康滇地轴南段江川—建水地区铀矿化特征与找矿前景
|
摘要
本论文以中国核工业地质局基础地质项目“康滇地轴铀矿资源潜力评价”和“康滇地轴南段江川306铀矿点深部钻探查证”为依托。在总结和深入分析前人资料的基础上,以具有代表性的江川306铀矿点为重点研究对象,详细研究了该点的铀矿化特征、控矿因素、成矿条件等,建立起江川地区的铀矿成矿模式。采用“点上研究寻求规律,面上调查寻找与点上相似的成矿地质环境”的技术路线,提出可供进一步开展工作的找矿前景区。论文研究取得了以下主要成果及认识:
1.通过调查研究江川-建水地区澄江组砂岩的岩石地层结构与沉积相特征,将澄江组划分为3段,第一段以冲积扇相沉积为特征;第二段以三角洲-湖泊相沉积为特征;第三段以辫状河-曲流河相沉积为特征。
2.江川306铀矿点铀矿化赋存于断裂构造带内以及断裂构造带旁侧澄江组第二段杂色砂岩构造裂隙中,铀矿化地段发育了硅化、绿泥石-水云母化、金属硫化物化、绢云母化、赤铁矿化等中-低温热液蚀变;铀成矿的控制因素主要为断裂构造,其次为中新元古界不整合面;成矿流体可能来源于基底岩石并切穿中新元古界不整合面的贯通性断裂带。
3.经江川306铀矿点深部钻探查证证实,306断裂为多期活动性断裂,早期为张性断裂,晚期为逆冲断裂。断裂带内存在热液活动中心,并非沿整个断裂带都存在热液活动。热液上升的通道位于采场附近断裂带转弯膨胀部位,从而形成“蘑菇”状构造蚀变带。铀矿化赋存于构造带内蚀变砂岩、砂砾岩、砾岩、泥岩中。
4.通过面上路线地质调查及地面伽玛能谱测量,在通海地区发现2条与306铀矿点相似的地质、构造蚀变带,构造蚀变带内有铀当量异常显示。
5.通过对江川306铀矿点特征与控矿因素的研究,探讨了该区的铀成矿模式,并对江川-建水地区铀矿资源潜力进行了评价。提出下一步找矿的重点部位应放在切穿中新元古界不整合面的断裂构造蚀变带上,具体是“一点一地区”,即江川县306铀矿点与通海地区。
上述成果和认识突破了该区受“层位”和“不整合面”控制的传统观点,对江慈?水地区今后的找矿和预测工作具有十分重要的指导意义。
The dissertation is supported by China National Nuclear Corporation project, studying“The uranium resources potential evaluation of Kangdian Axis”and“The depth portion drilling verification of 306 uranium in Jiangchuan of in South Section of Kangdian Axis”as a backing.In summarizes and analyzes the predecessor material thoroughly in the foundation, take has representative in Jiangchuan 306 uranium mine as the key object of study, which dissect uranium mineralization characteristic, ore-controlling factors, mineralization condition etc.,and establishes ore-forming model of the uranium mine in Jiangchuan area.Using“seek the rule to research the point, and seek with the point the similar mineralization geological environment on the surface investigates”the technical route, and proposed that before may supply to further do the work the prospecting. The author acquired some outcomes and recognitions:
1. Studying detailedly the rock stratal texture and sedimentary facies characteristics of the Jiangchuan to Jianshui area, the author dividesd in 3 sections of Chengjiang group sandstone's, such as the first section take alluvial fan facies as the characteristic; the second section take delta-lacustrine facies as the characteristic; the third section take braided-meandering river facies as the characteristic.
2. The uranium mine mineralization of Jiangchuan 306 hosted in the faulted structure belt as well as in the faulted structure belt side the second section of Chengjiang group mottled sandstone structure crevasse, which grow the low temperature hydrothermal alteration, such as silicalite, chloritization-hydromicatizatio-n, metal-sulfide, sericite, hematite etc. The main controlling factors of uranium mineralization is fault , next for Meso- to Neoproterozoic unconformity; the mineralization fluid possibly originates from under the basis rock and through fault incised the Meso- to Neoproterozoic unconformity.
