西藏拉抗俄斑岩铜钼矿床辉钼矿Re-Os同位素测年及其地质意义
|
摘要
西藏冈底斯成矿带拉抗俄斑岩铜钼矿床位于西藏特提斯构造域拉萨地块东段中南部,是近年来青藏高原地质大调查项目评价的重点矿床之一。本文在钻孔地质编录的基础上,采用辉钼矿Re-Os同位素测年技术,对拉抗俄铜钼矿床中8件产于花岗闪长斑岩中的辉钼矿进行定年,获得了拉抗俄矿床辉钼矿成矿年龄,辉钼矿Re-Os模式年龄为(13.20±0.20)Ma~(13.64±0.21)Ma,加权平均值为(13.38±0.15)Ma,等时线年龄为(13.12±0.44)Ma,代表了拉抗俄斑岩铜钼矿床的成矿时代,成矿作用发生于中新世。辉钼矿中Re的含量为343.6×10-6~835.7×10-6,平均557.8×10-6,指示其成矿物质中有幔源物质加入。拉抗俄斑岩铜钼矿床形成于印度—亚洲大陆碰撞造山带碰撞过程的伸展背景,其成矿年龄与冈底斯斑岩铜矿带东段中亚带众多斑岩-矽卡岩成矿系统年龄基本一致(17~12 Ma),相对于同一矿集区的驱龙、甲玛、邦铺斑岩-矽卡岩型铜多金属矿的成矿年龄小2~3 Ma,但其形成受控于相同的成矿地球动力学背景。
The Lakange porphyry Cu-Mo deposit in the Gangdise metallogenic belt of central and southern East Lhasa block within the Tethys tectonic domain is one of the key deposits in the Tibet Plateau geological survey project evaluation in recent years. ReOs isotopic dating technique was applied for determination of mineralization events, and eight molybdenite samples were analyzed for Re-Os isotopic compositions, with the model ages obtained ranging from(13.20±0.20) Ma to(13.64±0.21) Ma, and the isochron age being(13.12 ± 0.44)Ma which represents the metallogenic age of the Lakange porphyry Cu- Mo deposit, indicating Miocene.The Re content of the molybdenite is 343.6 × 10- 6-835.7×10- 6, with an average of 557.8 × 10- 6, suggesting that the metallogenic material originated from a source with mantle components. The Lakange porphyry Cu- Mo deposit was formed in a stretching background of India-Asia continental collision orogenic collision, the age(17-12 Ma) is identical with ages of numerous porphyryskarn mineralization systems in the eastern of Gangdise metallogenic belt, and is 2-3 Ma younger than ages of the porphyry-skarn copper polymetallic deposits in the same ore concentration area, such as Jiama, Qulong and Bangpu, with the formation controlled by the same metallogenic geodynamics setting.
The Lakange porphyry Cu-Mo deposit in the Gangdise metallogenic belt of central and southern East Lhasa block within the Tethys tectonic domain is one of the key deposits in the Tibet Plateau geological survey project evaluation in recent years. ReOs isotopic dating technique was applied for determination of mineralization events, and eight molybdenite samples were analyzed for Re-Os isotopic compositions, with the model ages obtained ranging from(13.20±0.20) Ma to(13.64±0.21) Ma, and the isochron age being(13.12 ± 0.44)Ma which represents the metallogenic age of the Lakange porphyry Cu- Mo deposit, indicating Miocene.The Re content of the molybdenite is 343.6 × 10- 6-835.7×10- 6, with an average of 557.8 × 10- 6, suggesting that the metallogenic material originated from a source with mantle components. The Lakange porphyry Cu- Mo deposit was formed in a stretching background of India-Asia continental collision orogenic collision, the age(17-12 Ma) is identical with ages of numerous porphyryskarn mineralization systems in the eastern of Gangdise metallogenic belt, and is 2-3 Ma younger than ages of the porphyry-skarn copper polymetallic deposits in the same ore concentration area, such as Jiama, Qulong and Bangpu, with the formation controlled by the same metallogenic geodynamics setting.
引文
[1]唐菊兴,李志军,多吉,等.西藏雄村铜金矿集区纽通门铜金矿床找矿勘查取得突破[J].矿床地质,2010,29(4):727-729.Tang Juxing,Li Zhijun,Duo Ji,et al.The prospecting exploration breakthrough of Niutongmen copper-gold deposit,Xiongcun copper-gold metallogenic district,Tibet[J].Mineral Deposits,2010,29(4):727-729(in Chinese with English abstract).
