楚雄盆地砂岩型铜矿床地质地球化学及找矿预测研究
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摘要
博士论文《楚雄盆地砂岩型铜矿床地质地球化学及找矿预测研究一以六苴、郝家河矿床为例》,依托全国危机矿山接替资源项目“云南省大姚县六苴铜矿小河-石门坎矿段接替资源勘查”(项目编号：200453001)与“云南省牟定县郝家河铜矿接替资源勘查”(项目编号：200653098)选题。
以六苴、郝家河床为研究对象,在矿床地质特征研究基础上,总结了矿区构造演化及控矿规律。对比了不同矿床、不同层位、含矿层不同位置元素地球化学特征,利用流体包裹体及同位素地球化学资料研究成矿流体的性质。结合电子探针分析结果,讨论含矿层浅、紫色砂岩的形成、金属矿物及元素分带机理,借鉴砂岩型铀矿床研究成果,提出“紫化聚铜”成矿模式。采用钻孔地球化学方法建立地球化学异常模式,结合地表地球化学勘查及地质综合分析,对研究区铜矿床深部及外围进行找矿预测,取得良好找矿效果。
1、阐述了“牟定斜坡”与楚雄盆地弧形砂岩铜矿带的空间关系。认为“牟定斜坡”沉积环境有利于铜质预富集。其构造作用控制砂岩型铜矿床的形成。
2、详细厘定了矿区出露地层的划分标志及依据。含矿层(K2ml1、K2mx2)以浅色砂岩为主,顶、底均以灰紫色含砾中-粗粒砂岩为其特征标志。
3、总结了构造演化及控矿规律。早期近东西向挤压形成的近南北向压扭性构造促进了铜的活化、迁移。晚期的构造活动改造,使铜矿体加富。后期近东西向压扭性断裂破坏矿体,将其向全浅带一侧错动。
4、矿床地球化学分析认为,含矿层砂岩经历了两种流(气)体活动过程：①还原性气(液)作用下砂岩褪色(砂岩由紫变浅)；②从紫色砂岩一侧进入的含氧层间流体。矿床形成于中低温环境,成矿流体具低盐度,以大气降水为主。成矿流体运移方向为从紫色砂岩一侧进入,向浅色砂岩一侧运移。提出“紫化聚铜”成矿模式。
5、采用钻孔地球化学方法建立地球化学异常模式,结合地表地球化学勘查及地质综合分析,圈定郝家河A、B、C三区,郝家河-老虎硐铜矿带,六苴石门坎NW侧,簸箕背斜、大雪山背斜倾没端等找矿预测区,部分已得到工程验证。
This doctoral dissertation, Studying on the Geology and Geochemistry, and the Prospecting Prognosis for the Sandstone Copper Deposit, in the Chuxiong Basin—Taking Liuju and Haojiahe Copper Deposit As the Case, is based on the Project of Superseding Resources Exploration for the State Crisis Mine—"Superseding Resources Exploration to the Xiaohe-Shimenkan Ore-body in Liuju Copper Deposit, Daoyao,Yunnan Province(NO.200453001)" and "Superseding Resources Exploration to the Haojiahe Copper Deposit, Mouding,Yunnan Province(NO.200653098)". Study on the geology and geochemistry, and the prospecting prognosis has guiding significance for metallogenic mechanism of sandstone copper deposit and exploration of copper resources in the Chuxiong Basin.
Take the Liuju and Haojiahe copper deposits as study objects; based on the geological features of deposit, it summarized the tectonic evolution and ore-controlling regularity in study area. Element geochemistry characteristics in different deposits and different color rocks were contrasted. The data of fluid inclusion and isotope geochemistry was used for the study of ore-forming fluid. On the basis of the electron probe analysis and sandstone-type uranium deposit research results, this paper discussed the formation of mauve sandstone and grayish sandstone, and the mechanism of mineral and element zonation. It builted the metallogenic model of the deposit, that is "copper aggregation during sandstone mauve alteration".
By adopting geochemical sections method from drill holes, it established the geochemical anomaly model. Combination with surface geochemical exploration and the synthetical geology analysis, it gained a good effect on prospecting prognosis in the deep and periphery.
1. It expounded the spatial relationship between the "Mouding Slope" and Arcuate Sandstone Copper Belt in Chuxiong Basin. The sedimentary environment of "Mouding Slope" was favorable to copper preconcentrtion. The tectonism controlled the formation of sandstone copper deposit.
2. It defined the exposure strata in detailed, and put forward the dividing indexes. Grayish sandstone was the main version in ore-bearing strata (K2m11、K2mx2), which is mauve pebbled and medium to coarse grained sandstones at the top and the bottom.
3. It summarized the tectonic evolution and ore-controlling regularity. The Nearly North-South compresso-shearing structures lead to copper activation and transport, and ore bodies reenrichment by late tectonic reworking. The Nearly East-West compresso-shearing faults formed in the last stage pushed ore-bodies to the grayish bed.
4. Analyzed of ore deposit geochemistry show that ore-bearing strata had experienced two processes fluid flow:①.Fading sandstone formed by reductive fluid (from mauve to grayish);②. Interlayer oxidative fluid came from the mauve direction. The sandstone copper deposit was formed in mid-low-temperature environmental, and ore-forming fluid derived from meteoric water, with low salinity. Ore-bearing hydrothermal solution came from the mauve direction and toward to the grayish direction. It builted the metallogenic model of the deposit, that is "copper aggregation during sandstone mauve alteration"
5. By adopting geochemical sections method from drill holes, it established the geochemical anomaly model. Combination with surface geochemical exploration and the synthetical geology analysis, it enclosed prospecting areas, such as Haojiahe A, B, C block; Haojiahe-Laohudong belt; northwest side of Shimenkan; pitching end of Boji and Daxueshan anticline, which had taken good effect by field examination.
以六苴、郝家河床为研究对象,在矿床地质特征研究基础上,总结了矿区构造演化及控矿规律。对比了不同矿床、不同层位、含矿层不同位置元素地球化学特征,利用流体包裹体及同位素地球化学资料研究成矿流体的性质。结合电子探针分析结果,讨论含矿层浅、紫色砂岩的形成、金属矿物及元素分带机理,借鉴砂岩型铀矿床研究成果,提出“紫化聚铜”成矿模式。采用钻孔地球化学方法建立地球化学异常模式,结合地表地球化学勘查及地质综合分析,对研究区铜矿床深部及外围进行找矿预测,取得良好找矿效果。
1、阐述了“牟定斜坡”与楚雄盆地弧形砂岩铜矿带的空间关系。认为“牟定斜坡”沉积环境有利于铜质预富集。其构造作用控制砂岩型铜矿床的形成。
2、详细厘定了矿区出露地层的划分标志及依据。含矿层(K2ml1、K2mx2)以浅色砂岩为主,顶、底均以灰紫色含砾中-粗粒砂岩为其特征标志。
3、总结了构造演化及控矿规律。早期近东西向挤压形成的近南北向压扭性构造促进了铜的活化、迁移。晚期的构造活动改造,使铜矿体加富。后期近东西向压扭性断裂破坏矿体,将其向全浅带一侧错动。
4、矿床地球化学分析认为,含矿层砂岩经历了两种流(气)体活动过程：①还原性气(液)作用下砂岩褪色(砂岩由紫变浅)；②从紫色砂岩一侧进入的含氧层间流体。矿床形成于中低温环境,成矿流体具低盐度,以大气降水为主。成矿流体运移方向为从紫色砂岩一侧进入,向浅色砂岩一侧运移。提出“紫化聚铜”成矿模式。
5、采用钻孔地球化学方法建立地球化学异常模式,结合地表地球化学勘查及地质综合分析,圈定郝家河A、B、C三区,郝家河-老虎硐铜矿带,六苴石门坎NW侧,簸箕背斜、大雪山背斜倾没端等找矿预测区,部分已得到工程验证。
This doctoral dissertation, Studying on the Geology and Geochemistry, and the Prospecting Prognosis for the Sandstone Copper Deposit, in the Chuxiong Basin—Taking Liuju and Haojiahe Copper Deposit As the Case, is based on the Project of Superseding Resources Exploration for the State Crisis Mine—"Superseding Resources Exploration to the Xiaohe-Shimenkan Ore-body in Liuju Copper Deposit, Daoyao,Yunnan Province(NO.200453001)" and "Superseding Resources Exploration to the Haojiahe Copper Deposit, Mouding,Yunnan Province(NO.200653098)". Study on the geology and geochemistry, and the prospecting prognosis has guiding significance for metallogenic mechanism of sandstone copper deposit and exploration of copper resources in the Chuxiong Basin.
Take the Liuju and Haojiahe copper deposits as study objects; based on the geological features of deposit, it summarized the tectonic evolution and ore-controlling regularity in study area. Element geochemistry characteristics in different deposits and different color rocks were contrasted. The data of fluid inclusion and isotope geochemistry was used for the study of ore-forming fluid. On the basis of the electron probe analysis and sandstone-type uranium deposit research results, this paper discussed the formation of mauve sandstone and grayish sandstone, and the mechanism of mineral and element zonation. It builted the metallogenic model of the deposit, that is "copper aggregation during sandstone mauve alteration".
By adopting geochemical sections method from drill holes, it established the geochemical anomaly model. Combination with surface geochemical exploration and the synthetical geology analysis, it gained a good effect on prospecting prognosis in the deep and periphery.
1. It expounded the spatial relationship between the "Mouding Slope" and Arcuate Sandstone Copper Belt in Chuxiong Basin. The sedimentary environment of "Mouding Slope" was favorable to copper preconcentrtion. The tectonism controlled the formation of sandstone copper deposit.
2. It defined the exposure strata in detailed, and put forward the dividing indexes. Grayish sandstone was the main version in ore-bearing strata (K2m11、K2mx2), which is mauve pebbled and medium to coarse grained sandstones at the top and the bottom.
3. It summarized the tectonic evolution and ore-controlling regularity. The Nearly North-South compresso-shearing structures lead to copper activation and transport, and ore bodies reenrichment by late tectonic reworking. The Nearly East-West compresso-shearing faults formed in the last stage pushed ore-bodies to the grayish bed.
4. Analyzed of ore deposit geochemistry show that ore-bearing strata had experienced two processes fluid flow:①.Fading sandstone formed by reductive fluid (from mauve to grayish);②. Interlayer oxidative fluid came from the mauve direction. The sandstone copper deposit was formed in mid-low-temperature environmental, and ore-forming fluid derived from meteoric water, with low salinity. Ore-bearing hydrothermal solution came from the mauve direction and toward to the grayish direction. It builted the metallogenic model of the deposit, that is "copper aggregation during sandstone mauve alteration"
5. By adopting geochemical sections method from drill holes, it established the geochemical anomaly model. Combination with surface geochemical exploration and the synthetical geology analysis, it enclosed prospecting areas, such as Haojiahe A, B, C block; Haojiahe-Laohudong belt; northwest side of Shimenkan; pitching end of Boji and Daxueshan anticline, which had taken good effect by field examination.
引文
[1]地质科学研究院情报所,国外砂页岩型铜矿.1975.9：1-2.
[2]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版社,1998：19.
[3]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[4]Laux JH, Lindenmayer ZG, Teixeira JBG, Neto AB.Ore genesis at the Camaqua copper mine, aneoproterozoic sediment-hosted deposit in Southern Brazil.ORE GEOLOGY REVIEWS,2005,26(1): 71-89.
[5]Durieux, C. Gustavo. Geological context, mineralization, and timing of the Juramento sediment-hosted stratiform copper-silver deposit, Salta district, northwestern Argentina. MINERALIUM DEPOSITA, 2007,42(8):879-899.
[6]El Desouky. The sandstone-hosted stratiform copper mineralization at Mwitapile and its relation to the mineralization at Lufukwe, Lufilian foreland, Democratic Republic of Congo. ORE GEOLOGY REVIEWS,2008,34(4):561-579.
[7]El Desouky, Hamdy A. Postorogenic origin of the stratiform Cu mineralization at Lufukwe, Lufilian foreland, Democratic Republic of Congo. ECONOMIC GEOLOGY,2008,103(3):555-582.
[8]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：270-276.
[9]冉崇英,张智筠,刘卫华等,康滇裂谷旋回与铜矿层楼结构及其地球化学演化.中国科学B辑,1994,24(3)：325-330.
[10]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：10-16.
[11]庄汉平,冉崇英,何明勤,卢家烂,滇中砂岩铜矿成矿过程中水-岩反应的证据与机理.地球科学-中国地质大学学报,1996,21(3)：327-331.
[12]李峰,甫为民,滇西红层铜矿地质.云南大学出版社,2000.8.
[13]王大鹏,张乾,朱笑青,张正伟,中国自然铜矿化类型、特点及形成类型浅析.矿物学报,2007,27(1)：57-63.
