村组(S1K)结晶灰岩,F6断层控制了南江铅锌矿的产出,呈北东向为矿液运移提供通道,后期发育了一系列缝隙,组成容矿构造。褐铁矿(化)体产于石炭系下统南好组上段(C1n—2)地层中,区内三组NNE向断裂控制了矿体的产出并为矿液运移提供通道。蓝洋岩体富碱、富钾、钙碱性,岩体分异指数高,分异程度完好,为铅锌矿和褐铁矿成矿提供热液流体和物质来源。根据矿床地质特征,结合物化探异常分析结果,认为铅锌矿为碳酸盐岩与花岗岩接触带附近成矿物质沿裂隙向上侵入成矿,为一中小型浅成交代热液矿床,成矿时期为海西-印支期；褐铁矿成矿时期为海西-印支期到中生代后,为中低温热液交代充填一风化淋滤型矿床。
Nanjiang lead-zinc polymetallic deposit in Danzhou city Hainan province is located in north-central Hainan Island, in department of Lingnan fold belt north edge of Wuzhishan and in the south of Wang wu to Wenjiao deep faults. Combined with actual production, through investigating regional geological background, mining area geological features, and geophysical and geochemical works, we discuss the lead and limonite ore geological features comprehensively and systematically for the first time, demonstrate the ore genesis and metallogenetic rules, propose mineralization model in this area, summarize ore-hunting indicators and forecast the mining and resource prospecting area in this article.
The follwing facts have been discovered after careful study:Kong liecun formation(S1k) strata in lower Silurian, Nanhao Formation(Cn—q) strata in lower Carboniferous and Quaternary were exposed in the mining area;the fold structure was not developeded and there is only one monoclinic stratum in the mining area; fractures and joints were developed, and there are seven fractures with strick direction of NNE, NW and EW in the mining area;Hercynian-Indosinian biotite monzogranite was appeared in the south and northwest of the mining area and vein rocks was found here.Lead-zinc ore and limonite body were developed in the mining area. lead-zinc ore was discovered with their occurrence being vein state and lens, and limonite body is composed by four ore blocks which was labeled by ore blockⅠ,ore blockⅡ, ore blockⅢand ore blockⅣ, respectively. The orebody with strick direction of NNE, tilt direction of SE and dip 40(degrees)-70(degrees) extend 800 meter sapproximately.The orebody with their occurrence being vein state and lens was exposed at the surface of the earth and its width is about 10-100 meters.According to analysis of geophysical and geochemical anomalies, one place with abnormal polarization geophysical anomaly, two places with low apparent resistivity geochemical anomaly and three places with geochemical anomaly were found.The above geophysical and geochemical anomalies are identical with the geological works.
It is believed by investigating that ore-forming material sources in the mining area are mainly from the stratum and magmatic hydrothermal sources, and lead-zinc and limonite are mainly controled by the strata, fracture and magmatic. The wall rocks of lead-zinc is crystalline limestone which is hosted in Kong Lie Cun Formation strata(S1K) in Silurian. Nanjiang lead-zinc deposit is controlled by F6 fault and the channels for ore solution migration is provided by the NE-trending faults(F6 fault). A series of cracks were developed after the fault formed and the ore-hosting structures are composed by them. Limonite deposit is hosted in the Nanhao Formation (C1n—2) strata in lower carboniferous, and the orebody is controlled by the NNE-trending faults and the channels for ore solution migration is provided by these faults. The Lanyang rock mass is alkali-rich, K-rich, calc-alkaline, and it has high differentiation index and good degree of differentiation, and hydrothermal fluids and materials sources for lead-zinc ore and limonite mineralization are provided by it. According to geological characteristics, combined with geophysical and geochemical anomalies, we speculate preliminarily that lead-zinc deposit is a middle and small hypabyssal metasomatic hydrothermal deposits, which mineralization period is Hercynian Indosinian; The mineralization period of limonite ore is from the Hercynian-Indosinian to the Mesozoic and it is a middle-low temperature hydrothermal type related tometasomstic filling-weathering and leaching deposit.