3. Confirmed after the uranium mine depth portion drilling verification of Jiangchuan 306, that 306 fault for many issue of activity faults, the eraly is extension fault, the later is reverse fault. In the fault zone has the hydrothermal activity center, by no means along the entire fault zone. Hydrothermal rise channel located at stope nearby fault zone curve inflation spot, thus forms the shape“mushroom”structure alteration belt. Uranium ore-body mainly hosted in cataclastic rock in fault and in motley sandstone, cataclastic sandstone, mudstone.
4. Through the geological investigation of route on the surface and ground Gamma-Ray spectrometry, discovered that 2 with 306 uranium mine similar geology environment, and tectonic-alteration belt in the Tonghai, which have the uranium equivalent exceptionally to demonstrate;
5. This paper summaries the characteristic of 306 uranium mine and Ore-controlling factors in Jiangchuan, and discussed its mineralization model. then has carried on the appraisal to the Jiangchuan to Jianshui area uranium mine resources potential. The authors considered, prospecting direction should be alteration belts of through fault incised the Meso- to Neoproterozoic unconformity next, concrete is:“One Point, One Area”, namely 306 uranium mines of Jiangchuan County and Tonghai area.
These achievements and views the author obtained brokethrough inland traditional theory on“The Stratum”and“The Unconformity”, they possess extremely important directing significance for ore exploration and prediction in Jiangchuan to Jianshui area.
1.通过调查研究江川-建水地区澄江组砂岩的岩石地层结构与沉积相特征,将澄江组划分为3段,第一段以冲积扇相沉积为特征;第二段以三角洲-湖泊相沉积为特征;第三段以辫状河-曲流河相沉积为特征。
2.江川306铀矿点铀矿化赋存于断裂构造带内以及断裂构造带旁侧澄江组第二段杂色砂岩构造裂隙中,铀矿化地段发育了硅化、绿泥石-水云母化、金属硫化物化、绢云母化、赤铁矿化等中-低温热液蚀变;铀成矿的控制因素主要为断裂构造,其次为中新元古界不整合面;成矿流体可能来源于基底岩石并切穿中新元古界不整合面的贯通性断裂带。
3.经江川306铀矿点深部钻探查证证实,306断裂为多期活动性断裂,早期为张性断裂,晚期为逆冲断裂。断裂带内存在热液活动中心,并非沿整个断裂带都存在热液活动。热液上升的通道位于采场附近断裂带转弯膨胀部位,从而形成“蘑菇”状构造蚀变带。铀矿化赋存于构造带内蚀变砂岩、砂砾岩、砾岩、泥岩中。
4.通过面上路线地质调查及地面伽玛能谱测量,在通海地区发现2条与306铀矿点相似的地质、构造蚀变带,构造蚀变带内有铀当量异常显示。
5.通过对江川306铀矿点特征与控矿因素的研究,探讨了该区的铀成矿模式,并对江川-建水地区铀矿资源潜力进行了评价。提出下一步找矿的重点部位应放在切穿中新元古界不整合面的断裂构造蚀变带上,具体是“一点一地区”,即江川县306铀矿点与通海地区。
上述成果和认识突破了该区受“层位”和“不整合面”控制的传统观点,对江慈?水地区今后的找矿和预测工作具有十分重要的指导意义。
The dissertation is supported by China National Nuclear Corporation project, studying“The uranium resources potential evaluation of Kangdian Axis”and“The depth portion drilling verification of 306 uranium in Jiangchuan of in South Section of Kangdian Axis”as a backing.In summarizes and analyzes the predecessor material thoroughly in the foundation, take has representative in Jiangchuan 306 uranium mine as the key object of study, which dissect uranium mineralization characteristic, ore-controlling factors, mineralization condition etc.,and establishes ore-forming model of the uranium mine in Jiangchuan area.Using“seek the rule to research the point, and seek with the point the similar mineralization geological environment on the surface investigates”the technical route, and proposed that before may supply to further do the work the prospecting. The author acquired some outcomes and recognitions:
1. Studying detailedly the rock stratal texture and sedimentary facies characteristics of the Jiangchuan to Jianshui area, the author dividesd in 3 sections of Chengjiang group sandstone's, such as the first section take alluvial fan facies as the characteristic; the second section take delta-lacustrine facies as the characteristic; the third section take braided-meandering river facies as the characteristic.