[2]唐菊兴,王登红,汪雄武,等.西藏甲玛铜多金属矿矿床地质特征及其矿床模型[J].地球学报,2010,31(4):495-506.Tang Juxing,Wang Denghong,Wang Xiongwu,et al.Geological features and metallogenic model of the Jiama copper-polymetallic deposit in Tibet[J].Acta Geoscientica Sinica,2010,31(4):495-506(in Chinese with English abstract).
[3]唐菊兴,邓世林,郑文宝,等.西藏墨竹工卡县甲玛铜多金属矿床勘查模型[J].矿床地质,2011,30(2):179-196.Tang Juxing,Deng Shilin,Zheng Wenbao,et al.An exporation model for Jiama copper polymetallic deposit in Maizhokunggar County,Tibet[J].Mineral Deposits,2011,30(2):179-196(in Chinese with English abstract).
[4]郭文铂,郑文宝,唐菊兴,等.西藏甲玛铜多金属矿床流体、成矿物质来源的地球化学约束[J].中国地质,2014,41(2):510-528.Guo Wenbo,Zheng Wenbao,Tang Juxing,et al.Geochemical constraints on the source of metallogenic fluids and materials in the Jiama polymetallic Cu deposit,Tibet[J].Geology in China,2014,41(2):510-528(in Chinese with English abstract).
[5]陈雷,秦克章,李光明,等.西藏冈底斯南缘努日铜钨钼矿床地质特征与矽卡岩矿物学研究[J].矿床地质,2012,31(3):417-437.Chen Lei,Qin Kezhang,Li Guangming,et al.Geological and skarn mineral characteristics of Nuri Cu-W-Mo deposit in southeast Gangdese,Tibet[J].Acta Geoscientica Sinica,2012,31(3):417-437(in Chinese with English abstract).
[6]李金祥,秦克章,李光明,等.冈底斯中段尼木斑岩铜矿田的KAr、40Ar/39Ar年龄:对岩浆-热液系统演化和成矿构造背景的制约[J].岩石学报,2007,23(5):953-966.Li Jinxiang,Qin Kezhang,Li Guangming,et al.K-Ar and40Ar/39Ar age dating of Nimu porphyry copper orefield in Central Gangdese:Constrains on magmatic-hydrothermal evolution and metallogenetic tectonic setting[J].Acta Petrologica Sinica,23(5):953-966(in Chinese with English abstract).
[7]郑有业,多吉,王瑞江,等.西藏冈底斯巨型斑岩铜矿带勘查研究最新进展[J].中国地质,2007,34(2):324-334.Zheng Youye,Duo Ji,Wang Ruijiang,et al.New Advances in the study of the gigantic Gandsese porphyry copper metallogenic zone,Tibet[J].Geology in China,2007,34(2):324-334(in Chinese with English abstract).
[8]杨志明,侯增谦,宋玉财,等.西藏驱龙超大型斑岩铜矿床:地质、蚀变与成矿[J].矿床地质,2008,27(3):279-318.Yang Zhiming,Hou Zengqian,Song Yucai,et al.Qulong superlarge porphyry Cu deposit in Tibet:Geology,alteration and mineralization[J].Mineral Deposits,2008,27(3):279-318(in Chinese with English abstract).
[9]王立强,唐菊兴,陈伟,等.西藏邦铺钼多金属矿床矽卡岩矿物学特征及其地质意义[J].中国地质,2014,41(2):562-576.Wang Liqiang,Tang Juxing,Chen Wei,et al.Mineralogical characteristics of skarn in the Bangpu Mo polymetallic deposit,Tibet,and their geological significance[J].Geology in China,2014,41(2):562-576(in Chinese with English abstract).
[10]高一鸣,陈毓川,唐菊兴,等.西藏工布江达县亚贵拉铅锌钼多金属矿床石英斑岩锆石SHRIMP定年及其地质意义[J].地质学报,2009,83(10):1436-1444.Gao Yiming,Chen Yuchuan,Tang Juxing,et al.SHRIMP U-Pb dating of zircon from quartz porphyry in the Yaguila Pb-Zn-Mo deposit,Gongbujiangda County,Tibet and ite Geological Implicatin[J].Acta Geologica Sinica,2009,83(10):1436-1444(in Chinese with English abstract).