研究发现,矿区出露地层为志留系下统空列村组(S1k)和石炭系下统南好组(Cn-q)及第四系(Q)；矿区褶皱构造不发育,为一单斜地层；断裂和节理较发育,共发育有7条断裂,走向北北东向、北西向及近东西向；矿区南部和西北角可见海西-印支期黑云母二长花岗岩侵入,脉岩发育。矿区发育有铅锌矿和褐铁矿体,铅锌矿呈透镜状、脉状产出；新发现褐铁矿(化)体由四个矿段组成,分别标为Ⅰ号矿段、Ⅱ号矿段、Ⅲ号矿段、Ⅳ号矿段,矿(化)体走向北北东向,倾向南东,倾角40°-70°,断续长达800m,地表出露宽度10-100m左右,呈脉状、透镜状产出,规模较大,矿体品位很高质量较好。根据物化探异常分析,圈出物探异常极化率异常带一处,视电阻率低阻带两处,化探异常发现三处较明显,物化探异常与地质工作成果相同。
研究认为,矿区成矿物质来源主要为地层沉积和岩浆热液来源,铅锌和褐铁矿主要受地层、断裂和岩浆岩控制。铅锌矿赋矿围岩为志留系空列村组(S1K)结晶灰岩,F6断层控制了南江铅锌矿的产出,呈北东向为矿液运移提供通道,后期发育了一系列缝隙,组成容矿构造。褐铁矿(化)体产于石炭系下统南好组上段(C1n—2)地层中,区内三组NNE向断裂控制了矿体的产出并为矿液运移提供通道。蓝洋岩体富碱、富钾、钙碱性,岩体分异指数高,分异程度完好,为铅锌矿和褐铁矿成矿提供热液流体和物质来源。根据矿床地质特征,结合物化探异常分析结果,认为铅锌矿为碳酸盐岩与花岗岩接触带附近成矿物质沿裂隙向上侵入成矿,为一中小型浅成交代热液矿床,成矿时期为海西-印支期；褐铁矿成矿时期为海西-印支期到中生代后,为中低温热液交代充填一风化淋滤型矿床。
Nanjiang lead-zinc polymetallic deposit in Danzhou city Hainan province is located in north-central Hainan Island, in department of Lingnan fold belt north edge of Wuzhishan and in the south of Wang wu to Wenjiao deep faults. Combined with actual production, through investigating regional geological background, mining area geological features, and geophysical and geochemical works, we discuss the lead and limonite ore geological features comprehensively and systematically for the first time, demonstrate the ore genesis and metallogenetic rules, propose mineralization model in this area, summarize ore-hunting indicators and forecast the mining and resource prospecting area in this article.
The follwing facts have been discovered after careful study:Kong liecun formation(S1k) strata in lower Silurian, Nanhao Formation(Cn—q) strata in lower Carboniferous and Quaternary were exposed in the mining area;the fold structure was not developeded and there is only one monoclinic stratum in the mining area; fractures and joints were developed, and there are seven fractures with strick direction of NNE, NW and EW in the mining area;Hercynian-Indosinian biotite monzogranite was appeared in the south and northwest of the mining area and vein rocks was found here.Lead-zinc ore and limonite body were developed in the mining area. lead-zinc ore was discovered with their occurrence being vein state and lens, and limonite body is composed by four ore blocks which was labeled by ore blockⅠ,ore blockⅡ, ore blockⅢand ore blockⅣ, respectively. The orebody with strick direction of NNE, tilt direction of SE and dip 40(degrees)-70(degrees) extend 800 meter sapproximately.The orebody with their occurrence being vein state and lens was exposed at the surface of the earth and its width is about 10-100 meters.According to analysis of geophysical and geochemical anomalies, one place with abnormal polarization geophysical anomaly, two places with low apparent resistivity geochemical anomaly and three places with geochemical anomaly were found.The above geophysical and geochemical anomalies are identical with the geological works.