[14]秦德先,马宏,滇中郝家河砂岩铜矿的地球化学及其成因意义.地质论评,1994,40(2)：181-191.
[15]芮宗瑶,论某些层控铜矿交代分带.地质学报,1979,4：337-349.
[16]徐一仁,张素华,论砂岩铜矿的成因机制及其在找矿中的指导作用.有色金属矿产与地质,1993,(1)：6-13.
[17]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[18]金儒丹,黔北侏罗纪砂岩铜矿成因初探.贵州地质,1990,24(3)：237-242.
[19]陈根文,夏斌,吴延之等,沉积岩对楚雄盆地砂岩铜矿成矿的控制.矿物岩石,2002,22(3)：24-28.
[20]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[21]Wu Peng, Han Runsheng.3D geochemical anomalous model in the Liuju sandstone-type copper deposit, Yunnan, China. GEOCHIMICA ET COSMOCHIMICA ACTA,2008,72(12):A1039-A1039.
[22]Chen Wengen, Xia Bin.Diagenetic origin of the Luzhou copper deposit, Yunnan Province, China. Mineral Deposit Research:Meeting the Global Challenge,2005(1),91-92.
[23]Chen GW, Xia B, Wu YZ, Tu GZ, Yu HX. The metallogenic mechanism of the sandstone-type copper deposits in the Chuxiong Basin, Yunnan Province. SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2000,43:262-272.
[24]Schwab F L. Framework mineralogy and chemical composition of continental margin -types and stone. Geology,1975,3:487-490.
[25]Dickinson W.R, Suczek C.A. Platetectonics and sandstone compositions. AAPG Bull,1979,63(12):2164-2182.
[26]Valloni R, Maynard J B. Detrital modes of recent deep-sea sands and their relation to tectonic setting:a first approximation. Sedimentology,1981,28:75-83.
[27]Bhatia M R. Rare earth element geochemistry of Australian Paleozoic greywackes and mudracks: provenance and tectonic control. Sedimentary Geology,1985,45:97-113.
[28]Roser B P. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K,O/NaO2 ratio. Geology,1986.94:635-650.
[29]Roser B P, R J Korsch. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data. Chem.Geol,198867:119-139.
[30]Pettijohn F J, Potter P E, Siever R. Sand and sandstone. Berlin,1972,1-62.
[31]Y.Bartura, U.Wurzburger. Gisements stratiformes et provincese cuprifres.1974:277-285.
[32]K.H.Wedepohl.International Association of the Genesis of Ore Deposits, Papers Issue,1971(3):268-273.
[33]E.M.Bennett. English commonwealth mining and metallurgical congress. Geology of Australian Ore Deposits,1965:233-246.
[34]Lee A.Woodward, William H. Economic Geology,1974.69(1):108-120.
[35]Clark, A.L. Stratabound copper sulfides in the Precambrian Belt Super group, northern Idaho and north western Montana, U.S. A:Procedings of the IMA-IAGOD Meeting, The society of Mining Geologists of Japan special Issue,1971(3):261-267.
[36]Harrison, J.E. Precambrian Belt basin of northwestern United States:Its geometry, sedimentation, and copper occurrences. Geol.soc.America Bull.1972,83(5):1215-1240.
[37]Harrison, J.E. Copper mineralization in miogeosynclinal clastics et provinces crpriferes.1974.
[38]C.O.Ensign. Ore Deposits in the United States,1968:460-485.
[39]F.Mendelsohn. The Geology of the Northern Rhodesia Copper belt.1961.
[40]Crook K A W. Lithogenesis and geotectonics:the significance of compositional variations in flusch arenites (graywaches). Tulsa:SEPM Special Publication,1974,19:304-310.
[41]Bhatia M R. Plate tectonics and geochemical compostion of sandstones. Geology+1983,92:611-627.
[42]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[43]孟祥化,葛铭等,沉积盆地与沉积建造.北京：地质出版社,1993：106-125.
[44]徐一仁,张素华,论砂岩铜矿的矿物分带及其在找矿中的应用.有色金属矿产与勘查,1994,3(3)：135-140.
[45]庄汉平,冉崇英,卢家烂,铜、盐、有机质相互作用的实验研究.地球化学,1995,25(2)：191-199.
[46]秦德先,马宏,滇中郝家河砂岩铜矿的地球化学及其成因意义.地质论评,1994,40(2)：181-191.
[47]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序和造山作用.岩相古地理,1996,16(3)：47-57.
[48]谭凯旋,张哲儒,王忠刚,辉铜矿、黄铜矿和斑铜矿的溶解动力学Ⅰ.温度、pH和NaCl浓度的影响.矿物学报,1997,17(1)：38-44.
[49]尹福光,蒲心纯,朱同兴,楚雄复式盆地演化及形成的动力学机制.岩相古地理,1997,17(3)：22-35.
[50]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录-以楚雄前陆盆地分析为例.岩相古地理,1999,19(3)：1-15.
[51]许效松,尹福光,万方等,楚雄盆地性质与沉积层序演化.岩相古地理,1999,19(5)：1-11.
[52]陈根文,吴延之,楚雄弧后前陆盆地的形成与演化.云南地质,1999,18(4)：392-397.
[53]谭富文,尹福光,许效松等,楚雄前陆盆地系统的构造单元及沉积标识.沉积学报,2000,18(4)：573-610.
[54]谭富文,尹福光,许效松等,楚雄前陆盆地的构造特征与沉积演化.大地构造与成矿学,2004,8：345-352.
[55]方维萱,胡瑞忠,谢桂青等,云南哀牢山地区构造岩石地层单元及其构造演化.大地构造矿学,2002,3：28-36.
[56]张志斌,曹德斌,滇中楚雄中生代盆地的形成、演化及其与哀牢山造山带的关系-以楚雄西舍路至禄丰碧城镇区域地质综合剖面为例.地球学报,2002,23(2)：129-134.
[57]尹福光,万方,许效松等,楚雄盆地晚三叠世古地理变迁.沉积与特提斯地质,2004,9：52-57.
[58]王国力,蔡立国,汪集旸等,楚雄盆地构造-热演化与古地温场研究.石油实验地质,2005,27.(1)：28-38.
[59]李儒峰,马永生,郭彤楼等,云南楚雄盆地上三叠统沉积及地球化学的海相特征.地质学报,2006,80(3)：374-381.
[60]中国矿床发现史-云南卷编委会,中国矿床发现史-云南卷.北京：地质出版社,1996：7.
[61]黄崇轲,白冶,朱裕生等,中国铜矿床(下册).北京：地质出版社,2001.
[62]云南省冶金局勘探公司309队,普查勘探大姚中部含铜砂岩的几点体会.云南含铜砂岩现场会议特辑.地质出版社,1959.
[63]雷文礼,初论云南某砂岩型铜矿的成因.1966.
[64]地质科学研究院地质矿产所,铁铜矿产专辑第三集.北京：地质出版社,1975,2.
[65]成冶,我国某地区砂岩铜矿床的成因及控矿因素的初步探讨.地质学报1975,38(1)：28-44.
[66]云南省冶金局地质勘探公司304队,大姚铜矿区六苴矿床补充勘探报告.1974：9.
[67]云南省冶金局地质勘探公司,成都地质学院砂岩铜矿专题队,大姚砂岩铜矿岩相及成矿特点的认识(内部刊物).1974.
[68]云南省冶金局地质勘探公司304队,大姚砂岩铜矿基本特征和矿床成因.1975.
[69]李雷,对滇中砂岩铜矿的再认识.地质与勘探,1988.
[70]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[71]曹迪夫,康滇地轴及其西缘(楚雄盆地)砂岩铜矿远景调查报告.1995.
[72]张可清,熊鹏飞,滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报,1995,20(2).
[73]昆明理工大学,大姚铜矿地质研究报告.2004.
[1]刘肇昌,李凡友,钟康惠等,扬子地台西缘构造演化与成矿.成都：电子科技大学出版社,1996：1-251.
[2]刘家铎,张成江,刘显凡等,扬子地台西南缘成矿规律及找矿方向.北京：地质出版社,2004.
[3]郭学兵,大姚矿区外围资源地质评价.云南省有色金属学会第四次会员代表大会论文集,2003：29.
[4]李国玉,吕鸣岗,中国含油气盆地图集.北京：石油工业出版社,2002.12：168-170.
[5]杨世瑜,王瑞雪,矿床遥感地质问题.昆明：云南大学出版社,2003：192-193.
[6]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录-以楚雄前陆盆地分析为例.岩相古地理,1999,19(3)：1-15
[7]许效松,中国西部大型盆地分析及地球动力学.北京：地质出版社,1997,12.
[8]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序和造山作用.岩相古地理,1996,16(3)：47-57.
[9]朱同兴,黄志英,尹福光,楚雄中生代前陆盆地的构造沉降史研究.沉积与特提斯地质,2000,20(4)：20-30.
[10]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[11]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[12]潘杏南,赵济湘,张选阳,康滇构造与裂谷作用.重庆：重庆出版社,1987：35-134.
[13]陈国达,彭省临,戴塔根等,云南铜-多金属壳体大地构造成矿学.长沙：中南大学出版社,2004：186-187.
[14]陈根文,夏斌,吴延之,楚雄盆地砂岩铜矿成矿机理研究.中国科学(D辑),2000,30：169-175.
[15]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：62-64.
[16]《地球科学大辞典》编辑委员会,地球科学大辞典(应用学科卷).北京：地质出版社,2005,11：194.
[17]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：262.
[18]史清琴,云南大、中型铜矿床成矿条件分布规律、找矿方向及建议.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：21-23.
[19]徐绍文,楚雄盆地砂岩铜矿的成矿机制和找矿方向.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：38.
[20]刘和甫,李晓清,刘立群,伸展构造与裂谷盆地成藏区带.石油与天然气地质,2005,25(5)：537-552.
[21]王祖关,云南岩相古地理图集.云南省地质矿产局,1991：169-179.
[22]云南大姚铜矿,西南有色地质楚雄勘查院,云南省大姚县六苴铜矿区地形地质图.2002.
[23]黄崇轲,白冶,朱裕生等,中国铜矿床(下册).北京：地质出版社,2001：588-599.
[24]云南省冶金局地质勘探公司304队,大姚铜矿区六苴矿床补充勘探报告.1974,9.
[25]云南省有色局地质勘探公司304队,大姚铜矿区六苴矿床地质勘探报告.1966,9.
[26]云南星焰有色金属股份有限公司,有色地质局楚雄勘查院,郝家河铜矿区地形地质图.2007.
[27]秦德先,马宏,滇中郝家河铜矿的地球化学及其成因意义.地质论评,1994,40(2)：183-192.
[28]秦德先,孟清,杨明初等,牟定郝家河铜矿床的沉积-改造成因.矿床地质,1993,12(2)：97-108.
[29]程相皋,滇中牟定矿区砂岩铜矿的赋存规律及找矿问题.西南矿产地质,1990,4(1)：26-29.
[30]秦德先,杨明初,牟定铜矿控矿因素及成矿预测.地质找矿论丛,1993,8(4)：49-61.
[31]普传杰,滇中郝家河铜矿矿石组构研究及在矿床成因上的意义.云南冶金,199(1)：29-31.
[32]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[1]陈国达,成矿构造研究法.北京：地质出版社,1985：59-195.
[2]霍裕生,林新多,矿田构造学.北京：地质出版社,1993：1-48.
[3]孙家骢,矿田地质力学导论(上册).昆明：昆明理工大学地质系,1986(内部油印稿).
[4]孙家骢,矿田地质力学方法.昆明工学院报,1988,13(3)：120-12.
[5]韩润生,陈进,李元,云南会泽铅锌矿床构造控矿规律及隐伏矿预测.矿物学报,2001,21(2)：665-669.
[6]韩润生,孙家骢,刘丛强,易门铜矿田一都厂地区断裂构造地球化学及隐伏矿定位预测.矿物学报,2003.
[7]韩润生,陈进,李元,云南会泽铅锌矿床构造控矿研究规律及其隐伏矿预测.矿物学报,2001,21(2)：265-269.
[8]韩润生,金世昌,刘丛强,铜厂矿田陈家坝地区断裂构造地球化学特征及定位预测.地质与勘探2000,36(5)：66-69.
[9]韩润生,刘丛强,马德云,易门式大型铜矿床构造成矿动力学模型.地质科学,2003,38(2)：200-213.
[10]韩润生,初论构造成矿动力学及其隐伏矿定位预测研究内容和方法.地质与勘探,2003,39(1)：5-9.
[11]韩润生,陕西铜厂矿田构造成矿动力学.昆明：云南科技出版社,2003：91-164.