[11]李光明,王高明,高达发,等.西藏冈底斯铜矿资源前景与找矿方向[J].矿床地质,2002,21(S1):144-147.Li Guangming,Wang Gaoming,Gao Dafa,et al.Perspective of copper ore deposit and its exploration direction in Gangdese metallogenic belt,Tibet[J].Mineral Deposits,2002,21(S1):144-147(in Chinese with English abstract).
[12]唐菊兴,陈毓川,多吉,等.西藏冈底斯成矿带东段主要矿床类型、成矿规律和找矿评价[J].矿物学报,2009,29(S1):476-478.Tang Juxing,Chen Yuchuan,Duo Ji,et al.The main ore types,metallogenic regularities and prospecting evaluation in the east of Gangdese metallogenic belt,Tibet[J].Acta Mieralogica Sinica,2009,29(S1):476-478(in Chinese with English abstract).
[13]曲晓明,侯增谦,李振清.冈底斯铜矿带含矿斑岩的40Ar/39Ar年龄及地质意义[J].地质学报,2003,77(2):245-252.Qu Xiaoming,Hou Zengqian,Li Zhenqing.40Ar/39Ar Ages of the ore-bearing porphyries of the Gangdese porphyry copper belt and their geological significanses[J].Acta Geologica Sinica,2003,77(2):245-252(in Chinese with English abstract).
[14]侯增谦,曲晓明,王淑贤,等.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用[J].中国科学(D辑),2003,33(7):609-618.Hou Zengqian,Qu Xiaoming,Wang Shuxian,et al.Re-Os dating of molybdenite from the Gangdese metallogenic belt,Tibet:applications of mineralization time and dynamic background[J].Science in China(Series D),2003,33(7):609-618(in Chinese).
[15]周详,曹佑功.西藏板块构造-建造图及说明书[M].北京:地质出版社,1984,1-20.Zhou Xiang,Cao Yougong.Tibet Plate Tectonics-construction Plans and Specifications[M].Beijing:Geological Publishing House,1984:1-20.
[16]潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533.Pan Guitang,Mo Xuanxue,Hou Zengqian,et al.Spatialtemporal framework of the Gangdese orogenic belt and its evolution[J].Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
[17]杨德明,李才,王天武.西藏冈底斯东段南北向构造特征与成因[J].中国区域地质,2001,20(4):392-397.Yang Deming,Li Cai,Wang Tianwu.Features and genesis of the north-south-trending tectonic belt in the eastern sector of the Gangdese Mountains,Tibet[J].Regional Geology of China,2001,20(4):392-397(in Chinese with English abstract).
[18]秦克章,李光明,赵俊兴,等.西藏首例独立钼矿:冈底斯沙让大型斑岩钼矿的发现及其意义[J].中国地质,2008,35(6):1101-1112.Qin Kezhang,Li Guangming,Zhao Junxing,et al.Discovery of sharing large-scale porphyry molybdenum deposit,the first single Mo deposit in Tibet and its significance[J].Geology in China,2008,35(6):1101-1112(in Chinese with English abstract).
[19]杜安道,何红蓼,殷宁万,等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347.Du Andao,He Hongliao,Yin Ningwan,et al.A study on the rhenium-osmium geochronometry of molybdenites[J].Acta Geologica Sinica,1994,68 4):339-347(in Chinese with English abstract).
[20]杜安道,赵敦敏,王淑贤,等.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄[J].岩矿测试,2001,20(4):247-252.Du Andao,Zhao Dunmin,Wang Shuxian,et al.Precise Re-Os dating for molybdenite by ID-NTIMS with Carius Tube sample preparation[J].Rock and Mineral Analysis,2001,20(4):247-252(in Chinese with English abstract).
[21]屈文俊,杜安道.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄[J].岩矿测试,2003:22(4):254-257.Qu Wenjun,Du Andao.Highly Precise Re-Os Dating of Molybdenite by ICP-MS with Carius Tube Sample Digestion[J].Rock and Mineral Analysis,2003,22(4):254-257(in Chinese with English abstract).
[22]Du A D,Wu S Q,Sun D Z,et al.Preparation and certificat ion of Re-Os dating reference materials:Molybdenite HLP and JDC[J].Geostandard and Geoanalytical Research,2004,28(1):41-52.