It is believed by investigating that ore-forming material sources in the mining area are mainly from the stratum and magmatic hydrothermal sources, and lead-zinc and limonite are mainly controled by the strata, fracture and magmatic. The wall rocks of lead-zinc is crystalline limestone which is hosted in Kong Lie Cun Formation strata(S1K) in Silurian. Nanjiang lead-zinc deposit is controlled by F6 fault and the channels for ore solution migration is provided by the NE-trending faults(F6 fault). A series of cracks were developed after the fault formed and the ore-hosting structures are composed by them. Limonite deposit is hosted in the Nanhao Formation (C1n—2) strata in lower carboniferous, and the orebody is controlled by the NNE-trending faults and the channels for ore solution migration is provided by these faults. The Lanyang rock mass is alkali-rich, K-rich, calc-alkaline, and it has high differentiation index and good degree of differentiation, and hydrothermal fluids and materials sources for lead-zinc ore and limonite mineralization are provided by it. According to geological characteristics, combined with geophysical and geochemical anomalies, we speculate preliminarily that lead-zinc deposit is a middle and small hypabyssal metasomatic hydrothermal deposits, which mineralization period is Hercynian Indosinian; The mineralization period of limonite ore is from the Hercynian-Indosinian to the Mesozoic and it is a middle-low temperature hydrothermal type related tometasomstic filling-weathering and leaching deposit.
引文
[1]海南省地质调查院.海南省1：25万琼海县幅区域地质调查报告.2004年10月
[2]中国科学院华南富铁科学研究队.海南岛地质与石碌铁矿地球化学.北京：科学出版社,1986：1-8
[3]彭省临,刘亮明,赖健清著.大型矿山接替资源勘查技术与示范研究.北京：地质出版社,2004：5-9
[4]范永香,阳正熙.成矿规律与成矿预测[M].徐州：中国矿业大学出版社.2003.
[5](苏)M.B.罗蒙诺索夫(M. JIOMOHOCOB著,马万钧译.论地层[M].北京：科学出版社,1958.
[6]曹新志,孙华山,徐伯骏.关于成矿预测研究的若干进展[M].黄金,2003,24(4)：11-14.
[7]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,1988：9-14
[8]张海军.国内成矿规律与成矿预测研究发展与趋势[J].工程科学.2008(1)：28-29
[9]胡旺亮,吕瑞英,高怀忠,等.矿床统计预测方法流程[J].地球科学：中国地质大学学报,1995,20(2)：128-132.
[10]王明志,李闫华,鄢云飞.等.若干成矿预测理论研究综述[J].资源环境与工程.2007,21(4)：363-369
[11]王世称,王於天.综合信息解译原理与矿产预测图编制方法[J].长春：吉林大学出版社,1989
[12]戴自希,盛继福,白冶等.世界铅矿资源的分布与潜力[M].北京：地震出版社,2005,8
[13]陈喜峰,彭润民.铅锌矿床类型划分评析[J].化工矿产地质,2007,(4)：209-214
[14]Bastin E. S.. Contributions toa knowledge of the kad and Zinc Deposits of the Mississ VaHey Region[J]. Geological Society of America,Special Paper,1939, 24:156
[15]Sangster D. F.. Mississippi Valley-type lead-zinc, In:Geology ofCanadian mineral deposittype[J]. Geol Surv Can,1996,(8):253～261
[16]黄智龙,陈进,韩润生,等.云南会泽超大型铅锌矿床地球化学及成因[M]出版社,2004：141
[17]官军.渝东南地区铅锌矿地质特征及成矿模式：[硕士学位论文].成都：成都理工大学,2007：5-7
[18]Leach D. L, Rowan E. L. Genetic link between Ouachita foldbelt tectoni-sm and the Mississippi Valley-type lead-zinc deposits of the Ozarks[J]. Ge-ology,1986,14:931～935
[19]Sawkins F.J..The significance of Na+/K+ and Cl-/SO42+ rations in fluid inchlusions and suiface waters withrespect to the genesis of Misssissippi Valler-type deposite[J].Econ Geol,1968,63:301～305
[20]Oliver J.. Fluid expelled tectonically from orogennic belts:Their role in hydrocar migration and other geologic phenomena[J]. Geology,1986,14:99～102
[21]Frankin J.M., Sangster D.F.,Lydon J.W..Volcanic-associated massive sulfide deposits[J].Economic Geology,1981, (75th Anniv):485～627
[22]Sawkins F.J.. Massive sulfide deposits in relation to geotectonics[J]. Geo-logical Association Of Canada,1976,(Spec Pagerl4):221～240
[23]Stoltz AJ.,Large R.R.. Evaluation of the source control on precious metal grades in volcanic-hosted massive sulfide deposits from wesgem Tasmania[J]. Economic Geology,1992.87:720～738
[24]Stanton R. L. Magmatic evolution and the ore type—lava type afffliatious of volcani exhalative ores[J].Australasian lustitule of Mining & Metallurgy Proceeding.1990,15:101～107
[25]吴健民.地质地球化学进展—铅锌矿床研究与找矿新进展[M].重庆：科学技术社重庆分社,1990：53-63.