2. The uranium mine mineralization of Jiangchuan 306 hosted in the faulted structure belt as well as in the faulted structure belt side the second section of Chengjiang group mottled sandstone structure crevasse, which grow the low temperature hydrothermal alteration, such as silicalite, chloritization-hydromicatizatio-n, metal-sulfide, sericite, hematite etc. The main controlling factors of uranium mineralization is fault , next for Meso- to Neoproterozoic unconformity; the mineralization fluid possibly originates from under the basis rock and through fault incised the Meso- to Neoproterozoic unconformity.
3. Confirmed after the uranium mine depth portion drilling verification of Jiangchuan 306, that 306 fault for many issue of activity faults, the eraly is extension fault, the later is reverse fault. In the fault zone has the hydrothermal activity center, by no means along the entire fault zone. Hydrothermal rise channel located at stope nearby fault zone curve inflation spot, thus forms the shape“mushroom”structure alteration belt. Uranium ore-body mainly hosted in cataclastic rock in fault and in motley sandstone, cataclastic sandstone, mudstone.
4. Through the geological investigation of route on the surface and ground Gamma-Ray spectrometry, discovered that 2 with 306 uranium mine similar geology environment, and tectonic-alteration belt in the Tonghai, which have the uranium equivalent exceptionally to demonstrate;
5. This paper summaries the characteristic of 306 uranium mine and Ore-controlling factors in Jiangchuan, and discussed its mineralization model. then has carried on the appraisal to the Jiangchuan to Jianshui area uranium mine resources potential. The authors considered, prospecting direction should be alteration belts of through fault incised the Meso- to Neoproterozoic unconformity next, concrete is:“One Point, One Area”, namely 306 uranium mines of Jiangchuan County and Tonghai area.
These achievements and views the author obtained brokethrough inland traditional theory on“The Stratum”and“The Unconformity”, they possess extremely important directing significance for ore exploration and prediction in Jiangchuan to Jianshui area.
引文
[1] R.H.Mc Millan.1980.加拿大重要铀矿床的分类和成因问题[J].放射性地质,第1期:34～41。
[2]陈友良.2004.西南地区铀资源现状与找矿前景展望.铀矿地质[J].铀矿地质20(1):1～15。
[3]陈祖伊.2003.世界铀资源及勘查[J].世界核地质科学,20(2):63～69。
[4]陈祖伊.2002.亚洲砂岩型铀矿区域分布规律和中国砂岩型铀矿找矿对策[J].铀矿地质,18(3):129～137。
[5]川西南地区—铀矿地质工作总结[R].核工业西南地质局二八一大队,1984。
[6]戴杰敏,朱西养.1992.寄希望于康滇地轴——康滇地轴铀矿远景评价研讨会报道[J].铀矿地质,8(3):130～155。
[7]戴杰敏.1992.康滇地轴中、新元古代不整合面铀矿远景分析[J].铀矿地质,8(6):330～337。
[8]郭葆墀,钱法荣,蔡煜琦等.1997.康滇地轴中南段铀成矿条件及远景分析[J].铀矿地质,13(4):202～208。
[9]黄建光.1992.江川盆地及盆缘澄江组砂岩铀、氡水文地球化学特征与铀矿化的关系及成矿远景预测[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,85～87。
[10]黄净白,黄世杰.2005.中国铀资源区域成矿特征[J],铀矿地质,21(3):129～138。
[11]黄世杰,张书栋.1992.有关康滇地轴找矿的若干问题[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,13～16。