[23]蒋少涌,杨竞红,赵葵东,等.金属矿床Re-Os同位素示踪与定年研究[J].南京大学学报(自然科学版),2000,36(6):669-677.Jiang Shaoyong,Yang Jinghong,Zhao Kuidong,et al.Re-Os isotope tracer and dating methods in ore deposits research[J].Journal of Nanjing University(Natural Sciences),2000,36(6):669-677(in Chinese with English abstract).
[24]Shen J J,Papanastassiou D A,Wasserburg G J.Precise Re-Os determinations and systematics of iron meteorit es[J].Geochim.Cosmochim.Acta,1996,60:2887-2900.
[25]Smoliar M I,Walker R J,Morgan J W.Re-Os ages of groupⅡA,ⅢA,ⅣA andⅥB iron meteorites[J].Science,1996,271:1099-1102.
[26]Ludwig K R.User’s Manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center Special Publication,2003:1-70.
[27]Deng J,Wang Q F,Yang S J,et al.Genetic relationship between the Emeishan plume and the bauxite deposits in western Guangxi,China:Constraints from U-Pb and Lu-Hf isotopes of the detrital zircons in bauxite ores[J].Journal of Asian Earth Sciences,2010,37(5/6):412-424.
[28]孟健寅,杨立强,吕亮,等.滇西北红山铜钼矿床辉钼矿Re-Os同位素测年及其成矿意义[J].岩石学报,2013,4:1214-1222.Meng Jianyin,Yang Liqiang,Lv Liang,et al.Re-Os dating of molybdenite from the Hongshan Cu-Mo deposit in Northwest Yunnan and ite implications for mineralization[J].Acta Petrologica Sinica,2013,4:1214-1222(in Chinese with English abstract).
[29]聂凤军,张万益,杜安道,等.内蒙古小东沟斑岩型钼矿床辉钼矿铼-锇同位素年龄及地质意义[J].地质学报,2007,81(7):898-905.Nie Fengjun,Zhang Wanyi,Du Andao,et al.Re-Os isotopic dating on molybdenite separates from the Xiaodonggou porphyry Mo deposit,Hexigten Qi,inner Mongolia[J].Acta Geologica Sinica,2007,81(7):898-905(in Chinese with English abstract).
[30]李超,屈文俊,杜安道,等.含有普通锇的辉钼矿Re-Os同位素定年研究[J].岩石学报,2012,2:702-708.Li Chao,Qu Wenjun,Du Andao,et al.Study on Re-Os isotope in molybdenite containing common Os[J].Acta Petrologica Sinica,2012,2:702-708(in Chinese with English abstract).
[30]Stein H J.Low-rhenium molybdenite by metamorphism in northern Sweden:Recognition,genesis,and global implications[J].Lithos,2006,87:300-327.
[31]黄勇,唐菊兴,丁俊,等.西藏雄村斑岩铜矿床辉钼矿Re-Os同位素体系[J].中国地质,2013,40(1):302-311.Huang Yong,Tang Juxing,Ding Jun,et al.The Re-Os isotope system of the Xiongcun porphyry copper-gold deposit,Tibet[J].Geology in China,2013,40(1):302-311(in Chinese with English abstract).
[32]Mao J W,Wang Y T,Lehmann B,et al.Molybdenite Re-Os and albite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications[J].Ore Geology Reviews,2006,29:307-324.
[33]王登红,陈郑辉,陈毓川,等.我国重要矿产地成岩成矿年代学研究新数据[J].地质学报,2010,84(7):1030-1040.Wang Denghong,Chen Zhenhui,Chen Yuchuan,et al.New Data of the Rock-Foeming and Ore-Forming Chronology for China’s Important Mineeal Resources Areas[J].Acta Geologica Sinica,2010,84(7):1030-1040(in Chinese with English abstract).
[34]Wang L Q,Chen Y C,Tang J X,et al.LA-ICP-MS zircon U-Pb dating of intermediate-acidic intrusive rocks and molybdenite Re-Os dating from the Bangpu Mo(Cu)deposit,Tibet and its geological implication[J].Acta Geologica Sinica,2012,86(5):1225-1240.
[35]Stein H J,Morgan J W,Markey R J,et al.An introduction to ReOs:What's in it for the mineral industry?[J].SEG Newsletter,1998,32(1):8-15.