[26]Sangster D. F.. Mississippi Valley-type deposits:a geological melange. In: Kisv-G,Grant S K,Pratt WP Koenig J W(eds) International confb Rnooon Missis Aalley-type lead-zinc deposit-s[M]. University of Missouri press,Roll-a,Missouri.1983,7～19
[27]Sangster D.R.World class MVT and SEDEX lead--zinc deposits [A].//Geol. Survey of Canada Mjn. Colloquium,1[C]. Ottawa:Ottawa Congress Centr-e.
[28]朱上庆,黄华盛.层控矿床地质学[M].北京：冶金工业出版社,1988：116-120
[29]large, D.E.沉积岩中的海底喷流铅锌矿床一地质特征与成因评述,1981.《层控矿床和层状矿床》,第九卷.地质出版社,1986：299-322
[30]祝朝辉,张乾,朱笑青,等.中国SEDEX型矿床成矿流体硼、硅、氮—氧同位索组成研评述[J].矿物岩石地球化学通报,2006,25(3)：279-284
[31]Sangster D. F.张明被译.密西西比河谷型与沉积喷气型矿床的对比[J].国外地质科技.1991,(8)：5-20
[32]汪啸风,马大铨,蒋大海,等.海南岛地质(二)岩浆岩.北京：地质出版社,1991：16-22
[33]姚培慧,王可南,杜春林.中国铁矿志[M].北京：冶金工业出版社,1993年12月：8-19
[34]汪国栋,宋雄.中国铁矿成矿地质特征和资源潜力[J].地质找矿论丛,1996,(4)：35-41
[35]许德如,王力,肖勇等.“石碌式”铁氧化物-铜(金)-钴矿床成矿模式初探[J].矿床地质,2008,(6)：681-694
[36]陈国达.地洼学说新进展.北京：科学出版社,1992
[37]侯威,陈惠芳等.海南岛大地构造与金成矿学.北京：科学出版社,1996：8-9
[38]湖南继善矿业有限公司北方分公司.海南省琼中县乘坡农场三队铅锌矿地质普查报告,2009：11-12
[39]汪啸风,马大铨,蒋大海,等.海南岛地质(三)构造地质.北京：地质出版社,1991：78-108,123-132
[40]海南省地质勘查局资源环境调查院符启基、谢新菊等.海南省儋州市南江铅锌矿详查设计书.琼中金洲铅锌矿业有限公司,2006年4月：3-4
[41]汪啸风,马大铨,蒋大海,等.海南岛地质(一)地层古生物.北京：地质出版社,1991：67-127
[42]潘兆橹.结晶学及矿物学.北京：地质出版社,1994：224
[43]海南地质大队何圣华等.儋县兰洋地区钨锡矿初步普查报告.1983
[44]黎彤,袁怀雨,吴胜昔.中国花岗岩类和世界花岗岩类平均化学成分的对比研究[J].大地构造与成矿学,1998,22(1)：29-34
[45]杨中宝.湖南浏阳七宝山铜多金属矿床的地质特征及成因研究[硕士学位论文].长沙：中南大学：30
[46]肖庆辉等.花岗岩研究思维与方法,北京：地质出版社,2002