[12]韩润生,陈进,黄智龙,构造成矿动力学及隐伏矿定位预测-以云南会泽超大型铅锌(银、锗)矿床为例.北京：科学出版社,2006：80-96.
[13]孙家骢,云南省主要构造体系的成生发展及某些矿产的分布规律.昆明工学院学报,1988,13(3)：88-111.
[14]谭凯旋,龚文君,李小明,地洼盆地砂岩铜矿床的构造-流体-成矿体系及演化.大地构造与成矿学,1999,23(1)：35-41.
[15]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[16]黄敦义,滇中六苴铜矿床原生矿段的构造研究.西南矿产地质,1992,3：50-58.
[17]刘迅,地质力学的方法与实践第五篇(上)：地质力学在矿产资源勘查中的应用.北京：地质出版社,1998.8：33-42.
[18]庄培仁,常志忠,断裂构造研究.北京：地震出版社,1996：169-200.
[19]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：259.
[20]张可清,熊鹏飞.滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报,1995,20(2)：199-202.
[21]陈根文,夏斌,王国强,楚雄盆地砂岩铜矿床构造控矿分析.大地构造与成矿学,2002,6：167-169.
[22]肖荣阁,云南中新生代盆地构造环境、沉积建造及成矿作用.西南矿产与地质,1990,4(4)：73-82.
[23]肖荣阁,陈卉,袁见齐,云南中新生代地质与矿产.北京：海洋出版社,1985：177-179.
[24]陈朝德,滇西思茅坳陷构造特征.青藏高原地质文集.北京：地质出版社,1983：12.
[25]普传杰,秦德先,牟定郝家河铜矿床的构造控矿特征.云南地质,1992,11(2)：162-168.
[26]孙家骢,云南省主要构造体系的成生发展及某些矿产的分布规律.昆明工学院学报,1988,13(3)：88—111.
[27]万玲,郭随平,刘德良,滇中楚雄盆地构造演化与油气关系.南京大学学报(自然科学),1998,34(3)：322-329.
[28]尹光福,蒲心纯,朱同兴,楚雄复式盆地演化及形成的动力学机制.岩相古地理,1997,17(3)：22-35.
[29]陈根文,吴延之,楚雄弧后前陆盆地的形成及演化.云南地质,1999,18(4)：392-397.
[30]吴健民,黄永平,黎功举,扬子地台西缘内带大型铜矿床的“叠加裂谷—多源—热水”成矿作用.矿产与地质,1996,10(1)：17-21.
[31]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录—以楚雄前陆盆地分析为例.岩相古地理,1999,13(3)：1-15.
[32]汪士昭,从遥感图象看楚雄盆地的断裂构造格局及油气勘探远景.石油勘探与开发,1991,3：25-38.
[33]刘贻军,孟祥化,葛铭,云南楚雄前陆盆地晚三叠世沉积建造及盆地演化.现代地质,1998,12(4)：576-581.
[34]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序与造山作用.岩相古地理,1996,16(3)：47-57.
[35]许效松,尹光福,万方等,楚雄盆地性质与沉积层序演化.岩相古地理,1999,19(5)：1-11.
[36]尹光福,许效松,万方等,楚雄前陆盆地逆冲带的油气潜力.岩相古地理,1999,19(6)：1-8.
[37]谭富文,尹福光,许效松等,楚雄前陆盆地的构造特征与沉积演化.大地构造与成矿学,2004,28(3)：345-352.
[38]张志斌,曹德斌,滇中楚雄中生代盆地的形成、演化及其与哀牢山造山带的关系—以楚雄西舍路至禄丰碧城镇.地球学报,2002,23(2)：129-134.
[39]尹福光,万方,许效松,楚雄盆地晚三叠世古地理变迁.沉积与特提斯地质,2004,24(3)：52-57.
[40]郭赤奇,楚雄盆地晚三叠世海相沉积展布特征.云南地质,1992,11(1)：21-23.
[41]林青,周明辉,魏志红,晚三叠世末期楚雄盆地云龙凹陷海相沉积的分子地球化学证据.石油勘探 与开发,2004,31(4)：29-31.
[42]Liu, F., Liu, J., Zhong, D., He, J., You, Q. The subducted slab of Yangtze continental block beneath the Tethyian orogen in western Yunnan. Chinese Science Bulletin.2000,45,466-472.
[43]Dennis V. Kent, G. Xu, K. Huang, W. Y. Zhang and Neil D. Opdyke. Paleomagnetism of upper Cretaceous rocks from South China. Earth and Planetary Science Letters, Volume 79, Issues 1-2, August 1986, 179-184.
[44]Kainian Huang and Neil D. Opdyke. Paleomagnetism of Cretaceous to lower Tertiary rocks from southwestern Sichuan:a revisit. Earth and Planetary Science Letters, Volume 112, Issues 1-4, August 1992, Pages 29-40.
[45]Ken Sato, Yuyan Liu, Zhicheng Zhu, Zhenyu Yang and Yo-ichiro Otofuji. Paleomagnetic study of middle Cretaceous rocks from Yunlong, western Yunnan, China:evidence of southward displacement of Indochina. Earth and Planetary Science Letters, Volume 165, Issue 1,15 January 1999, Pages 1-15.
[46]Shin'ya Yoshioka, Yu Yan Li, Ken Sato, Hiroo Inokuchi, Li Su, Haider Zaman, Yo-ichiro Otofuji,. Paleomagnetic evidence for post-Cretaceous internal deformation of the Chuan Dian Fragment in the Yangtze block:a consequence of indentation of India into Asia. Tectonophysics,2003:61-74.
[47]Kainian Huang and Neil D. Opdyke. Paleomagnetic results from Cretaceous and Jurassic rocks of South and Southwest Yunnan. Earth and Planetary Science Letters,1993:507-524.
[48]Shoubu Funahara, Nobukazu Nishiwaki, Masako Miki, Fumiyuki Murata, Yo-ichiro Otofuji and Yi Zhao Wang. Paleomagnetic study of Cretaceous rocks from the Yangtze block, central Yunnan, China. Earth and Planetary Sctence Letters,1992:77-91.
[49]Yo-ichiro Otofuji, Yuyan Liu, Masahiko Yokoyama, Masato Tamai, Jiyun Yin. Tectonic deformation of the southwestern part of the Yangtze craton inferred from pale magnetism. Earth and Planetary Science Letters,1998:47-60.
[50]Xiaofeng Wang, I. Metcalfeb, Ping Jian, Longqing He, Chuanshan Wang. The Jinshajiang-Ailaoshan Suture Zone, China:tectonostratigraphy, age and evolution. Journal of Asian Earth Sciences, 2000,675-690.
[51]Haest, Maarten. Structural control on the Dikulushi Cu-Ag deposit, Katanga, Democratic Republic of Congo. ECONOMIC GEOLOGY.2007,102(7) 1321-1333.
[52]Chambefort I, Moritz R. Late cretaceous structural control and alpine overprint of the high-sulfidation Cu-Au epithermal Chelopech deposit, Srednogorie belt, Bulgaria.MINERALIUM DEPOSITA.2006,41(3): 259-280.
[53]Dan-Ping Yan, Mei-Fu Zhou, Christina Yan Wang, Bin Xia. Structural and geochronological constraints on the tectonic evolution of the Dulong-Song Chay tectonic dome in Yunnan province, SW China. Journal of Asian Earth Sciences,2006,332-353.
[54]Khin Zaw, Stephen G. Peters, Paul Cromie, Clive Burrett, Zengqian Hou. Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews,2007,3-47.
[55]曹德斌,张志斌,楚雄盆地中—新生界构造变形特征.云南地质,2001,21(1)：50-59.
[56]吴根耀,马力,许效松,喜马拉雅运动对川滇交界区古地理重建的制约和楚雄盆地的改造.古地理学报,2001,3(2)：3-10.
[57]陈智梁,陈世瑜,扬子地块西缘地质构造演化.重庆：重庆出版社,1988：9-17.
[58]韩润生,邹海俊,吴鹏等,云南省大姚县六苴铜矿小河—石门坎矿段接替资源勘查—2007年工作总结报告[R].2007年11月.
[59]冉崇英,刘卫华,康滇地轴铜矿床地球化学与矿床层楼结构机理.北京：科学出版社,1993.
[60]黎功举,地壳演化与成矿作用：以川滇地洼系“四层楼”铜矿床系列为例.大地构造与成矿学,1991,15(4)：327-334.
[61]冉崇英,张智筠,庄汉平,楚雄盆地铜、膏盐、有机矿床组合地球化学.成都理工学院学报,1998,25(2)：241-245.
[62]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[63]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[1]中国科学院地球化学研究所,铁的地球化学.北京：科学出版社,1981：52-85.
[2]刘英俊,曹励明,李兆麟,元素地球化学.北京：科学出版社,1984：95-176.
[3]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：19-40.
[4]冯增昭,王英华,刘焕杰,中国沉积学.北京：石油工业出版社,1994：347-456.
[5]王中刚,于学元,赵振华,稀土元素地球化学.北京：科学出版社,1989,88-93,436.
[6]Bau M. Rare-earth mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium. Chem. Geol.,1991,93:219-230.
[7]Giuliani G, Chelletz A and Mechiche M. Behavior of REE during thermal metamorphism and hydrothermal infiltration associated with skarn-and-vein-type tungsten orebodies in Central Morocco. Chem. Geol., 1987,64:279-294.
[8]凌其聪,刘丛强,水-岩反应与稀土元素行为.矿物学报,2001,21(1)：107-114.
[9]Michard A and Albarede F. The REE content of some hydrothermal fluids. Chem. Geol.,1986,55:51-60.
[10]Oi T, Kikawada Honda T, Ossaka T and Kakihana H. Determination of the lanthanoids in a neutral hot spring water by neutron activation analysis. J. Radioanal. Nucl. Chem.,1990,140:365-377.
[11]Sanjuan B, Michard A and Michard G. Influence of the temperature of CO2- rich springs on their aluminium and rare-earth elements contents. Chem. Geol.,1988,68:57-67.
[12]McLennan W H. REE mobility at constant in inter-REE ratio in the alteration zone at the Phelps Dodge missive sulfide deposits, M atagami, Quebe.Mineral. Deposita,1988,23:231-238.
[13]Lottermoser B G. Rare-earth element behaviour associated with strata-bound scheelite mineralization(Broken Hilll, Australia.Chem. Geol.,1989a,78:119-134.
[14]Michard A, Beaucarire C and Michard G. Uranium and rare-earth elements in CO2- rich waters from Vals-Bains(France). Geochim. Cosmochim. Acta,1987,51:901-909.
[15]Wendlant R F and Harrison W J. Rare-earth partitioning between immiscible carbonate and silicate liquids and CO2 vapour, result and implications for the formation of light earth-enriched rocks. contrib. Mineral.,1979,69:409-419.
[16]Oreskes N and Einaudi T. Origin of rare earth elements-enriched hematite breccias at the Olympic Dam Cu-U-Au-Ag deposits, Roxby downs, South Australia. Econ. Geol.,1990.85:1-28.
[17]Dickin A P. Evidence for limited REE leaching from the Roffna Gneiss, Switzerland-a discussion of the paper by Vocke et al.. Contrib, Mineral. Petrol.,1988,99:273-275.
[18]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：58-64.
[19]卢涣章,范宏瑞,倪培等.流体包裹体.北京：科学出版社,2004.
[20]普传杰,秦德先,牟定铜矿的稳定同位素及流体包裹体研究.云南地质,1994,13(2)：166-176.
[21]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[22]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[23]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版社,1998：65-67.
[24]陈骏,王鹤年,地球化学.北京：科学出版社,2004：131.
[25]冉崇英,刘卫华,何明勤等,康滇地轴铜矿床地球化学与矿床层楼结构机理.北京：科学出版社,1993：1-71,106-133.
[26]陈根文,吴延之,夏斌等,楚雄盆地砂岩铜矿床同位素特征及矿床成因.大地构造与成矿学,2002,26(3)：279-284.
[27]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[28]何明勤,冉崇英,刘卫华等,大姚铜矿床有机质特征及其与成矿的关系.石油与天然气地质,1991,12(2)：195-206.
[29]陈岳龙,杨忠芳,赵志丹,同位素地质年代学与地球化学.北京：地质出版社.2005：275-276.
[30]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[31]张理刚,稳定同位素在地质科学中的应用.西安：陕西科学技术出版社,1985.
[32]陈好寿,冉崇英等,康滇地轴铜矿床同位素地球化学.北京：地质出版社,1992：1-86.
[1]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[2]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[3]冉崇英,康滇地轴层控铜矿床的成矿机理.北京：地质出版社.1989.
[4]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：10-16.
[5]徐一仁,张素华,论砂岩铜矿的成因机制及其在找矿中的指导作用.有色金属矿产与地质,1993,(1)：6-13.