[36]Stein H J,Markey R J,Morgan J W,et al.The remarkable Re-Os chronometer in molybdenite:How and why it works[J].Terra Nova,2001,13(6):479-486.
[37]Stein H J,Scherstén A,Hannah J L,et al.Subgrain-scale decoupling of Re and187Os and assessment of laser ablation ICPMS spot dating in molybdenite[J].Geochimica et Cosmochimica,2003,67:3673-3686.
[38]Martin C E,Carlson R W,Shirey S B,et al.Os isotopic variation in basalts from Haleakala Volcano,Maui,Hawaii:a record of mamgmatic processes in oceanic mantle and crust[J].Earth Planet.Sci.Lett.,1994,128:287-301.
[39]Mao J W,Zhang Z C,Zhang Z H,et al.Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo)deposit in the northern Qilian Mountains and its geological significance[J].Geochimica et Cosmochimica Acta,1999,63(11/12):1815-1818.
[40]Mao J W,Du A D,Seltmann R,et al.Re-Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite,central Urals,Russia[J].Mineralium Deposita,2003,38:251-257.
[41]王富春,陈静,谢志勇,等.东昆仑拉陵灶火钼多金属矿床地质特征及辉钼矿Re-Os同位素定年[J].中国地质,2013,40(4):1209-1217.Wang Fuchun,Chen Jing,Xie Zhiyong,et al.Geological features and Re-Os isotopic dating of the Lalingzaohuo molybdenum polymetallic deposit in East Kunlun[J].Geology in China,2013,40(4):1209-1217(in Chinese with English abstract).
[42]曲晓明,侯增谦,李佑国.S、Pb同位素对冈底斯斑岩铜矿带成矿物质来源和造山带物质循环的指示[J].地质通报,2002,21(11):768-776.Qu Xaioming,Hou Zengqian,Li Youguo.Implications of S and Pb isotopic compositions of the Gangdese porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt[J].Geological Bulletin of China,2002,21(11):768-776(in Chinese with English abstract).
[43]Chang K.Review of Sino-Tibetan:A Conspectus(Benedict).JAS,1973,32:335-337.
[44]Pearce J A,Mei H.Volcanic rocks for the 1985 Tibet Geotraverse Lhasa to Golmud[J].Phil.Trans.Roy.Soc.Load.A,1988,327:203-213.
[45]莫宣学,董国臣,赵志丹,等.西藏冈底斯带花岗岩的时空分布特征及地壳生长演化信息[J].高校地质学报,2005,11(3):281-290.Mo Xuanxue,Dong Guochen,Zhao Zhidan,et al.Spatial and temporal distribution and characteristics of granitoids in the Gangdese,Tibet and implication for crustal growth and evolution[J].Geological Journal of China Universities,2005,11(3):281-290(in Chinese with English abstract).
[46]朱弟成,潘桂棠,王立全,等.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境[J].地质通报,2008,27(4):458-466.Zhu Dicheng,Pan Guitang,Wang Liquan,et al.Spatial-temporal distribution and tectonic setting of Jurassic magmatism in the Gangdese belt,Tibet,China[J].Geological Bulletin of China,2008,27(4):458-468(in Chinese with English abstract).
[47]唐菊兴,黄勇,李志军,等.西藏谢通门县雄村同金矿床元素地球化学特征[J].矿床地质,2009,28(1):15-28.Tang Juxing,Huang Yong,Li Zhijun,et al.Element geochemical characteristics of Xiongcun Cu-Au deposit in Xaitongmoin County,Tibet[J].Mineral Deposits,2009,28(1):15-28(in Chinese with English abstract).
[48]闫学义,黄树峰,杜安道.冈底斯泽当大型钨铜钼矿Re-Os年龄及陆缘走滑转换成矿作用[J].地质学报,2010,84(3):398-405.Yan Xueyi,Huang Shufeng,Du Andao.Re-Os ages of large tungsten,copper and molybdenum deposit in the Zetang orefield,Gangdese and marginal strike-slip transforming metallogenesis[J].Acta Geoloica Sinica,2010,84(3):398-405(in Chinese with English abstract).
[49]应立娟,王登红,唐菊兴,等.西藏甲玛铜多金属矿辉钼矿ReOs定年及其成矿意义[J].地质学报,2010,84(8):1165-1174.Ying Lijuan,Wang Denghong,Tang Juxing,et al.Re-Os Dating of Molybdenite from the Jiama Copper Polymetallic Deposit in Tebet and its Metallogenic Significance[J].Acta Geologica Sinica,2010,84(8):1165-1174(in Chinese with English abstract).