[12]黄世杰,从卫克,韩德仁.1995.加拿大萨斯喀彻温省北部若干铀金矿床的考察简介[J].铀矿地质,11(6):373～376。
[13]康滇地轴江地区江川、禄丰不整合面型铀矿的成矿远景[R].核工业北京地质研究院,1994。
[14]康滇地轴元古代地层矿化类型及成矿富集控制因素[R].核工业西南地勘局二八O研究所矿化组,1988。
[15]康滇地轴南段不整合面型铀成矿基本条件的物化探研究[R].核工业北京地质研究院,1996。
[16]康滇地轴中南段铀矿化地质调查报告[R].核工业西南地质局二八一大队,1984。
[17]康滇地轴元古代地层成矿类型、地质背景及找矿方向[R].核工业西南地质局二八O研究所,1990。
[18]康滇地轴元古代地层放射场特征及铀钍分布规律[R].核工业西南地质局二八O研究所,1990。
[19]康滇地轴遥感处理及线性构造解译[R].核工业西南地质局二八O研究所,1990。
[20]康滇地轴元古代地层矿化类型的岩石矿物及地球化学特征[R].核工业西南地质局二八O研究所,1990。
[21]康滇地轴前寒武纪地壳演化特征及铀成矿远景研究[R].核工业西南地质局二八O研究所,1990。
[22]李巨初,罗朝文,童运福.1992.康滇地轴中南段元古界主要矿化类型及其成矿远景初步探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,56～58。
[23]李余华.1998.康滇地轴南段构造—岩浆活动与铀矿化关系探讨[J].云南地质,17(1):81～85。
[24]李余华.1992.康滇地轴南段构造—岩浆活动与铀矿化关系探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,42～43。
[25]李子颖,李胜祥.2000.加拿大萨斯喀彻温省北部铀成矿的特点与启示[J].铀矿地质,16(3):129～135。
[26]刘凤祥.1992.云南江川306铀矿点地质特征[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,61～62。
[27]刘金河.1992.康滇地轴中段铀成矿地质条件及找矿关系浅析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,39～41。
[28]刘兴源,巫声扬,王德生.1992.康滇地轴前震旦纪结晶基底岩系中的铀矿化特征[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,66～67。
[29]刘正安.1992.川滇边区前震旦系含铀性及找矿前景分析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,34～35。
[30]刘英俊,曹励明,等.元素地球化学[M].科学出版社,1984。
[31]罗朝文,李巨初.1992.康滇地轴不整合脉(面)型铀矿床成矿条件评价问题[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,28～29。
[32]罗一月.1990.对康滇地轴铀成矿环境的初步探讨[J].铀矿地质,6(4):226～231。
[33]罗一月,马光中,魏明基.1993.遥感信息在康滇地轴铀资源评价中的应用[J].铀矿地质,9(6):342～346。
[34]罗一月,魏明基,马光中.1998.浅析康滇地轴构造运动与铀成矿的关系[J].铀矿地质,14(2):72～81。
[35]罗一月,马光中,魏明基.1992.对康滇地轴元古代地质体中铀矿化与断裂构造关系的初步探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,36～38。
[36]马光中,罗一月,魏明基.1992.康滇地轴元古界地球化学场特征初探[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,76～77。
[37]潘连昌.1992.康滇地轴地球物理场特征及其与铀矿化的关系[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,68～69。
[38]齐泽润.1992.国外某些铀矿地质特征和康滇地轴找矿问题的探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,47～52。
[39]钱法荣.1996.康滇地轴中南段元古代地层中铀矿化类型及其特征[J].铀矿地质,12(4):214～219。
[40]裘大铨.1992.滇中前寒武系铀成矿条件浅析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,25～27。
[41]徐开礼,朱志澄.构造地质学[M].地质出版社.2003。
[42]孙泽轩.2000.盈江盆地盖层氧化带发育特征及其与铀矿化的关系[J].铀矿地质,16(2):79～84。
[43]孙泽轩,姚毅锋,陈勇,等.2004.龙川江盆地砂岩型铀矿成矿条件及找矿远景分析[J],西南铀矿地质,10(1):1～10。
[44]孙泽轩,陈洪德,吴英,等.2006.滇西新生代盆地与砂岩型铀矿成矿[J],地质论评,52(4):494～500。
[45]田文浩.1992.康滇地轴南段不整合型铀矿地球物理勘查模式探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,88～90。
[46]王鼎云,刘凤祥.1992.康滇地轴南段铀成矿条件及找矿前景[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,30～33。
[47]王隆秋.1995.720富铀矿床热液蚀变及其地球化学特征[J].铀矿地质,11(2):80。
[48]巫声扬,刘兴源,王德生.1992.康滇地轴中南段元古宙主要矿化特征及找矿方向分析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,53～55。
[49]西南铀矿地质志[M].中国核工业地质局,2005。
[50]胥德恩.1992.康滇地轴地壳演化与铀成矿作用探讨[J].铀矿地质,8(6):348～378。
[51]杨云.1992.从江川地区遥感图象特征看铀成矿条件[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,59～60。
[52]云南省康滇地轴南段江川(小冲—长岭岗地段)不整合型铀矿深部探索报告[R].核工业西南地勘局二O九大队,1993。