[6]秦德先,牟定郝家河铜矿含矿浅色层及矿床成因.云南地质,1994,13(1)：49-56.
[7]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版补.1998:170-113
[8]沈定华,与峨眉山玄武岩有关的铜矿床的成矿机制剖析.四川地质学报,1993,13(1)：32-36.
[9]陈国达,彭省临,戴塔根,云南铜-多金属壳体大地构造成矿学.长沙：中南大学出版社,2004,10：186-210.
[10]徐绍文,楚雄盆地砂岩铜矿的成矿机制和找矿方向.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：38.
[11]张可清,熊鹏飞,滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报.1995.20(2)：199-202.
[12]涂光炽,中国层控矿床地球化学(第三卷).北京：科学出版社,1988：1-20.312-336.
[13]秦德先,孟清,杨明初等,牟定郝家河铜矿床的沉积-改造成因.矿床地质,1993.12(2)97-108.
[14]何明勤,冉崇英,刘卫华等,大姚铜矿床有机质特征及其与成矿的关系.石油与天然气地质,1991,12(2)：195-206.
[15]张位及,红铁尘-红层的染色剂与砂岩铜矿的成因.西南冶金地质勘探公司内部资料.
[16]刘立钧,王均灿,地洼活动与花岗岩型铀矿化.活化构造理论(地洼学说)的应用与发展-“地洼学说奖”历届获奖论文选集.中国科学院长沙大地构造研究所：地震出版社,北京,1999.
[17]马艳萍,刘池洋,吴柏林,砂岩漂白现象的形成及其启示(盆地多种能源矿产共存富集成藏(矿)研究进展).北京：科学出版社,2005：141-149.
[18]Moulton G F. Some features of red bed bleaching. American Association of Petroleum Geologists Bulletin,1922,10:304-311.
[19]Shebl M A, Redox reactions in hydrocarbon clastic reservoirs:Experiental validation of this mechanism for porosity enhancement. Chemical Geology,1996,132:103-117.
[20]Suradm R C, Redox reactions involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstone. AAPG Bulletin,1993,77:1509-1518.
[21]余达淦,吴仁贵,陈培荣,铀资源地质学教程.哈尔滨：哈尔滨工程大学出版社,2007,10：250-290.
[22]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：219-247.
[23]E.N.哈什曼,S.S.亚当斯,秦楚笛译,陆相砂岩卷型铀矿床地质学和识别判据.原子能出版社,1980：37-158
[24]Sandstone-type Uranium deposits in China:geology and exploration techniques. Atomic Energy Press,2002.
[25]Adler,H. Concepts of uranium ore formation in reducing environments in sandstones and other sediments, in Formation of uranium ore deposits:Athens, International Atomic Energy Agency,1974:141-168.
[26]Brunt,D.A. Uranium in Tertiary stream channels, Lake Frome area, South Australia:Proceedings, Australian Institute of Mining and Metallurgy,1978,266:79-90.
[27]Childers,M.O. Uranium geology of the Kaycee area, Johns on County, Wyoming,:Wyoming geological Association,22nd Field Conference Guidebook,1970:13-20.
[28]Carrol,A.R. Late Paleozoic tectonic amalgamation of northwestern China:Sedimentary record of the northern Tarim, northwestern Turpan, and southern junggar Basins, Geol. Soc. Am. Bull.1995:571-594.
[29]De Veslud, Christian Le Carlier,3D modeling of uranium-bearing solution-collapse breccias in Proterozoic sandstones (Athabasca Basin, Canada)-Metallogenic interpretations. COMPUTERS & GEOSCIENCES,2009,35(1):92-107
[30]Alexandre, Paul, Geochronology of unconformity-related uranium deposits in the Athabasca Basin, Saskatchewan, Canada and their integration in the evolution of the basin. MINERALIUM DEPOSITA,2009,44(1):41-59.
[31]Li Ziying, And superposition metallogenic model of the sandstone-type uranium deposit in the northeastern Ordos Basin, China. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2008,82(4):745-749.
[32]Srivastava. S. K. Occurrence of sandstone-type uranium mineralization in the Umthongkut area, Mahadek Basin, West Khasi Hills District, Meghalaya, India. CURRENT SCIENCE,2008,94(12):1573-1575.
[33]Yang, X. Y. Occurrence of uranium minerals from sandstone-type uranium deposits, Ordos Basin. GEOCHIMICA ET COSMOCHIMICA ACTA,2008,72(12):A1058
[34]Rajesh, H. M. Mapping Proterozoic unconformity-related uranium deposits in the Rockhole area, Northern Territory, Australia using landsat ETM. ORE GEOLOGY REVIEWS, 2008,33(3):382-396.
[35]Li ZiYing, Origin of gray-green sandstone in ore bed of sandstone type uranium deposit in north Ordos Basin. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:165-173.
[36]Wu BoLin, Basical characteristics of fluid geologic process of interlayer oxidation zone sandstone-type uranium deposit. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:185-194.
[37]Fan AiPing, Research on diagenesis of the sandstone-type uranium deposits in Dongsheng area, Ordos Basin. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:195-202.
[38]Liu, J. A study of forming processes and prospecting indicators of sandstone type uranium ore by uranium series isotopes. WATER-ROCK INTERACTION, VOLS 1 AND 2, PROCEEDINGS, 2007:755-758.
[39]郭召杰,陈正乐,舒良树等,中国西部中亚型造山带中新生代陆内造山过程与砂岩型铀矿成矿作用.北京：地质出版社,2006.
[40]郭华,李明,夏斌等,查干诺尔盆地构造演化及铀成矿条件分析.北京：地质出版社,2004.
[41]李学礼,孙占学,周文斌,古水热系统与铀成矿作用.北京：地质出版社,2000.
[42]姚振凯,郑大瑜,刘翔,多因复成铀矿床及其成矿演化.北京：地质出版社,1998.
[43]刘池洋,盆地多种能源矿产共存富集成藏(矿)研究进展.北京：科学出版社,2005.
[44]孙泽轩,姚毅锋,巴音宝力格隆起带中新生代盆地砂岩铀矿类型及区域预测判据.矿物岩石,2004,24(4)：43-48.
[45]孙泽轩,陈洪德,朱西养,滇西新生代盆地砂岩型铀矿勘查现状与找矿前景.四川地质学报,2006,26(1)：24-28.
[46]孙泽轩,陈洪德,吴英,滇西新生代盆地与砂岩型铀矿成矿.地质论评,2006,52(4)：494-500.
[47]孙泽轩,陈洪德,朱西养,滇西新生代盆山耦合与砂岩型铀矿找矿方向.铀矿地质,2007,23(5)：289-296.
[48]蔡煜琦,韩效忠,李胜祥,天山造山带内中新生代盆地构造演化与砂岩型铀矿成矿的关系-以伊犁盆地、吐哈盆地为例.矿物学报,2007：91-92.
[49]李卫红,天山造山带中新生代盆地改造与砂岩型铀矿成矿.西北铀矿地质,2004,30(2)：41-47.
[50]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录—以楚雄前陆盆地分析为例.岩相古地理.1999,19(3)：1-15.
[51]涂光炽,中国层控矿床地球化学(第三卷).北京：科学出版社,1988：255-297.
[52]田儒,对412矿床成矿条件及成因的一些认识.北京地质研究院,1980年报：193-304.
[53]田儒,我国中新生代陆相红层盆地铀矿床基本特征.北京轴矿地质研究所,1982年报： 21-25.
[54]刘武生,漆富成,谢佑新,塔里木盆地中新生代地质构造演化与砂岩型铀成矿作用关系探讨.世界核地质科学,2006,23(4)：187-193.
[55]龚斌利,李卫红,鄂尔多斯盆地直罗组和志丹群砂岩型铀矿形成条件及找矿方向.西北铀矿地质,2005,31(1)：7-11.
[56]唐相生,甘肃省酒泉一金塔地区砂岩型铀成矿条件浅析.华东铀矿地质,2005(1)：8-14.
[57]刘健,陈正乐,张红喜,准噶尔盆地西北部中新生代地层铀矿成矿能力探讨.地质力学学报,2003,9(3)：241-244.
[58]冉崇英,张智筠,刘卫华等,康滇裂谷旋回与铜矿层楼结构及其地球化学演化.中国科学B辑,1994,24(3)：325-330.
[59]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[60]赵宝光,陈友良,姚毅峰,滇西新生代盆地沉积特征及砂岩型铀矿成矿条件.铀矿地质,2003,19(6)：344-348.
[61]陈戴生,李胜祥,蔡煜琦,我国中、新生代盆地砂岩型铀矿沉积环境研究概述.沉积学报,2006,24(2)：223-228.
[62]陈戴生,李胜祥,蔡煜琦,我国中新生代盆地砂岩型铀矿研究现状及发展方向的探讨.沉积学报,2003,21(1)：113-116.
[63]陈根文,夏斌,吴延之,楚雄盆地砂岩铜矿成矿机理研究.中国科学(D辑),2002,30：169-175.
[64]陈正乐,李细根,宫红良,新疆库车黑英山地区晚新生代构造运动及其对砂岩型铀矿成矿的控制作用初析.中国地质,2006,33(3)：572-579.
[65]李宝新,徐建国,王冰,新疆伊犁盆地南缘新生代构造特征及其对砂岩型铀矿的控制作用.新疆地质,2008,26(3)：297-300.
[66]彭云彪,陈安平,焦养泉,鄂尔多斯盆地中北部中、新生代构造演化与大规模砂岩型铀成矿作用.矿物学报,2007：110-111.
[67]李建威,李先福,李紫金,湘赣边区中新生代走滑断裂系统及对热液铀成矿作用的控制.地质找矿论丛,2000,15(2)：166-173.
[68]陈小东,刘翔,邓国泉,湘桂地区中新生代走滑断裂系统对铀成矿的控制作用.大地构造与成矿学,2002,26(4)：345-353.
[69]陈祖伊,黄世杰.试述华东南中新生代不整合面型铀矿床.铀矿地质,1990,6(6)：349-358.
[70]涂汉江,铀、金地球化学研究中的Eh-pH相图简介.世界核地质科学,1990(4)：32-35.
[71]关广岳,金属矿床氧化带微生物地球化学.北京：科学出版社,1999,94-95.
[72]刘英俊,曹励明,李兆麟,元素地球化学.北京：科学出版社,1984,10：216-223,283-293.
[73]刘英俊,曹励明,元素地球化学导论.北京：地质出版社,1985.4,81-97,176-192.
[74]谢学锦,程志中,张立生,中国西南地区76种元素地球化学图集.北京：地质出版社,2008：73,121.
[75]魏继生,朱西养,陶晓风,四川盆地地浸砂岩型铀矿的区域成矿条件浅析.四川地质学报,2005,5(3)：135-139.
[76]刘建华,朱西养,王四利,四川盆地地质构造演化特征与可地浸砂岩型铀矿找矿前景.铀矿地质,2005,21(6)：321-330.
[77]朱觉人,巫声扬,冯佩莘,四川盆地北部中生代砂岩型铀矿床成因探讨.四川地质学报,1991,2(1),53-63.
[78]中国科学院地球化学研究所,铁的地球化学.北京：科学出版社,1981：52-85.
[79]谭凯旋,张哲儒,王忠刚,辉铜矿、黄铜矿和斑铜矿的溶解动力学Ⅰ.温度、pH和NaCl浓度的影响.矿物学报,1997,17(1)：38-44.
[80]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[81]黄敦义,滇中六苴铜矿床原生矿段的构造研究.西南矿产地质,1992,3：50-58.
[82]陈根文,吴延之,夏斌等,楚雄盆地砂岩铜矿床同位素特征及矿床成因.大地构造与成矿学,2002,26(3)：279-284.
[83]杨蔚华,刘友梅,滇中中生代层控铜矿床的地球化学.中国科学(B辑),1983,8：833-841.
[84]Agterberg F P, Geomathematics, Elvsevier Scientific Publishing Company. Ameteradm, London, New York,1974.
[85]梁祥济,水-岩相互作用和成矿物质来源.北京：学苑出版社,1995,12：129.
[86]Goldhaber M B,Mechanisms of sulfur incorporation and isotope fractionation during earsy diagenesis in sediments of the Gulf of California. Marine Chemistry,1980,9:95-143.
[87]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[88]刘存林,滇中含铜砂岩成矿规律及找矿方向.《铁铜矿产专辑》第七集.北京：地质出版社,1977.
[89]P.Ramdohr(德),谢宇平等译,金属矿物及其交生(中册).长春：长春地质学院图书馆,长春地质学院图书馆情报部,1986,10：7.
[90]戴塔根,龚铃兰,张起钻,应用地球化学.长沙：中南大学出版社,2005：257-258.