[50]孟祥金,侯增谦,高永丰,等.西藏冈底斯成矿带驱龙铜矿ReOs年龄及成矿学意义[J].地质论评,2003,49(6):660-666.Meng Xiangjin,Hou Zengqian,Gao Yongfeng,et al.Re-Os dating for molybdenite from Qulong porphyry copper deposit in Gangdese metallogenic belt,Tibet and its metallogenic significance[J].Geological Review,2003,49(6):660-666(in Chinese with English abstract).
[51]芮宗瑶,侯增谦,曲晓明,等.冈底斯斑岩铜矿成矿时代及青藏高原隆升[J].矿床地质,2003,22(3):217-225.Rui Zongyao,Hou Zengqian,Qu Xiaoming,et al.Metallogenetic epoch of Gangdese porphyry copper belt and uplift of QinghaiTibet Plateau[J].Mineral Deposits,2003,22(3):217-225(in Chinese with English abstract).
[52]芮宗瑶,李光明,张立生,等.西藏斑岩铜矿对重大地质事件的响应[J].地学前缘,2004,11(1):145-152.Rui Zongyao,Li Guangming,Zhang Lisheng,et al.The response of porphyry copper deposits to important geological events in Tibet[J].Earth Science Frontiers,2004,11(1):145-152(in Chinese with English abstract).
[53]李光明,芮宗瑶,王高明,等.西藏冈底斯成矿带甲马和知不拉铜多金属矿床的Re-Os同位素年龄及意义[J].矿床地质,2005,24(5):482-489.Li Guangming,Rui Zongyao,Wang Gaoming,et al.Molybdenite Re-Os dating of Jiama and Zhibula polymetallic copper deposits in Gangdese metallogenic belt of Tibet and its significance[J].Mineral Deposits,2005,24(5):482-489(in Chinese with English abstract).
[54]唐菊兴,陈毓川,王登红,等.西藏工布江达县沙让斑岩钼矿床辉钼矿铼-锇同位素年龄及其地质意义[J].地质学报,2009,83(5):698-702.Tang Juxing,Chen Yuchuan,Wang Denghong,et al.Re-Os dating of molybdenite from the Sharang porphyry molybdenum deposit in Gongbo’gyamda County,Tibet and its geological significance[J].Acta Geologica Sinica,2009,83(5):698-702(in Chinese with English abstract).
[55]高一鸣,陈毓川,唐菊兴,等.西藏工布江达地区亚贵拉铅锌钼矿床辉钼矿Re-Os测年及其地质意义[J].地质通报,2011,30(7):1027-1036.Gao Yiming,Chen Yuchuan,Tang Juxing,et al.Re-Os dating of molybdenite from the Yaguila porphyry molybdenum deposit in Gongbo’gyamada area,Tibet,and its geological significance[J].Geological Bulletin of China,2011,30(7):1027-1036(in Chinese with English abstract).
[56]李光明,刘波,佘宏全,等.西藏冈底斯成矿带南缘喜马拉雅早期成矿作用——来自冲木达铜金矿床的Re-Os同位素年龄证据[J].地质通报,2006,12:1481-1486.Li Guangming,Liu Bo,She Hongquan,et al.Early Himalayan mineralization on the southern margin of the Gangdese metallogenic belt,Tibet,China:Evidence from Re-Os ages of the Chongmuda skarn-type Cu-Au deposit[J].Geological Bulletin of China,2006,25(12):1481-1486(in Chinese with English abstract).
[57]张刚阳,郑有业,龚福志,等.西藏吉如斑岩铜矿:与陆陆碰撞过程相关的斑岩成岩成矿时代约束[J].岩石学报,2008,24(3):473-479.Zhang Gangyang,Zheng Youye,Gong Fuzhi,et al.Geochronolgic constraints on magmatic instusions and mineralization of the Jiru porphyry copper deposit,Tibet,associated with continent-continent collisional process[J].Acta Petrologica Sinica,24(3):473-479(in Chinese with English abstract).