[53]云南省康滇地轴南段江川县(小冲县—长岭岗地段)不整合型铀矿电磁法深部探索报告[R].核工业西南地勘局二O九大队,1994。
[54]云南省江川县306铀矿点储量估算报告[R].云南省第三地质队,1961。
[55]云南省江川县三O七地区工作总结[R].中南二O九队五队八连二排,1970。
[56]云南省江川县三O六,三O七,三五七,一O一地区外围普查工作小结[R].中南二O九队五队八连一排,1970。
[57]云南省区域地质志[M].地质出版社,1990年。
[58]张书成,白云生,吴慧山.2006.康滇地轴南段不整合面型铀成矿基本条件的物化探研究[J].China Academic Journal Electronic Publishing House,1～12。
[59]张金带,徐高中,陈安平,等.2005.中国可地浸砂岩型铀矿成矿模式初步探讨[J],铀矿地质,21(3):139～145。
[60]张金带,李友良,简晓飞,等.2007.“十五”期间铀矿地质勘查主要成果及“十一五”的总体思路[J].铀矿地质,23(1):1～6。
[61]仉宝聚.2001.铀矿大型矿集区与成矿作用[J].铀矿地质,2001(1):5～17。
[62]赵凤民.1992.碱交代型铀矿床和加拿大不整合脉型铀矿床地质特征和找矿标志[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,44～46。
[63]赵凤民编著.俄罗斯铀矿地质[C],核工业北京地质研究院,2006。
[64]周维勋.元古宙不整合型铀矿及其寻找[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,13～16。
[65] Adams S.S.and Smith R.B..1981.Geology and recognition criteriafor sandstone uranium deposits in mixed fluvial shallow marine sedimentary sequences,South Texas—final report:U.S.Department of Energy , Grand Junction Office , Colorado , Bendix Field Engineering Corporation,GJBX-4(81),p.146.
[66] Adler H.H.and Sharp B.J..1967.Uranium ore rolls-occurrence,genesis,and physical and chemical characteristics[M],in Uranium districts of southeastern Utah: Utah Geological Society Guidebook to Geology of Utah Vol.21:53～77.
[67] Davis J.F..1979.Uranium in the U.S.A.:Genesis and Exploration Implications.Philosophical Transactions of the Royal Society of London.Series A,Mathematical and Physical Sciences,Vol.291(1381):301～306.
[68] Dickinson K. A. and J.S. Duval..1977.South Texas Uranium:Geologic Controls , Exploration Techniques,and Potential,Chapter 2:Trend Areas and Exploration Techniques Utilization in Geology of Alternate Energy Resources in the South-Central United States (M.D.Campbell(ed)),Houston Geological Society,pp.45～66.
[69] Goldhaber M.B. , Reynolds R.L , Rye R..1978.Otigin of a South Texas roll-type uranium deposits: II.Petrology and sulfur isotope studies.Econmic Geology,73(8):1690～1705.
[70] Grange H.C.,Santos.E.S.,Dean.B.G. et al..1961.Sandstone-type uranium deposits at Ambrosia Lake,New Mexico;an interim report.Economic Geology,Vol.56(7):1179～1210.
[71] Harshman E.N.1972.Geology and uranium deposits,Shirley Basin area,Wyoming:U.S. Geological Survey Professional Paper 745,p.82.
[72] Harshman E.N. and Adams S.S..1980.Geology and recognition criteria for roll-type uranium deposits in continental sandstones Final report:U.S.Department of Energy,Grand Junction,Colorado,GJBX-1(81),p.181.
[73] Harshman E .N.,Adams S.S..1981. Geology and Recognition Criteria for Roll-Type Uranium Deposits in Continental Sandstones.Colorado:US Department of Energy,Grand Junction Office,p.185.
[74] Holen H.K. et al..1986.Geological characterization of New Mexico uranium deposits for extraction by In Situ Leach recovery, New Mexico Bureau of Mines and Mineral Resources, Open File Report No.251.