[91]Haynes.D.W, Stratiform copper deposits hosted by low-energy sediments:Nature of source rocks and composition of metal transporting water. Econ.Geol.1986,81:266-280.
[92]J.B.梅纳德,沉积矿床地球化学.北京：地质出版社,1986：13-49.
[93]陈俊,王鹤年,地球化学.北京：科学出版社2004：312-314.
[94]刘宝珺,沉积岩石学.北京：地质出版社,1980：60-66.
[1]刘英俊,邱德同,勘查地球化学.北京：科学出版社,1987.
[2]西南冶金地质勘探公司地研所情报室,国外地质资料(铜矿专辑).1982.
[3]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.
[4]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[5]欧阳宗圻,李惠,刘汉忠,典型有色金属矿床地球化学异常模式.科学出版社,1990.
[6]B.A.巴尔苏科夫,成矿理论的发展是应用地球化学继续进步的基本前提.国外地质科技,1983,No.4.
[7]B.C.波波夫,大型矿床的矿物-地球化学指示标志.地质科技动态,1986,No.2.
[8]M.C.拉斐洛维奇,金矿床某些元素的物理化学性质、地球化学组合和垂直地球化学分带.地质科技动态,1984,No.22.
[9]H.E.Hawkes and J.S.Webb:1962,Geochemistry in Mineral Exploration,Harper & Row.New York and Enanston.
[10]A.A.Levinson:1973,Introduction to Exploration Geochemistry. Applied Publishing Ltd.Colgary,Alberta,Canada.
[11]H.E.Hawkes and J.S.Webb:1979,Geochemistry in Mineral Exploration(Second edition).
[12]A.A.Levinson:1980,Introduction to Exploration Geochemistry(Second edition).
[13]F.R.Siegel:1974,Applied Geochemistry.
[14]I.L.Ellcott and W.K.Flelcher:1974,Geochemical Exploration.
[15]Doe, B.R. and Zartman,R.E.,1979,Plumbotectonic,the Phanerozoic,In: Geochemistry of Hydrothermal Ore Deposits,2nd edition. John Wolley & Sons, Inc.,pp.22-66.
[16]Boyle,R.W.,1977,Geochemistry overview,Paper Presented at "Exploration77".
[17]谢学锦,邵跃,地球化学岩石测量的工作方法与解释推断方法,物探化探研究报导,地质部物探研究所,1956,No.5.
[18]邵跃,白银厂地区的地球化学探矿.地球物理勘探,1956,No.9.
[19]邵跃,辽宁某铅-锌矿区原生晕的研究.地球物理勘探,1956,No.12.
[20]谢学锦,陈洪才,原生晕方法普查勘探中的作用.地质学报,1961,41.
[21]谢学锦,区域化探.地质出版社,1979.
[22]张本仁,《勘查地球物理勘查地球化学文集》第二集.地质出版社出版,1985.
[23]欧阳宗圻,李惠,刘汉忠,典型有色金属矿床地球化学异常模式.科学出版社,1990.
[24]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[25]邵跃,热液矿床岩石测量找矿.北京：地质出版社,1997.
[26]黄薰德,吴郁彦,地球化学找矿.北京：地质出版社,1986.
[27]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：257-259.
[28]周永章,Jayanta Guha, Edward H. Chown,卢焕章,元素迁移的分维结构、级序路径及共轭地球化学异常存在的理论依据.地球化学,1995,24(1)：69-75.
[29]戴塔根,龚铃兰,张起钻,应用地球化学.长沙：中南大学出版社,2005：257-258.
[30]刘英俊,邱德同,勘查地球化学.北京：科学出版社,1987：15-16.
[31]桂林冶金地质研究所,地球化学探矿分析方法.冶金出版社,1974.
[32]吴锡生,化探数据处理方法.北京：地质出版社,1992.
[33]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[34]闵茂中,白南静,地质测试样品采集及送测指南.北京：科学出版社,1990：1-8.
[35]张承亮,程德兰,地球化学样品分析.北京：地质出版社,1989.
[36]范永香,阳正熙,成矿规律与矿矿预测.徐州：中国矿业大学出版社,2003：251-266.
[37]胡惠民,大比例尺成矿预测方法.北京：地质出版社,1995.
[38]徐强,潘桂棠,王立全,主要类型铜矿床(体)快速定位预测.北京：地质出版社,2003：1-10.
[39]翟裕生,邓军,崔彬等,成矿系统及综合地质异常.现代地质,1999,13(2).
[40]翟裕生,邓军,王建平等,深部找矿研究问题.矿床地质,2004,23(2).
[41]谢学锦,程志中,张立生,中国西南地区76种元素地球化学图集.北京：地质出版社,2008：73.
[42]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：58-64.
[43]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[44]韩润生,邹海俊,吴鹏等,云南省大姚县六苴铜矿小河—石门坎矿段接替资源勘查—2007年工作总结报告[R].2007,11.
[2]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版社,1998：19.
[3]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[4]Laux JH, Lindenmayer ZG, Teixeira JBG, Neto AB.Ore genesis at the Camaqua copper mine, aneoproterozoic sediment-hosted deposit in Southern Brazil.ORE GEOLOGY REVIEWS,2005,26(1): 71-89.
[5]Durieux, C. Gustavo. Geological context, mineralization, and timing of the Juramento sediment-hosted stratiform copper-silver deposit, Salta district, northwestern Argentina. MINERALIUM DEPOSITA, 2007,42(8):879-899.
[6]El Desouky. The sandstone-hosted stratiform copper mineralization at Mwitapile and its relation to the mineralization at Lufukwe, Lufilian foreland, Democratic Republic of Congo. ORE GEOLOGY REVIEWS,2008,34(4):561-579.
[7]El Desouky, Hamdy A. Postorogenic origin of the stratiform Cu mineralization at Lufukwe, Lufilian foreland, Democratic Republic of Congo. ECONOMIC GEOLOGY,2008,103(3):555-582.
[8]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：270-276.
[9]冉崇英,张智筠,刘卫华等,康滇裂谷旋回与铜矿层楼结构及其地球化学演化.中国科学B辑,1994,24(3)：325-330.
[10]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：10-16.
[11]庄汉平,冉崇英,何明勤,卢家烂,滇中砂岩铜矿成矿过程中水-岩反应的证据与机理.地球科学-中国地质大学学报,1996,21(3)：327-331.
[12]李峰,甫为民,滇西红层铜矿地质.云南大学出版社,2000.8.
[13]王大鹏,张乾,朱笑青,张正伟,中国自然铜矿化类型、特点及形成类型浅析.矿物学报,2007,27(1)：57-63.
[14]秦德先,马宏,滇中郝家河砂岩铜矿的地球化学及其成因意义.地质论评,1994,40(2)：181-191.
[15]芮宗瑶,论某些层控铜矿交代分带.地质学报,1979,4：337-349.
[16]徐一仁,张素华,论砂岩铜矿的成因机制及其在找矿中的指导作用.有色金属矿产与地质,1993,(1)：6-13.
[17]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[18]金儒丹,黔北侏罗纪砂岩铜矿成因初探.贵州地质,1990,24(3)：237-242.
[19]陈根文,夏斌,吴延之等,沉积岩对楚雄盆地砂岩铜矿成矿的控制.矿物岩石,2002,22(3)：24-28.
[20]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[21]Wu Peng, Han Runsheng.3D geochemical anomalous model in the Liuju sandstone-type copper deposit, Yunnan, China. GEOCHIMICA ET COSMOCHIMICA ACTA,2008,72(12):A1039-A1039.
[22]Chen Wengen, Xia Bin.Diagenetic origin of the Luzhou copper deposit, Yunnan Province, China. Mineral Deposit Research:Meeting the Global Challenge,2005(1),91-92.
[23]Chen GW, Xia B, Wu YZ, Tu GZ, Yu HX. The metallogenic mechanism of the sandstone-type copper deposits in the Chuxiong Basin, Yunnan Province. SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2000,43:262-272.
[24]Schwab F L. Framework mineralogy and chemical composition of continental margin -types and stone. Geology,1975,3:487-490.
[25]Dickinson W.R, Suczek C.A. Platetectonics and sandstone compositions. AAPG Bull,1979,63(12):2164-2182.
[26]Valloni R, Maynard J B. Detrital modes of recent deep-sea sands and their relation to tectonic setting:a first approximation. Sedimentology,1981,28:75-83.
[27]Bhatia M R. Rare earth element geochemistry of Australian Paleozoic greywackes and mudracks: provenance and tectonic control. Sedimentary Geology,1985,45:97-113.
[28]Roser B P. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K,O/NaO2 ratio. Geology,1986.94:635-650.
[29]Roser B P, R J Korsch. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data. Chem.Geol,198867:119-139.
[30]Pettijohn F J, Potter P E, Siever R. Sand and sandstone. Berlin,1972,1-62.
[31]Y.Bartura, U.Wurzburger. Gisements stratiformes et provincese cuprifres.1974:277-285.
[32]K.H.Wedepohl.International Association of the Genesis of Ore Deposits, Papers Issue,1971(3):268-273.
[33]E.M.Bennett. English commonwealth mining and metallurgical congress. Geology of Australian Ore Deposits,1965:233-246.
[34]Lee A.Woodward, William H. Economic Geology,1974.69(1):108-120.
[35]Clark, A.L. Stratabound copper sulfides in the Precambrian Belt Super group, northern Idaho and north western Montana, U.S. A:Procedings of the IMA-IAGOD Meeting, The society of Mining Geologists of Japan special Issue,1971(3):261-267.
[36]Harrison, J.E. Precambrian Belt basin of northwestern United States:Its geometry, sedimentation, and copper occurrences. Geol.soc.America Bull.1972,83(5):1215-1240.
[37]Harrison, J.E. Copper mineralization in miogeosynclinal clastics et provinces crpriferes.1974.
[38]C.O.Ensign. Ore Deposits in the United States,1968:460-485.
[39]F.Mendelsohn. The Geology of the Northern Rhodesia Copper belt.1961.
[40]Crook K A W. Lithogenesis and geotectonics:the significance of compositional variations in flusch arenites (graywaches). Tulsa:SEPM Special Publication,1974,19:304-310.
[41]Bhatia M R. Plate tectonics and geochemical compostion of sandstones. Geology+1983,92:611-627.
[42]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[43]孟祥化,葛铭等,沉积盆地与沉积建造.北京：地质出版社,1993：106-125.
[44]徐一仁,张素华,论砂岩铜矿的矿物分带及其在找矿中的应用.有色金属矿产与勘查,1994,3(3)：135-140.
[45]庄汉平,冉崇英,卢家烂,铜、盐、有机质相互作用的实验研究.地球化学,1995,25(2)：191-199.
[46]秦德先,马宏,滇中郝家河砂岩铜矿的地球化学及其成因意义.地质论评,1994,40(2)：181-191.
[47]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序和造山作用.岩相古地理,1996,16(3)：47-57.
[48]谭凯旋,张哲儒,王忠刚,辉铜矿、黄铜矿和斑铜矿的溶解动力学Ⅰ.温度、pH和NaCl浓度的影响.矿物学报,1997,17(1)：38-44.
[49]尹福光,蒲心纯,朱同兴,楚雄复式盆地演化及形成的动力学机制.岩相古地理,1997,17(3)：22-35.
[50]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录-以楚雄前陆盆地分析为例.岩相古地理,1999,19(3)：1-15.
[51]许效松,尹福光,万方等,楚雄盆地性质与沉积层序演化.岩相古地理,1999,19(5)：1-11.
[52]陈根文,吴延之,楚雄弧后前陆盆地的形成与演化.云南地质,1999,18(4)：392-397.
[53]谭富文,尹福光,许效松等,楚雄前陆盆地系统的构造单元及沉积标识.沉积学报,2000,18(4)：573-610.
[54]谭富文,尹福光,许效松等,楚雄前陆盆地的构造特征与沉积演化.大地构造与成矿学,2004,8：345-352.
[55]方维萱,胡瑞忠,谢桂青等,云南哀牢山地区构造岩石地层单元及其构造演化.大地构造矿学,2002,3：28-36.
[56]张志斌,曹德斌,滇中楚雄中生代盆地的形成、演化及其与哀牢山造山带的关系-以楚雄西舍路至禄丰碧城镇区域地质综合剖面为例.地球学报,2002,23(2)：129-134.
[57]尹福光,万方,许效松等,楚雄盆地晚三叠世古地理变迁.沉积与特提斯地质,2004,9：52-57.
[58]王国力,蔡立国,汪集旸等,楚雄盆地构造-热演化与古地温场研究.石油实验地质,2005,27.(1)：28-38.
[59]李儒峰,马永生,郭彤楼等,云南楚雄盆地上三叠统沉积及地球化学的海相特征.地质学报,2006,80(3)：374-381.