[58]王保弟,许继峰,陈建林,等.冈底斯东段汤不拉斑岩Mo-Cu矿床成岩成矿时代与成因研究[J].岩石学报,2010,26(6):1820-1832.Wang Baodi,Xu Jifeng,Chen Jianlin,et al.Petrogenesis and geochronology of the ore-bearing porphyritic rocks in Tangbula porphyry molybdenum-copper deposit in the eastern segment of the Gangdese metallogenic belt[J].Acta Petrologica Sinica,26(6):1820-1832(in Chinese with English abstract).
[59]郎兴海,唐菊兴,陈毓川,等.西藏冈底斯成矿带南缘新特提斯洋俯冲期成矿作用:来自雄村矿集区Ⅰ号矿体的Re-Os同位素年龄证据[J].地球科学——中国地质大学学报,2012,37(3):515-525.Lang Xinghai,Tang Juxing,Chen Yuchuan,et al.Neo-Tethys mineralization on the southern Margin of the Gangdese metallogenic belt,Tibet,China:Evidence from Re-Os ages of Xiongcun orebody No.Ⅰ[J].Earth Science—Journal of China University of Geosciences,2012,37(3):515-525(in Chinese with English abstract).
[60]郎兴海,唐菊兴,陈毓川,等.西藏谢通门县雄村斑岩型铜金矿集区Ⅱ号矿体中辉钼矿Re-Os年代学及地质意义[J].矿物岩石,2010,4:55-61.Lang Xinghai,Tang Juxing,Chen Yuchuan,et al.Re-Os dating of molybdenite from orebody No.Ⅱof the Xiongcun porphyry copper-gold metallogenic district,Xietongmen,Tibet and its geological significance[J].J.Mineral.Petrol.,2010,4:55-61(in Chinese with English abstract).
[61]Zhu D C,Pan G T,Chung S L,et al.SHRIMP zircon age and geochemical constraints on the origin of Lower Jurassic volcanic rocks from the Yeba Formation,southern Gangdese,south Tibet[J].International Geology Review,2008,50:442-471.
[62]唐菊兴,黎风佶,李志军,等.西藏谢通门县雄村铜金矿主要地质体形成的时限:锆石U-Pb、辉钼矿Re-Os年龄的证据[J].矿床地质,2010,29(3):461-472.Tang Juxing,Li Fengji,Li Zhijun,et al.Time limit for formation of main geological bodies in Xiongcun copper-gold deposit,Xietongmen County,Tibet:Evidence from zircon U-Pb ages and Re-Os age of molybdenite[J].Mineral Deposits,2010,29(3):461-472(in Chinese with English abstract).
[63]莫宣学,赵志丹,邓晋福,等.印度—亚洲大陆主碰撞过程的火山作用响应[J].地学前缘,2003,10(3):135-148.Mo Xuanxue,Zhao Zhidan,Deng Jinfu,et al.Response of volcanism to the India-Asia collision[J].Earth Science Frontiers,2003,10(3):135-148(in Chinese with English abstract).
[64]Miller C,Schuater R,Klotzli U,et al.Poat-collisional potassic and ultrapotassic magmatiam in SW Tibet:Geochemical and SrNd-Pb-O isotopic constraints for mantle source characteristics and petrogenesis[J].Journal of Petrology,1999,40:1399-1424.
[65]Mahéo G,Guillot S,Blichert-Tofa J,et al.A slab breakoff model for the Neogene thermal evolution of South Karakorum and South Tibet[J].Earth Science Letter,2002,195:45-58.
[66]侯增谦,高永丰,孟祥金,等.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制[J].岩石学报,2004,20(2):239-248.Hou Zengqian,Gao Yongfeng,Meng Xiangjin,et al.Genesis of adakitic porphyry and tectonic controls on the Gangdese Miocene porphyry copper belt in the Tibetan orogen[J].Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract).
[67]Hou Z Q,Gao Y F,Qu X M,et al.Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet[J].Earth and Planetary Science Letters,2004,220:139-155.
[68]侯增谦.大陆碰撞成矿论[J].地质学报,2010,84(1):30-58.Hou Zengqian.Metallogensis of continental collision[J].Acta Geologica Sinica,2010,84(1):30-58(in Chinese with English abstract).
1西藏自治区地质调查院.西藏达孜县拉抗俄铜矿调查评价报告(内部资料),2010.
1西藏自治区地质调查院.西藏达孜县拉抗俄铜矿调查评价报告.(内部资料),2010.