[75] Lambert I et al.,Australia′s Uranium Endoment:Metallogeny,Exploration and Potential,Proceedings of a Technical Committee Meeting《International Symposium Uranium Producti-on and Raw Materials for the Nuclear Fuel Cycle Supply and Demand,Economics,the Envir-onmental and Energy Security》Vienna,2005
[76] OECD(NEA)/IAEA Uranium Resources,Production and Demand,OECD,Paris:1993,1995,1997,1999,2001,2003.
[77] Pollock GD,McArthur River Project,Saskatchewan,Canada,Proceedings of a Technical Committee Meeting《Assessment of Uranium Deposit Types and Resources a worldwide Perspective》IAEA,Vienna,2001.
[78] Roy C et al.,Millennium Deposit - Basementhosted Derivative of the Unconformity Model,Proceedings of a Technical Committee Meeting《International Symposium》Vienna,2005.
[79] Sibbald Tll,Geolgy and genesis of the Althabasca basin uranium deposits,Proceediugs of a T-Echnical Committee Meeting《Recognition of Uranium Provinces》,London,1988.
[2]陈友良.2004.西南地区铀资源现状与找矿前景展望.铀矿地质[J].铀矿地质20(1):1～15。
[3]陈祖伊.2003.世界铀资源及勘查[J].世界核地质科学,20(2):63～69。
[4]陈祖伊.2002.亚洲砂岩型铀矿区域分布规律和中国砂岩型铀矿找矿对策[J].铀矿地质,18(3):129～137。
[5]川西南地区—铀矿地质工作总结[R].核工业西南地质局二八一大队,1984。
[6]戴杰敏,朱西养.1992.寄希望于康滇地轴——康滇地轴铀矿远景评价研讨会报道[J].铀矿地质,8(3):130～155。
[7]戴杰敏.1992.康滇地轴中、新元古代不整合面铀矿远景分析[J].铀矿地质,8(6):330～337。
[8]郭葆墀,钱法荣,蔡煜琦等.1997.康滇地轴中南段铀成矿条件及远景分析[J].铀矿地质,13(4):202～208。
[9]黄建光.1992.江川盆地及盆缘澄江组砂岩铀、氡水文地球化学特征与铀矿化的关系及成矿远景预测[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,85～87。
[10]黄净白,黄世杰.2005.中国铀资源区域成矿特征[J],铀矿地质,21(3):129～138。
[11]黄世杰,张书栋.1992.有关康滇地轴找矿的若干问题[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,13～16。
[12]黄世杰,从卫克,韩德仁.1995.加拿大萨斯喀彻温省北部若干铀金矿床的考察简介[J].铀矿地质,11(6):373～376。
[13]康滇地轴江地区江川、禄丰不整合面型铀矿的成矿远景[R].核工业北京地质研究院,1994。
[14]康滇地轴元古代地层矿化类型及成矿富集控制因素[R].核工业西南地勘局二八O研究所矿化组,1988。
[15]康滇地轴南段不整合面型铀成矿基本条件的物化探研究[R].核工业北京地质研究院,1996。
[16]康滇地轴中南段铀矿化地质调查报告[R].核工业西南地质局二八一大队,1984。
[17]康滇地轴元古代地层成矿类型、地质背景及找矿方向[R].核工业西南地质局二八O研究所,1990。
[18]康滇地轴元古代地层放射场特征及铀钍分布规律[R].核工业西南地质局二八O研究所,1990。
[19]康滇地轴遥感处理及线性构造解译[R].核工业西南地质局二八O研究所,1990。
[20]康滇地轴元古代地层矿化类型的岩石矿物及地球化学特征[R].核工业西南地质局二八O研究所,1990。
[21]康滇地轴前寒武纪地壳演化特征及铀成矿远景研究[R].核工业西南地质局二八O研究所,1990。
[22]李巨初,罗朝文,童运福.1992.康滇地轴中南段元古界主要矿化类型及其成矿远景初步探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,56～58。
[23]李余华.1998.康滇地轴南段构造—岩浆活动与铀矿化关系探讨[J].云南地质,17(1):81～85。
[24]李余华.1992.康滇地轴南段构造—岩浆活动与铀矿化关系探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,42～43。
[25]李子颖,李胜祥.2000.加拿大萨斯喀彻温省北部铀成矿的特点与启示[J].铀矿地质,16(3):129～135。
[26]刘凤祥.1992.云南江川306铀矿点地质特征[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,61～62。
[27]刘金河.1992.康滇地轴中段铀成矿地质条件及找矿关系浅析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,39～41。
[28]刘兴源,巫声扬,王德生.1992.康滇地轴前震旦纪结晶基底岩系中的铀矿化特征[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,66～67。