[47]邱家骧,林景仟.岩石化学.地质出版社.1991：276
[48]戴塔根.微量元素地球化学长沙：中南大学出版社
[49]季克俭等.热液矿床的矿源、水源和热源及矿床分布规律[M].北京：北京科学技术出版社,1991
[50]赵一,林文蔚,等.中国矽卡岩矿床[M].北京：地质出版社,1990：1-2
[51]中国科学院地球化学研究所.铁的地球化学[M].北京：科学出版社,1981：7-10
[52]候德义.找矿勘探地质学[M].北京：地质出版社,1984：205-207
[53]地矿部地矿司南岭铅锌矿专题组.南岭地区铅锌矿床成矿规律[M].湖南长沙：湖南科学技术出版社,1985：53-54
[54]袁见齐,朱上庆,翟峪生.矿床学[M].北京：地质出版社,1993：72-104
[55]宋仕珠.关于紫金县下告铁矿成因类型的重新认识[J].西部探矿工程,2006(8)：30-31
[56]罗文强,张尚坤,张义江,等.陈家山褐铁矿矿床地质特征及矿床成因[J].有色金属(矿山部分),2009,5(3)：29-31,35
[57]孙文涛,孙吉国,刘志远.辽东裂谷中部多金属矿集区成矿规律与成矿模式[J].科技创新导报.2008(6)：77-79
[58]陈毓川,朱裕生.中国矿床成矿模式.北京：地质出版社,1993：151-171
[59]地质矿产部书刊编辑室.勘探地球物理专辑,第一辑磁法勘探.北京：地质出版社,1985：88-96
[60]秦保瑚等.高精度磁法勘探[M].长沙：中南工业大学出版社,1988：229-249
[61]何继善.双频激电法.北京：高等教育出版社,2006：66-89
[62]朴化荣.电磁测深法原理.北京：地质出版社,1990(2)：220-242
[63]戴塔根,龚铃兰,张起钻.应用地球化学.长沙：中南大学出版社,2005
[64]吴锡生,地质矿产部教材编辑室.化探数据处理方法[M].北京：地质出版社,1993：18-36
[65]徐耀鉴.湖南东山钨矿成矿地质条件及成矿预测研究：[硕士论文].长沙：中南大学：28
[66]中华人民共和国国家质量监督检验检疫总局.GB/T 13908-2002.中华人民共和国国家标准-固体矿产地质勘查规范总则.北京：中国标准出版社,2002年8月28日
[2]中国科学院华南富铁科学研究队.海南岛地质与石碌铁矿地球化学.北京：科学出版社,1986：1-8
[3]彭省临,刘亮明,赖健清著.大型矿山接替资源勘查技术与示范研究.北京：地质出版社,2004：5-9
[4]范永香,阳正熙.成矿规律与成矿预测[M].徐州：中国矿业大学出版社.2003.
[5](苏)M.B.罗蒙诺索夫(M. JIOMOHOCOB著,马万钧译.论地层[M].北京：科学出版社,1958.
[6]曹新志,孙华山,徐伯骏.关于成矿预测研究的若干进展[M].黄金,2003,24(4)：11-14.
[7]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,1988：9-14
[8]张海军.国内成矿规律与成矿预测研究发展与趋势[J].工程科学.2008(1)：28-29
[9]胡旺亮,吕瑞英,高怀忠,等.矿床统计预测方法流程[J].地球科学：中国地质大学学报,1995,20(2)：128-132.