[60]中国矿床发现史-云南卷编委会,中国矿床发现史-云南卷.北京：地质出版社,1996：7.
[61]黄崇轲,白冶,朱裕生等,中国铜矿床(下册).北京：地质出版社,2001.
[62]云南省冶金局勘探公司309队,普查勘探大姚中部含铜砂岩的几点体会.云南含铜砂岩现场会议特辑.地质出版社,1959.
[63]雷文礼,初论云南某砂岩型铜矿的成因.1966.
[64]地质科学研究院地质矿产所,铁铜矿产专辑第三集.北京：地质出版社,1975,2.
[65]成冶,我国某地区砂岩铜矿床的成因及控矿因素的初步探讨.地质学报1975,38(1)：28-44.
[66]云南省冶金局地质勘探公司304队,大姚铜矿区六苴矿床补充勘探报告.1974：9.
[67]云南省冶金局地质勘探公司,成都地质学院砂岩铜矿专题队,大姚砂岩铜矿岩相及成矿特点的认识(内部刊物).1974.
[68]云南省冶金局地质勘探公司304队,大姚砂岩铜矿基本特征和矿床成因.1975.
[69]李雷,对滇中砂岩铜矿的再认识.地质与勘探,1988.
[70]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[71]曹迪夫,康滇地轴及其西缘(楚雄盆地)砂岩铜矿远景调查报告.1995.
[72]张可清,熊鹏飞,滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报,1995,20(2).
[73]昆明理工大学,大姚铜矿地质研究报告.2004.
[1]刘肇昌,李凡友,钟康惠等,扬子地台西缘构造演化与成矿.成都：电子科技大学出版社,1996：1-251.
[2]刘家铎,张成江,刘显凡等,扬子地台西南缘成矿规律及找矿方向.北京：地质出版社,2004.
[3]郭学兵,大姚矿区外围资源地质评价.云南省有色金属学会第四次会员代表大会论文集,2003：29.
[4]李国玉,吕鸣岗,中国含油气盆地图集.北京：石油工业出版社,2002.12：168-170.
[5]杨世瑜,王瑞雪,矿床遥感地质问题.昆明：云南大学出版社,2003：192-193.
[6]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录-以楚雄前陆盆地分析为例.岩相古地理,1999,19(3)：1-15
[7]许效松,中国西部大型盆地分析及地球动力学.北京：地质出版社,1997,12.
[8]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序和造山作用.岩相古地理,1996,16(3)：47-57.
[9]朱同兴,黄志英,尹福光,楚雄中生代前陆盆地的构造沉降史研究.沉积与特提斯地质,2000,20(4)：20-30.
[10]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[11]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[12]潘杏南,赵济湘,张选阳,康滇构造与裂谷作用.重庆：重庆出版社,1987：35-134.
[13]陈国达,彭省临,戴塔根等,云南铜-多金属壳体大地构造成矿学.长沙：中南大学出版社,2004：186-187.
[14]陈根文,夏斌,吴延之,楚雄盆地砂岩铜矿成矿机理研究.中国科学(D辑),2000,30：169-175.
[15]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：62-64.
[16]《地球科学大辞典》编辑委员会,地球科学大辞典(应用学科卷).北京：地质出版社,2005,11：194.
[17]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：262.
[18]史清琴,云南大、中型铜矿床成矿条件分布规律、找矿方向及建议.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：21-23.
[19]徐绍文,楚雄盆地砂岩铜矿的成矿机制和找矿方向.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：38.
[20]刘和甫,李晓清,刘立群,伸展构造与裂谷盆地成藏区带.石油与天然气地质,2005,25(5)：537-552.
[21]王祖关,云南岩相古地理图集.云南省地质矿产局,1991：169-179.
[22]云南大姚铜矿,西南有色地质楚雄勘查院,云南省大姚县六苴铜矿区地形地质图.2002.
[23]黄崇轲,白冶,朱裕生等,中国铜矿床(下册).北京：地质出版社,2001：588-599.
[24]云南省冶金局地质勘探公司304队,大姚铜矿区六苴矿床补充勘探报告.1974,9.
[25]云南省有色局地质勘探公司304队,大姚铜矿区六苴矿床地质勘探报告.1966,9.
[26]云南星焰有色金属股份有限公司,有色地质局楚雄勘查院,郝家河铜矿区地形地质图.2007.
[27]秦德先,马宏,滇中郝家河铜矿的地球化学及其成因意义.地质论评,1994,40(2)：183-192.
[28]秦德先,孟清,杨明初等,牟定郝家河铜矿床的沉积-改造成因.矿床地质,1993,12(2)：97-108.
[29]程相皋,滇中牟定矿区砂岩铜矿的赋存规律及找矿问题.西南矿产地质,1990,4(1)：26-29.
[30]秦德先,杨明初,牟定铜矿控矿因素及成矿预测.地质找矿论丛,1993,8(4)：49-61.
[31]普传杰,滇中郝家河铜矿矿石组构研究及在矿床成因上的意义.云南冶金,199(1)：29-31.
[32]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[1]陈国达,成矿构造研究法.北京：地质出版社,1985：59-195.
[2]霍裕生,林新多,矿田构造学.北京：地质出版社,1993：1-48.
[3]孙家骢,矿田地质力学导论(上册).昆明：昆明理工大学地质系,1986(内部油印稿).
[4]孙家骢,矿田地质力学方法.昆明工学院报,1988,13(3)：120-12.
[5]韩润生,陈进,李元,云南会泽铅锌矿床构造控矿规律及隐伏矿预测.矿物学报,2001,21(2)：665-669.
[6]韩润生,孙家骢,刘丛强,易门铜矿田一都厂地区断裂构造地球化学及隐伏矿定位预测.矿物学报,2003.
[7]韩润生,陈进,李元,云南会泽铅锌矿床构造控矿研究规律及其隐伏矿预测.矿物学报,2001,21(2)：265-269.
[8]韩润生,金世昌,刘丛强,铜厂矿田陈家坝地区断裂构造地球化学特征及定位预测.地质与勘探2000,36(5)：66-69.
[9]韩润生,刘丛强,马德云,易门式大型铜矿床构造成矿动力学模型.地质科学,2003,38(2)：200-213.
[10]韩润生,初论构造成矿动力学及其隐伏矿定位预测研究内容和方法.地质与勘探,2003,39(1)：5-9.
[11]韩润生,陕西铜厂矿田构造成矿动力学.昆明：云南科技出版社,2003：91-164.
[12]韩润生,陈进,黄智龙,构造成矿动力学及隐伏矿定位预测-以云南会泽超大型铅锌(银、锗)矿床为例.北京：科学出版社,2006：80-96.
[13]孙家骢,云南省主要构造体系的成生发展及某些矿产的分布规律.昆明工学院学报,1988,13(3)：88-111.
[14]谭凯旋,龚文君,李小明,地洼盆地砂岩铜矿床的构造-流体-成矿体系及演化.大地构造与成矿学,1999,23(1)：35-41.
[15]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[16]黄敦义,滇中六苴铜矿床原生矿段的构造研究.西南矿产地质,1992,3：50-58.
[17]刘迅,地质力学的方法与实践第五篇(上)：地质力学在矿产资源勘查中的应用.北京：地质出版社,1998.8：33-42.
[18]庄培仁,常志忠,断裂构造研究.北京：地震出版社,1996：169-200.
[19]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：259.
[20]张可清,熊鹏飞.滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报,1995,20(2)：199-202.
[21]陈根文,夏斌,王国强,楚雄盆地砂岩铜矿床构造控矿分析.大地构造与成矿学,2002,6：167-169.
[22]肖荣阁,云南中新生代盆地构造环境、沉积建造及成矿作用.西南矿产与地质,1990,4(4)：73-82.
[23]肖荣阁,陈卉,袁见齐,云南中新生代地质与矿产.北京：海洋出版社,1985：177-179.
[24]陈朝德,滇西思茅坳陷构造特征.青藏高原地质文集.北京：地质出版社,1983：12.
[25]普传杰,秦德先,牟定郝家河铜矿床的构造控矿特征.云南地质,1992,11(2)：162-168.
[26]孙家骢,云南省主要构造体系的成生发展及某些矿产的分布规律.昆明工学院学报,1988,13(3)：88—111.
[27]万玲,郭随平,刘德良,滇中楚雄盆地构造演化与油气关系.南京大学学报(自然科学),1998,34(3)：322-329.
[28]尹光福,蒲心纯,朱同兴,楚雄复式盆地演化及形成的动力学机制.岩相古地理,1997,17(3)：22-35.
[29]陈根文,吴延之,楚雄弧后前陆盆地的形成及演化.云南地质,1999,18(4)：392-397.
[30]吴健民,黄永平,黎功举,扬子地台西缘内带大型铜矿床的“叠加裂谷—多源—热水”成矿作用.矿产与地质,1996,10(1)：17-21.
[31]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录—以楚雄前陆盆地分析为例.岩相古地理,1999,13(3)：1-15.
[32]汪士昭,从遥感图象看楚雄盆地的断裂构造格局及油气勘探远景.石油勘探与开发,1991,3：25-38.
[33]刘贻军,孟祥化,葛铭,云南楚雄前陆盆地晚三叠世沉积建造及盆地演化.现代地质,1998,12(4)：576-581.
[34]蒲心纯,尹福光,朱同兴,楚雄前陆盆地的充填层序与造山作用.岩相古地理,1996,16(3)：47-57.
[35]许效松,尹光福,万方等,楚雄盆地性质与沉积层序演化.岩相古地理,1999,19(5)：1-11.
[36]尹光福,许效松,万方等,楚雄前陆盆地逆冲带的油气潜力.岩相古地理,1999,19(6)：1-8.
[37]谭富文,尹福光,许效松等,楚雄前陆盆地的构造特征与沉积演化.大地构造与成矿学,2004,28(3)：345-352.
[38]张志斌,曹德斌,滇中楚雄中生代盆地的形成、演化及其与哀牢山造山带的关系—以楚雄西舍路至禄丰碧城镇.地球学报,2002,23(2)：129-134.
[39]尹福光,万方,许效松,楚雄盆地晚三叠世古地理变迁.沉积与特提斯地质,2004,24(3)：52-57.
[40]郭赤奇,楚雄盆地晚三叠世海相沉积展布特征.云南地质,1992,11(1)：21-23.
[41]林青,周明辉,魏志红,晚三叠世末期楚雄盆地云龙凹陷海相沉积的分子地球化学证据.石油勘探 与开发,2004,31(4)：29-31.
[42]Liu, F., Liu, J., Zhong, D., He, J., You, Q. The subducted slab of Yangtze continental block beneath the Tethyian orogen in western Yunnan. Chinese Science Bulletin.2000,45,466-472.
[43]Dennis V. Kent, G. Xu, K. Huang, W. Y. Zhang and Neil D. Opdyke. Paleomagnetism of upper Cretaceous rocks from South China. Earth and Planetary Science Letters, Volume 79, Issues 1-2, August 1986, 179-184.
[44]Kainian Huang and Neil D. Opdyke. Paleomagnetism of Cretaceous to lower Tertiary rocks from southwestern Sichuan:a revisit. Earth and Planetary Science Letters, Volume 112, Issues 1-4, August 1992, Pages 29-40.
[45]Ken Sato, Yuyan Liu, Zhicheng Zhu, Zhenyu Yang and Yo-ichiro Otofuji. Paleomagnetic study of middle Cretaceous rocks from Yunlong, western Yunnan, China:evidence of southward displacement of Indochina. Earth and Planetary Science Letters, Volume 165, Issue 1,15 January 1999, Pages 1-15.
[46]Shin'ya Yoshioka, Yu Yan Li, Ken Sato, Hiroo Inokuchi, Li Su, Haider Zaman, Yo-ichiro Otofuji,. Paleomagnetic evidence for post-Cretaceous internal deformation of the Chuan Dian Fragment in the Yangtze block:a consequence of indentation of India into Asia. Tectonophysics,2003:61-74.
[47]Kainian Huang and Neil D. Opdyke. Paleomagnetic results from Cretaceous and Jurassic rocks of South and Southwest Yunnan. Earth and Planetary Science Letters,1993:507-524.
[48]Shoubu Funahara, Nobukazu Nishiwaki, Masako Miki, Fumiyuki Murata, Yo-ichiro Otofuji and Yi Zhao Wang. Paleomagnetic study of Cretaceous rocks from the Yangtze block, central Yunnan, China. Earth and Planetary Sctence Letters,1992:77-91.
[49]Yo-ichiro Otofuji, Yuyan Liu, Masahiko Yokoyama, Masato Tamai, Jiyun Yin. Tectonic deformation of the southwestern part of the Yangtze craton inferred from pale magnetism. Earth and Planetary Science Letters,1998:47-60.