[29]刘正安.1992.川滇边区前震旦系含铀性及找矿前景分析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,34～35。
[30]刘英俊,曹励明,等.元素地球化学[M].科学出版社,1984。
[31]罗朝文,李巨初.1992.康滇地轴不整合脉(面)型铀矿床成矿条件评价问题[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,28～29。
[32]罗一月.1990.对康滇地轴铀成矿环境的初步探讨[J].铀矿地质,6(4):226～231。
[33]罗一月,马光中,魏明基.1993.遥感信息在康滇地轴铀资源评价中的应用[J].铀矿地质,9(6):342～346。
[34]罗一月,魏明基,马光中.1998.浅析康滇地轴构造运动与铀成矿的关系[J].铀矿地质,14(2):72～81。
[35]罗一月,马光中,魏明基.1992.对康滇地轴元古代地质体中铀矿化与断裂构造关系的初步探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,36～38。
[36]马光中,罗一月,魏明基.1992.康滇地轴元古界地球化学场特征初探[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,76～77。
[37]潘连昌.1992.康滇地轴地球物理场特征及其与铀矿化的关系[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,68～69。
[38]齐泽润.1992.国外某些铀矿地质特征和康滇地轴找矿问题的探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,47～52。
[39]钱法荣.1996.康滇地轴中南段元古代地层中铀矿化类型及其特征[J].铀矿地质,12(4):214～219。
[40]裘大铨.1992.滇中前寒武系铀成矿条件浅析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,25～27。
[41]徐开礼,朱志澄.构造地质学[M].地质出版社.2003。
[42]孙泽轩.2000.盈江盆地盖层氧化带发育特征及其与铀矿化的关系[J].铀矿地质,16(2):79～84。
[43]孙泽轩,姚毅锋,陈勇,等.2004.龙川江盆地砂岩型铀矿成矿条件及找矿远景分析[J],西南铀矿地质,10(1):1～10。
[44]孙泽轩,陈洪德,吴英,等.2006.滇西新生代盆地与砂岩型铀矿成矿[J],地质论评,52(4):494～500。
[45]田文浩.1992.康滇地轴南段不整合型铀矿地球物理勘查模式探讨[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,88～90。
[46]王鼎云,刘凤祥.1992.康滇地轴南段铀成矿条件及找矿前景[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,30～33。
[47]王隆秋.1995.720富铀矿床热液蚀变及其地球化学特征[J].铀矿地质,11(2):80。
[48]巫声扬,刘兴源,王德生.1992.康滇地轴中南段元古宙主要矿化特征及找矿方向分析[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,53～55。
[49]西南铀矿地质志[M].中国核工业地质局,2005。
[50]胥德恩.1992.康滇地轴地壳演化与铀成矿作用探讨[J].铀矿地质,8(6):348～378。
[51]杨云.1992.从江川地区遥感图象特征看铀成矿条件[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,59～60。
[52]云南省康滇地轴南段江川(小冲—长岭岗地段)不整合型铀矿深部探索报告[R].核工业西南地勘局二O九大队,1993。
[53]云南省康滇地轴南段江川县(小冲县—长岭岗地段)不整合型铀矿电磁法深部探索报告[R].核工业西南地勘局二O九大队,1994。
[54]云南省江川县306铀矿点储量估算报告[R].云南省第三地质队,1961。
[55]云南省江川县三O七地区工作总结[R].中南二O九队五队八连二排,1970。
[56]云南省江川县三O六,三O七,三五七,一O一地区外围普查工作小结[R].中南二O九队五队八连一排,1970。
[57]云南省区域地质志[M].地质出版社,1990年。
[58]张书成,白云生,吴慧山.2006.康滇地轴南段不整合面型铀成矿基本条件的物化探研究[J].China Academic Journal Electronic Publishing House,1～12。
[59]张金带,徐高中,陈安平,等.2005.中国可地浸砂岩型铀矿成矿模式初步探讨[J],铀矿地质,21(3):139～145。
[60]张金带,李友良,简晓飞,等.2007.“十五”期间铀矿地质勘查主要成果及“十一五”的总体思路[J].铀矿地质,23(1):1～6。
[61]仉宝聚.2001.铀矿大型矿集区与成矿作用[J].铀矿地质,2001(1):5～17。
[62]赵凤民.1992.碱交代型铀矿床和加拿大不整合脉型铀矿床地质特征和找矿标志[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,44～46。
[63]赵凤民编著.俄罗斯铀矿地质[C],核工业北京地质研究院,2006。
[64]周维勋.元古宙不整合型铀矿及其寻找[M].康滇地轴铀矿远景评价研讨会论文摘要汇编,13～16。
[65] Adams S.S.and Smith R.B..1981.Geology and recognition criteriafor sandstone uranium deposits in mixed fluvial shallow marine sedimentary sequences,South Texas—final report:U.S.Department of Energy , Grand Junction Office , Colorado , Bendix Field Engineering Corporation,GJBX-4(81),p.146.