[10]王明志,李闫华,鄢云飞.等.若干成矿预测理论研究综述[J].资源环境与工程.2007,21(4)：363-369
[11]王世称,王於天.综合信息解译原理与矿产预测图编制方法[J].长春：吉林大学出版社,1989
[12]戴自希,盛继福,白冶等.世界铅矿资源的分布与潜力[M].北京：地震出版社,2005,8
[13]陈喜峰,彭润民.铅锌矿床类型划分评析[J].化工矿产地质,2007,(4)：209-214
[14]Bastin E. S.. Contributions toa knowledge of the kad and Zinc Deposits of the Mississ VaHey Region[J]. Geological Society of America,Special Paper,1939, 24:156
[15]Sangster D. F.. Mississippi Valley-type lead-zinc, In:Geology ofCanadian mineral deposittype[J]. Geol Surv Can,1996,(8):253～261
[16]黄智龙,陈进,韩润生,等.云南会泽超大型铅锌矿床地球化学及成因[M]出版社,2004：141
[17]官军.渝东南地区铅锌矿地质特征及成矿模式：[硕士学位论文].成都：成都理工大学,2007：5-7
[18]Leach D. L, Rowan E. L. Genetic link between Ouachita foldbelt tectoni-sm and the Mississippi Valley-type lead-zinc deposits of the Ozarks[J]. Ge-ology,1986,14:931～935
[19]Sawkins F.J..The significance of Na+/K+ and Cl-/SO42+ rations in fluid inchlusions and suiface waters withrespect to the genesis of Misssissippi Valler-type deposite[J].Econ Geol,1968,63:301～305
[20]Oliver J.. Fluid expelled tectonically from orogennic belts:Their role in hydrocar migration and other geologic phenomena[J]. Geology,1986,14:99～102
[21]Frankin J.M., Sangster D.F.,Lydon J.W..Volcanic-associated massive sulfide deposits[J].Economic Geology,1981, (75th Anniv):485～627
[22]Sawkins F.J.. Massive sulfide deposits in relation to geotectonics[J]. Geo-logical Association Of Canada,1976,(Spec Pagerl4):221～240
[23]Stoltz AJ.,Large R.R.. Evaluation of the source control on precious metal grades in volcanic-hosted massive sulfide deposits from wesgem Tasmania[J]. Economic Geology,1992.87:720～738
[24]Stanton R. L. Magmatic evolution and the ore type—lava type afffliatious of volcani exhalative ores[J].Australasian lustitule of Mining & Metallurgy Proceeding.1990,15:101～107
[25]吴健民.地质地球化学进展—铅锌矿床研究与找矿新进展[M].重庆：科学技术社重庆分社,1990：53-63.
[26]Sangster D. F.. Mississippi Valley-type deposits:a geological melange. In: Kisv-G,Grant S K,Pratt WP Koenig J W(eds) International confb Rnooon Missis Aalley-type lead-zinc deposit-s[M]. University of Missouri press,Roll-a,Missouri.1983,7～19
[27]Sangster D.R.World class MVT and SEDEX lead--zinc deposits [A].//Geol. Survey of Canada Mjn. Colloquium,1[C]. Ottawa:Ottawa Congress Centr-e.