[50]Xiaofeng Wang, I. Metcalfeb, Ping Jian, Longqing He, Chuanshan Wang. The Jinshajiang-Ailaoshan Suture Zone, China:tectonostratigraphy, age and evolution. Journal of Asian Earth Sciences, 2000,675-690.
[51]Haest, Maarten. Structural control on the Dikulushi Cu-Ag deposit, Katanga, Democratic Republic of Congo. ECONOMIC GEOLOGY.2007,102(7) 1321-1333.
[52]Chambefort I, Moritz R. Late cretaceous structural control and alpine overprint of the high-sulfidation Cu-Au epithermal Chelopech deposit, Srednogorie belt, Bulgaria.MINERALIUM DEPOSITA.2006,41(3): 259-280.
[53]Dan-Ping Yan, Mei-Fu Zhou, Christina Yan Wang, Bin Xia. Structural and geochronological constraints on the tectonic evolution of the Dulong-Song Chay tectonic dome in Yunnan province, SW China. Journal of Asian Earth Sciences,2006,332-353.
[54]Khin Zaw, Stephen G. Peters, Paul Cromie, Clive Burrett, Zengqian Hou. Nature, diversity of deposit types and metallogenic relations of South China. Ore Geology Reviews,2007,3-47.
[55]曹德斌,张志斌,楚雄盆地中—新生界构造变形特征.云南地质,2001,21(1)：50-59.
[56]吴根耀,马力,许效松,喜马拉雅运动对川滇交界区古地理重建的制约和楚雄盆地的改造.古地理学报,2001,3(2)：3-10.
[57]陈智梁,陈世瑜,扬子地块西缘地质构造演化.重庆：重庆出版社,1988：9-17.
[58]韩润生,邹海俊,吴鹏等,云南省大姚县六苴铜矿小河—石门坎矿段接替资源勘查—2007年工作总结报告[R].2007年11月.
[59]冉崇英,刘卫华,康滇地轴铜矿床地球化学与矿床层楼结构机理.北京：科学出版社,1993.
[60]黎功举,地壳演化与成矿作用：以川滇地洼系“四层楼”铜矿床系列为例.大地构造与成矿学,1991,15(4)：327-334.
[61]冉崇英,张智筠,庄汉平,楚雄盆地铜、膏盐、有机矿床组合地球化学.成都理工学院学报,1998,25(2)：241-245.
[62]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[63]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[1]中国科学院地球化学研究所,铁的地球化学.北京：科学出版社,1981：52-85.
[2]刘英俊,曹励明,李兆麟,元素地球化学.北京：科学出版社,1984：95-176.
[3]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：19-40.
[4]冯增昭,王英华,刘焕杰,中国沉积学.北京：石油工业出版社,1994：347-456.
[5]王中刚,于学元,赵振华,稀土元素地球化学.北京：科学出版社,1989,88-93,436.
[6]Bau M. Rare-earth mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium. Chem. Geol.,1991,93:219-230.
[7]Giuliani G, Chelletz A and Mechiche M. Behavior of REE during thermal metamorphism and hydrothermal infiltration associated with skarn-and-vein-type tungsten orebodies in Central Morocco. Chem. Geol., 1987,64:279-294.
[8]凌其聪,刘丛强,水-岩反应与稀土元素行为.矿物学报,2001,21(1)：107-114.
[9]Michard A and Albarede F. The REE content of some hydrothermal fluids. Chem. Geol.,1986,55:51-60.
[10]Oi T, Kikawada Honda T, Ossaka T and Kakihana H. Determination of the lanthanoids in a neutral hot spring water by neutron activation analysis. J. Radioanal. Nucl. Chem.,1990,140:365-377.
[11]Sanjuan B, Michard A and Michard G. Influence of the temperature of CO2- rich springs on their aluminium and rare-earth elements contents. Chem. Geol.,1988,68:57-67.
[12]McLennan W H. REE mobility at constant in inter-REE ratio in the alteration zone at the Phelps Dodge missive sulfide deposits, M atagami, Quebe.Mineral. Deposita,1988,23:231-238.
[13]Lottermoser B G. Rare-earth element behaviour associated with strata-bound scheelite mineralization(Broken Hilll, Australia.Chem. Geol.,1989a,78:119-134.
[14]Michard A, Beaucarire C and Michard G. Uranium and rare-earth elements in CO2- rich waters from Vals-Bains(France). Geochim. Cosmochim. Acta,1987,51:901-909.
[15]Wendlant R F and Harrison W J. Rare-earth partitioning between immiscible carbonate and silicate liquids and CO2 vapour, result and implications for the formation of light earth-enriched rocks. contrib. Mineral.,1979,69:409-419.
[16]Oreskes N and Einaudi T. Origin of rare earth elements-enriched hematite breccias at the Olympic Dam Cu-U-Au-Ag deposits, Roxby downs, South Australia. Econ. Geol.,1990.85:1-28.
[17]Dickin A P. Evidence for limited REE leaching from the Roffna Gneiss, Switzerland-a discussion of the paper by Vocke et al.. Contrib, Mineral. Petrol.,1988,99:273-275.
[18]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：58-64.
[19]卢涣章,范宏瑞,倪培等.流体包裹体.北京：科学出版社,2004.
[20]普传杰,秦德先,牟定铜矿的稳定同位素及流体包裹体研究.云南地质,1994,13(2)：166-176.
[21]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[22]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[23]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版社,1998：65-67.
[24]陈骏,王鹤年,地球化学.北京：科学出版社,2004：131.
[25]冉崇英,刘卫华,何明勤等,康滇地轴铜矿床地球化学与矿床层楼结构机理.北京：科学出版社,1993：1-71,106-133.
[26]陈根文,吴延之,夏斌等,楚雄盆地砂岩铜矿床同位素特征及矿床成因.大地构造与成矿学,2002,26(3)：279-284.
[27]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[28]何明勤,冉崇英,刘卫华等,大姚铜矿床有机质特征及其与成矿的关系.石油与天然气地质,1991,12(2)：195-206.
[29]陈岳龙,杨忠芳,赵志丹,同位素地质年代学与地球化学.北京：地质出版社.2005：275-276.
[30]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[31]张理刚,稳定同位素在地质科学中的应用.西安：陕西科学技术出版社,1985.
[32]陈好寿,冉崇英等,康滇地轴铜矿床同位素地球化学.北京：地质出版社,1992：1-86.
[1]云南省冶金局地质勘探公司,砂岩铜矿地质.北京：冶金工业出版社,1977：1-227.
[2]方向池,卢今才,王维贤,云南六苴矿区构造动力成矿探讨.西南矿产地质,1990,4(4)：49-56.
[3]冉崇英,康滇地轴层控铜矿床的成矿机理.北京：地质出版社.1989.
[4]冉崇英,庄汉平,楚雄盆地铜、盐、有机矿床组合地球化学.北京：科学出版社,1998：10-16.
[5]徐一仁,张素华,论砂岩铜矿的成因机制及其在找矿中的指导作用.有色金属矿产与地质,1993,(1)：6-13.
[6]秦德先,牟定郝家河铜矿含矿浅色层及矿床成因.云南地质,1994,13(1)：49-56.
[7]谭凯旋,砂岩铜矿地球化学和成矿动力学.地震出版补.1998:170-113
[8]沈定华,与峨眉山玄武岩有关的铜矿床的成矿机制剖析.四川地质学报,1993,13(1)：32-36.
[9]陈国达,彭省临,戴塔根,云南铜-多金属壳体大地构造成矿学.长沙：中南大学出版社,2004,10：186-210.
[10]徐绍文,楚雄盆地砂岩铜矿的成矿机制和找矿方向.铜矿地质论文汇编,云南省地质矿产局地质科技情报中心,1992,9：38.
[11]张可清,熊鹏飞,滇中砂岩铜矿成矿作用和成矿模式.地球科学-中国地质大学报.1995.20(2)：199-202.
[12]涂光炽,中国层控矿床地球化学(第三卷).北京：科学出版社,1988：1-20.312-336.
[13]秦德先,孟清,杨明初等,牟定郝家河铜矿床的沉积-改造成因.矿床地质,1993.12(2)97-108.
[14]何明勤,冉崇英,刘卫华等,大姚铜矿床有机质特征及其与成矿的关系.石油与天然气地质,1991,12(2)：195-206.
[15]张位及,红铁尘-红层的染色剂与砂岩铜矿的成因.西南冶金地质勘探公司内部资料.
[16]刘立钧,王均灿,地洼活动与花岗岩型铀矿化.活化构造理论(地洼学说)的应用与发展-“地洼学说奖”历届获奖论文选集.中国科学院长沙大地构造研究所：地震出版社,北京,1999.
[17]马艳萍,刘池洋,吴柏林,砂岩漂白现象的形成及其启示(盆地多种能源矿产共存富集成藏(矿)研究进展).北京：科学出版社,2005：141-149.
[18]Moulton G F. Some features of red bed bleaching. American Association of Petroleum Geologists Bulletin,1922,10:304-311.
[19]Shebl M A, Redox reactions in hydrocarbon clastic reservoirs:Experiental validation of this mechanism for porosity enhancement. Chemical Geology,1996,132:103-117.
[20]Suradm R C, Redox reactions involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstone. AAPG Bulletin,1993,77:1509-1518.
[21]余达淦,吴仁贵,陈培荣,铀资源地质学教程.哈尔滨：哈尔滨工程大学出版社,2007,10：250-290.
[22]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：219-247.
[23]E.N.哈什曼,S.S.亚当斯,秦楚笛译,陆相砂岩卷型铀矿床地质学和识别判据.原子能出版社,1980：37-158
[24]Sandstone-type Uranium deposits in China:geology and exploration techniques. Atomic Energy Press,2002.
[25]Adler,H. Concepts of uranium ore formation in reducing environments in sandstones and other sediments, in Formation of uranium ore deposits:Athens, International Atomic Energy Agency,1974:141-168.
[26]Brunt,D.A. Uranium in Tertiary stream channels, Lake Frome area, South Australia:Proceedings, Australian Institute of Mining and Metallurgy,1978,266:79-90.
[27]Childers,M.O. Uranium geology of the Kaycee area, Johns on County, Wyoming,:Wyoming geological Association,22nd Field Conference Guidebook,1970:13-20.
[28]Carrol,A.R. Late Paleozoic tectonic amalgamation of northwestern China:Sedimentary record of the northern Tarim, northwestern Turpan, and southern junggar Basins, Geol. Soc. Am. Bull.1995:571-594.
[29]De Veslud, Christian Le Carlier,3D modeling of uranium-bearing solution-collapse breccias in Proterozoic sandstones (Athabasca Basin, Canada)-Metallogenic interpretations. COMPUTERS & GEOSCIENCES,2009,35(1):92-107
[30]Alexandre, Paul, Geochronology of unconformity-related uranium deposits in the Athabasca Basin, Saskatchewan, Canada and their integration in the evolution of the basin. MINERALIUM DEPOSITA,2009,44(1):41-59.
[31]Li Ziying, And superposition metallogenic model of the sandstone-type uranium deposit in the northeastern Ordos Basin, China. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2008,82(4):745-749.
[32]Srivastava. S. K. Occurrence of sandstone-type uranium mineralization in the Umthongkut area, Mahadek Basin, West Khasi Hills District, Meghalaya, India. CURRENT SCIENCE,2008,94(12):1573-1575.
[33]Yang, X. Y. Occurrence of uranium minerals from sandstone-type uranium deposits, Ordos Basin. GEOCHIMICA ET COSMOCHIMICA ACTA,2008,72(12):A1058
[34]Rajesh, H. M. Mapping Proterozoic unconformity-related uranium deposits in the Rockhole area, Northern Territory, Australia using landsat ETM. ORE GEOLOGY REVIEWS, 2008,33(3):382-396.
[35]Li ZiYing, Origin of gray-green sandstone in ore bed of sandstone type uranium deposit in north Ordos Basin. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:165-173.
[36]Wu BoLin, Basical characteristics of fluid geologic process of interlayer oxidation zone sandstone-type uranium deposit. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:185-194.
[37]Fan AiPing, Research on diagenesis of the sandstone-type uranium deposits in Dongsheng area, Ordos Basin. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50:195-202.
[38]Liu, J. A study of forming processes and prospecting indicators of sandstone type uranium ore by uranium series isotopes. WATER-ROCK INTERACTION, VOLS 1 AND 2, PROCEEDINGS, 2007:755-758.
[39]郭召杰,陈正乐,舒良树等,中国西部中亚型造山带中新生代陆内造山过程与砂岩型铀矿成矿作用.北京：地质出版社,2006.
[40]郭华,李明,夏斌等,查干诺尔盆地构造演化及铀成矿条件分析.北京：地质出版社,2004.
[41]李学礼,孙占学,周文斌,古水热系统与铀成矿作用.北京：地质出版社,2000.