[66] Adler H.H.and Sharp B.J..1967.Uranium ore rolls-occurrence,genesis,and physical and chemical characteristics[M],in Uranium districts of southeastern Utah: Utah Geological Society Guidebook to Geology of Utah Vol.21:53～77.
[67] Davis J.F..1979.Uranium in the U.S.A.:Genesis and Exploration Implications.Philosophical Transactions of the Royal Society of London.Series A,Mathematical and Physical Sciences,Vol.291(1381):301～306.
[68] Dickinson K. A. and J.S. Duval..1977.South Texas Uranium:Geologic Controls , Exploration Techniques,and Potential,Chapter 2:Trend Areas and Exploration Techniques Utilization in Geology of Alternate Energy Resources in the South-Central United States (M.D.Campbell(ed)),Houston Geological Society,pp.45～66.
[69] Goldhaber M.B. , Reynolds R.L , Rye R..1978.Otigin of a South Texas roll-type uranium deposits: II.Petrology and sulfur isotope studies.Econmic Geology,73(8):1690～1705.
[70] Grange H.C.,Santos.E.S.,Dean.B.G. et al..1961.Sandstone-type uranium deposits at Ambrosia Lake,New Mexico;an interim report.Economic Geology,Vol.56(7):1179～1210.
[71] Harshman E.N.1972.Geology and uranium deposits,Shirley Basin area,Wyoming:U.S. Geological Survey Professional Paper 745,p.82.
[72] Harshman E.N. and Adams S.S..1980.Geology and recognition criteria for roll-type uranium deposits in continental sandstones Final report:U.S.Department of Energy,Grand Junction,Colorado,GJBX-1(81),p.181.
[73] Harshman E .N.,Adams S.S..1981. Geology and Recognition Criteria for Roll-Type Uranium Deposits in Continental Sandstones.Colorado:US Department of Energy,Grand Junction Office,p.185.
[74] Holen H.K. et al..1986.Geological characterization of New Mexico uranium deposits for extraction by In Situ Leach recovery, New Mexico Bureau of Mines and Mineral Resources, Open File Report No.251.
[75] Lambert I et al.,Australia′s Uranium Endoment:Metallogeny,Exploration and Potential,Proceedings of a Technical Committee Meeting《International Symposium Uranium Producti-on and Raw Materials for the Nuclear Fuel Cycle Supply and Demand,Economics,the Envir-onmental and Energy Security》Vienna,2005
[76] OECD(NEA)/IAEA Uranium Resources,Production and Demand,OECD,Paris:1993,1995,1997,1999,2001,2003.
[77] Pollock GD,McArthur River Project,Saskatchewan,Canada,Proceedings of a Technical Committee Meeting《Assessment of Uranium Deposit Types and Resources a worldwide Perspective》IAEA,Vienna,2001.
[78] Roy C et al.,Millennium Deposit - Basementhosted Derivative of the Unconformity Model,Proceedings of a Technical Committee Meeting《International Symposium》Vienna,2005.
[79] Sibbald Tll,Geolgy and genesis of the Althabasca basin uranium deposits,Proceediugs of a T-Echnical Committee Meeting《Recognition of Uranium Provinces》,London,1988.
© 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 |