[28]朱上庆,黄华盛.层控矿床地质学[M].北京：冶金工业出版社,1988：116-120
[29]large, D.E.沉积岩中的海底喷流铅锌矿床一地质特征与成因评述,1981.《层控矿床和层状矿床》,第九卷.地质出版社,1986：299-322
[30]祝朝辉,张乾,朱笑青,等.中国SEDEX型矿床成矿流体硼、硅、氮—氧同位索组成研评述[J].矿物岩石地球化学通报,2006,25(3)：279-284
[31]Sangster D. F.张明被译.密西西比河谷型与沉积喷气型矿床的对比[J].国外地质科技.1991,(8)：5-20
[32]汪啸风,马大铨,蒋大海,等.海南岛地质(二)岩浆岩.北京：地质出版社,1991：16-22
[33]姚培慧,王可南,杜春林.中国铁矿志[M].北京：冶金工业出版社,1993年12月：8-19
[34]汪国栋,宋雄.中国铁矿成矿地质特征和资源潜力[J].地质找矿论丛,1996,(4)：35-41
[35]许德如,王力,肖勇等.“石碌式”铁氧化物-铜(金)-钴矿床成矿模式初探[J].矿床地质,2008,(6)：681-694
[36]陈国达.地洼学说新进展.北京：科学出版社,1992
[37]侯威,陈惠芳等.海南岛大地构造与金成矿学.北京：科学出版社,1996：8-9
[38]湖南继善矿业有限公司北方分公司.海南省琼中县乘坡农场三队铅锌矿地质普查报告,2009：11-12
[39]汪啸风,马大铨,蒋大海,等.海南岛地质(三)构造地质.北京：地质出版社,1991：78-108,123-132
[40]海南省地质勘查局资源环境调查院符启基、谢新菊等.海南省儋州市南江铅锌矿详查设计书.琼中金洲铅锌矿业有限公司,2006年4月：3-4
[41]汪啸风,马大铨,蒋大海,等.海南岛地质(一)地层古生物.北京：地质出版社,1991：67-127
[42]潘兆橹.结晶学及矿物学.北京：地质出版社,1994：224
[43]海南地质大队何圣华等.儋县兰洋地区钨锡矿初步普查报告.1983
[44]黎彤,袁怀雨,吴胜昔.中国花岗岩类和世界花岗岩类平均化学成分的对比研究[J].大地构造与成矿学,1998,22(1)：29-34
[45]杨中宝.湖南浏阳七宝山铜多金属矿床的地质特征及成因研究[硕士学位论文].长沙：中南大学：30
[46]肖庆辉等.花岗岩研究思维与方法,北京：地质出版社,2002
[47]邱家骧,林景仟.岩石化学.地质出版社.1991：276
[48]戴塔根.微量元素地球化学长沙：中南大学出版社
[49]季克俭等.热液矿床的矿源、水源和热源及矿床分布规律[M].北京：北京科学技术出版社,1991
[50]赵一,林文蔚,等.中国矽卡岩矿床[M].北京：地质出版社,1990：1-2
[51]中国科学院地球化学研究所.铁的地球化学[M].北京：科学出版社,1981：7-10
[52]候德义.找矿勘探地质学[M].北京：地质出版社,1984：205-207
[53]地矿部地矿司南岭铅锌矿专题组.南岭地区铅锌矿床成矿规律[M].湖南长沙：湖南科学技术出版社,1985：53-54
[54]袁见齐,朱上庆,翟峪生.矿床学[M].北京：地质出版社,1993：72-104
[55]宋仕珠.关于紫金县下告铁矿成因类型的重新认识[J].西部探矿工程,2006(8)：30-31
[56]罗文强,张尚坤,张义江,等.陈家山褐铁矿矿床地质特征及矿床成因[J].有色金属(矿山部分),2009,5(3)：29-31,35
[57]孙文涛,孙吉国,刘志远.辽东裂谷中部多金属矿集区成矿规律与成矿模式[J].科技创新导报.2008(6)：77-79
[58]陈毓川,朱裕生.中国矿床成矿模式.北京：地质出版社,1993：151-171
[59]地质矿产部书刊编辑室.勘探地球物理专辑,第一辑磁法勘探.北京：地质出版社,1985：88-96
[60]秦保瑚等.高精度磁法勘探[M].长沙：中南工业大学出版社,1988：229-249
[61]何继善.双频激电法.北京：高等教育出版社,2006：66-89
[62]朴化荣.电磁测深法原理.北京：地质出版社,1990(2)：220-242
[63]戴塔根,龚铃兰,张起钻.应用地球化学.长沙：中南大学出版社,2005
[64]吴锡生,地质矿产部教材编辑室.化探数据处理方法[M].北京：地质出版社,1993：18-36
[65]徐耀鉴.湖南东山钨矿成矿地质条件及成矿预测研究：[硕士论文].长沙：中南大学：28
[66]中华人民共和国国家质量监督检验检疫总局.GB/T 13908-2002.中华人民共和国国家标准-固体矿产地质勘查规范总则.北京：中国标准出版社,2002年8月28日