[42]姚振凯,郑大瑜,刘翔,多因复成铀矿床及其成矿演化.北京：地质出版社,1998.
[43]刘池洋,盆地多种能源矿产共存富集成藏(矿)研究进展.北京：科学出版社,2005.
[44]孙泽轩,姚毅锋,巴音宝力格隆起带中新生代盆地砂岩铀矿类型及区域预测判据.矿物岩石,2004,24(4)：43-48.
[45]孙泽轩,陈洪德,朱西养,滇西新生代盆地砂岩型铀矿勘查现状与找矿前景.四川地质学报,2006,26(1)：24-28.
[46]孙泽轩,陈洪德,吴英,滇西新生代盆地与砂岩型铀矿成矿.地质论评,2006,52(4)：494-500.
[47]孙泽轩,陈洪德,朱西养,滇西新生代盆山耦合与砂岩型铀矿找矿方向.铀矿地质,2007,23(5)：289-296.
[48]蔡煜琦,韩效忠,李胜祥,天山造山带内中新生代盆地构造演化与砂岩型铀矿成矿的关系-以伊犁盆地、吐哈盆地为例.矿物学报,2007：91-92.
[49]李卫红,天山造山带中新生代盆地改造与砂岩型铀矿成矿.西北铀矿地质,2004,30(2)：41-47.
[50]朱同兴,黄志英,尹福光,盆山转换与沉积地质记录—以楚雄前陆盆地分析为例.岩相古地理.1999,19(3)：1-15.
[51]涂光炽,中国层控矿床地球化学(第三卷).北京：科学出版社,1988：255-297.
[52]田儒,对412矿床成矿条件及成因的一些认识.北京地质研究院,1980年报：193-304.
[53]田儒,我国中新生代陆相红层盆地铀矿床基本特征.北京轴矿地质研究所,1982年报： 21-25.
[54]刘武生,漆富成,谢佑新,塔里木盆地中新生代地质构造演化与砂岩型铀成矿作用关系探讨.世界核地质科学,2006,23(4)：187-193.
[55]龚斌利,李卫红,鄂尔多斯盆地直罗组和志丹群砂岩型铀矿形成条件及找矿方向.西北铀矿地质,2005,31(1)：7-11.
[56]唐相生,甘肃省酒泉一金塔地区砂岩型铀成矿条件浅析.华东铀矿地质,2005(1)：8-14.
[57]刘健,陈正乐,张红喜,准噶尔盆地西北部中新生代地层铀矿成矿能力探讨.地质力学学报,2003,9(3)：241-244.
[58]冉崇英,张智筠,刘卫华等,康滇裂谷旋回与铜矿层楼结构及其地球化学演化.中国科学B辑,1994,24(3)：325-330.
[59]崔银亮,中国南方砂(页)岩铜矿床硫同位素地球化学研究.地质地球化学.1997(2)：25-29.
[60]赵宝光,陈友良,姚毅峰,滇西新生代盆地沉积特征及砂岩型铀矿成矿条件.铀矿地质,2003,19(6)：344-348.
[61]陈戴生,李胜祥,蔡煜琦,我国中、新生代盆地砂岩型铀矿沉积环境研究概述.沉积学报,2006,24(2)：223-228.
[62]陈戴生,李胜祥,蔡煜琦,我国中新生代盆地砂岩型铀矿研究现状及发展方向的探讨.沉积学报,2003,21(1)：113-116.
[63]陈根文,夏斌,吴延之,楚雄盆地砂岩铜矿成矿机理研究.中国科学(D辑),2002,30：169-175.
[64]陈正乐,李细根,宫红良,新疆库车黑英山地区晚新生代构造运动及其对砂岩型铀矿成矿的控制作用初析.中国地质,2006,33(3)：572-579.
[65]李宝新,徐建国,王冰,新疆伊犁盆地南缘新生代构造特征及其对砂岩型铀矿的控制作用.新疆地质,2008,26(3)：297-300.
[66]彭云彪,陈安平,焦养泉,鄂尔多斯盆地中北部中、新生代构造演化与大规模砂岩型铀成矿作用.矿物学报,2007：110-111.
[67]李建威,李先福,李紫金,湘赣边区中新生代走滑断裂系统及对热液铀成矿作用的控制.地质找矿论丛,2000,15(2)：166-173.
[68]陈小东,刘翔,邓国泉,湘桂地区中新生代走滑断裂系统对铀成矿的控制作用.大地构造与成矿学,2002,26(4)：345-353.
[69]陈祖伊,黄世杰.试述华东南中新生代不整合面型铀矿床.铀矿地质,1990,6(6)：349-358.
[70]涂汉江,铀、金地球化学研究中的Eh-pH相图简介.世界核地质科学,1990(4)：32-35.
[71]关广岳,金属矿床氧化带微生物地球化学.北京：科学出版社,1999,94-95.
[72]刘英俊,曹励明,李兆麟,元素地球化学.北京：科学出版社,1984,10：216-223,283-293.
[73]刘英俊,曹励明,元素地球化学导论.北京：地质出版社,1985.4,81-97,176-192.
[74]谢学锦,程志中,张立生,中国西南地区76种元素地球化学图集.北京：地质出版社,2008：73,121.
[75]魏继生,朱西养,陶晓风,四川盆地地浸砂岩型铀矿的区域成矿条件浅析.四川地质学报,2005,5(3)：135-139.
[76]刘建华,朱西养,王四利,四川盆地地质构造演化特征与可地浸砂岩型铀矿找矿前景.铀矿地质,2005,21(6)：321-330.
[77]朱觉人,巫声扬,冯佩莘,四川盆地北部中生代砂岩型铀矿床成因探讨.四川地质学报,1991,2(1),53-63.
[78]中国科学院地球化学研究所,铁的地球化学.北京：科学出版社,1981：52-85.
[79]谭凯旋,张哲儒,王忠刚,辉铜矿、黄铜矿和斑铜矿的溶解动力学Ⅰ.温度、pH和NaCl浓度的影响.矿物学报,1997,17(1)：38-44.
[80]丁俊华,王雅芬,王正云等,云南大姚铜矿银的赋存状态与成矿地质特征.桂林冶金地质学院,1992：1-51.
[81]黄敦义,滇中六苴铜矿床原生矿段的构造研究.西南矿产地质,1992,3：50-58.
[82]陈根文,吴延之,夏斌等,楚雄盆地砂岩铜矿床同位素特征及矿床成因.大地构造与成矿学,2002,26(3)：279-284.
[83]杨蔚华,刘友梅,滇中中生代层控铜矿床的地球化学.中国科学(B辑),1983,8：833-841.
[84]Agterberg F P, Geomathematics, Elvsevier Scientific Publishing Company. Ameteradm, London, New York,1974.
[85]梁祥济,水-岩相互作用和成矿物质来源.北京：学苑出版社,1995,12：129.
[86]Goldhaber M B,Mechanisms of sulfur incorporation and isotope fractionation during earsy diagenesis in sediments of the Gulf of California. Marine Chemistry,1980,9:95-143.
[87]沈苏,金明霞,陆元法,西昌-滇中地区主要矿产成矿规律及找矿方向.重庆：重庆出版社,1988：191-197.
[88]刘存林,滇中含铜砂岩成矿规律及找矿方向.《铁铜矿产专辑》第七集.北京：地质出版社,1977.
[89]P.Ramdohr(德),谢宇平等译,金属矿物及其交生(中册).长春：长春地质学院图书馆,长春地质学院图书馆情报部,1986,10：7.
[90]戴塔根,龚铃兰,张起钻,应用地球化学.长沙：中南大学出版社,2005：257-258.
[91]Haynes.D.W, Stratiform copper deposits hosted by low-energy sediments:Nature of source rocks and composition of metal transporting water. Econ.Geol.1986,81:266-280.
[92]J.B.梅纳德,沉积矿床地球化学.北京：地质出版社,1986：13-49.
[93]陈俊,王鹤年,地球化学.北京：科学出版社2004：312-314.
[94]刘宝珺,沉积岩石学.北京：地质出版社,1980：60-66.
[1]刘英俊,邱德同,勘查地球化学.北京：科学出版社,1987.
[2]西南冶金地质勘探公司地研所情报室,国外地质资料(铜矿专辑).1982.
[3]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.
[4]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[5]欧阳宗圻,李惠,刘汉忠,典型有色金属矿床地球化学异常模式.科学出版社,1990.
[6]B.A.巴尔苏科夫,成矿理论的发展是应用地球化学继续进步的基本前提.国外地质科技,1983,No.4.
[7]B.C.波波夫,大型矿床的矿物-地球化学指示标志.地质科技动态,1986,No.2.
[8]M.C.拉斐洛维奇,金矿床某些元素的物理化学性质、地球化学组合和垂直地球化学分带.地质科技动态,1984,No.22.
[9]H.E.Hawkes and J.S.Webb:1962,Geochemistry in Mineral Exploration,Harper & Row.New York and Enanston.
[10]A.A.Levinson:1973,Introduction to Exploration Geochemistry. Applied Publishing Ltd.Colgary,Alberta,Canada.
[11]H.E.Hawkes and J.S.Webb:1979,Geochemistry in Mineral Exploration(Second edition).
[12]A.A.Levinson:1980,Introduction to Exploration Geochemistry(Second edition).
[13]F.R.Siegel:1974,Applied Geochemistry.
[14]I.L.Ellcott and W.K.Flelcher:1974,Geochemical Exploration.
[15]Doe, B.R. and Zartman,R.E.,1979,Plumbotectonic,the Phanerozoic,In: Geochemistry of Hydrothermal Ore Deposits,2nd edition. John Wolley & Sons, Inc.,pp.22-66.
[16]Boyle,R.W.,1977,Geochemistry overview,Paper Presented at "Exploration77".
[17]谢学锦,邵跃,地球化学岩石测量的工作方法与解释推断方法,物探化探研究报导,地质部物探研究所,1956,No.5.
[18]邵跃,白银厂地区的地球化学探矿.地球物理勘探,1956,No.9.
[19]邵跃,辽宁某铅-锌矿区原生晕的研究.地球物理勘探,1956,No.12.
[20]谢学锦,陈洪才,原生晕方法普查勘探中的作用.地质学报,1961,41.
[21]谢学锦,区域化探.地质出版社,1979.
[22]张本仁,《勘查地球物理勘查地球化学文集》第二集.地质出版社出版,1985.
[23]欧阳宗圻,李惠,刘汉忠,典型有色金属矿床地球化学异常模式.科学出版社,1990.
[24]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[25]邵跃,热液矿床岩石测量找矿.北京：地质出版社,1997.
[26]黄薰德,吴郁彦,地球化学找矿.北京：地质出版社,1986.
[27]涂光炽,中国层控矿床地球化学(第一卷).北京：科学出版社,1984：257-259.
[28]周永章,Jayanta Guha, Edward H. Chown,卢焕章,元素迁移的分维结构、级序路径及共轭地球化学异常存在的理论依据.地球化学,1995,24(1)：69-75.
[29]戴塔根,龚铃兰,张起钻,应用地球化学.长沙：中南大学出版社,2005：257-258.
[30]刘英俊,邱德同,勘查地球化学.北京：科学出版社,1987：15-16.
[31]桂林冶金地质研究所,地球化学探矿分析方法.冶金出版社,1974.
[32]吴锡生,化探数据处理方法.北京：地质出版社,1992.
[33]蒋敬业,应用地球化学.武汉：中国地质大学出版社,2006.
[34]闵茂中,白南静,地质测试样品采集及送测指南.北京：科学出版社,1990：1-8.
[35]张承亮,程德兰,地球化学样品分析.北京：地质出版社,1989.
[36]范永香,阳正熙,成矿规律与矿矿预测.徐州：中国矿业大学出版社,2003：251-266.
[37]胡惠民,大比例尺成矿预测方法.北京：地质出版社,1995.
[38]徐强,潘桂棠,王立全,主要类型铜矿床(体)快速定位预测.北京：地质出版社,2003：1-10.
[39]翟裕生,邓军,崔彬等,成矿系统及综合地质异常.现代地质,1999,13(2).
[40]翟裕生,邓军,王建平等,深部找矿研究问题.矿床地质,2004,23(2).
[41]谢学锦,程志中,张立生,中国西南地区76种元素地球化学图集.北京：地质出版社,2008：73.
[42]郭远生,罗荣生等,滇中砂岩铜矿地质.昆明：云南科技出版社,2008,12：58-64.
[43]王维贤,楚雄地区砂岩铜矿成矿预测及靶区优选.1997：8-154.
[44]韩润生,邹海俊,吴鹏等,云南省大姚县六苴铜矿小河—石门坎矿段接替资源勘查—2007年工作总结报告[R].2007,11.
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