[2]唐菊兴,王登红,汪雄武,等.西藏甲玛铜多金属矿矿床地质特征及其矿床模型[J].地球学报,2010,31(4):495-506.Tang Juxing,Wang Denghong,Wang Xiongwu,et al.Geological features and metallogenic model of the Jiama copper-polymetallic deposit in Tibet[J].Acta Geoscientica Sinica,2010,31(4):495-506(in Chinese with English abstract).
[3]唐菊兴,邓世林,郑文宝,等.西藏墨竹工卡县甲玛铜多金属矿床勘查模型[J].矿床地质,2011,30(2):179-196.Tang Juxing,Deng Shilin,Zheng Wenbao,et al.An exporation model for Jiama copper polymetallic deposit in Maizhokunggar County,Tibet[J].Mineral Deposits,2011,30(2):179-196(in Chinese with English abstract).
[4]郭文铂,郑文宝,唐菊兴,等.西藏甲玛铜多金属矿床流体、成矿物质来源的地球化学约束[J].中国地质,2014,41(2):510-528.Guo Wenbo,Zheng Wenbao,Tang Juxing,et al.Geochemical constraints on the source of metallogenic fluids and materials in the Jiama polymetallic Cu deposit,Tibet[J].Geology in China,2014,41(2):510-528(in Chinese with English abstract).
[5]陈雷,秦克章,李光明,等.西藏冈底斯南缘努日铜钨钼矿床地质特征与矽卡岩矿物学研究[J].矿床地质,2012,31(3):417-437.Chen Lei,Qin Kezhang,Li Guangming,et al.Geological and skarn mineral characteristics of Nuri Cu-W-Mo deposit in southeast Gangdese,Tibet[J].Acta Geoscientica Sinica,2012,31(3):417-437(in Chinese with English abstract).
[6]李金祥,秦克章,李光明,等.冈底斯中段尼木斑岩铜矿田的KAr、40Ar/39Ar年龄:对岩浆-热液系统演化和成矿构造背景的制约[J].岩石学报,2007,23(5):953-966.Li Jinxiang,Qin Kezhang,Li Guangming,et al.K-Ar and40Ar/39Ar age dating of Nimu porphyry copper orefield in Central Gangdese:Constrains on magmatic-hydrothermal evolution and metallogenetic tectonic setting[J].Acta Petrologica Sinica,23(5):953-966(in Chinese with English abstract).
[7]郑有业,多吉,王瑞江,等.西藏冈底斯巨型斑岩铜矿带勘查研究最新进展[J].中国地质,2007,34(2):324-334.Zheng Youye,Duo Ji,Wang Ruijiang,et al.New Advances in the study of the gigantic Gandsese porphyry copper metallogenic zone,Tibet[J].Geology in China,2007,34(2):324-334(in Chinese with English abstract).
[8]杨志明,侯增谦,宋玉财,等.西藏驱龙超大型斑岩铜矿床:地质、蚀变与成矿[J].矿床地质,2008,27(3):279-318.Yang Zhiming,Hou Zengqian,Song Yucai,et al.Qulong superlarge porphyry Cu deposit in Tibet:Geology,alteration and mineralization[J].Mineral Deposits,2008,27(3):279-318(in Chinese with English abstract).
[9]王立强,唐菊兴,陈伟,等.西藏邦铺钼多金属矿床矽卡岩矿物学特征及其地质意义[J].中国地质,2014,41(2):562-576.Wang Liqiang,Tang Juxing,Chen Wei,et al.Mineralogical characteristics of skarn in the Bangpu Mo polymetallic deposit,Tibet,and their geological significance[J].Geology in China,2014,41(2):562-576(in Chinese with English abstract).
[10]高一鸣,陈毓川,唐菊兴,等.西藏工布江达县亚贵拉铅锌钼多金属矿床石英斑岩锆石SHRIMP定年及其地质意义[J].地质学报,2009,83(10):1436-1444.Gao Yiming,Chen Yuchuan,Tang Juxing,et al.SHRIMP U-Pb dating of zircon from quartz porphyry in the Yaguila Pb-Zn-Mo deposit,Gongbujiangda County,Tibet and ite Geological Implicatin[J].Acta Geologica Sinica,2009,83(10):1436-1444(in Chinese with English abstract).
[11]李光明,王高明,高达发,等.西藏冈底斯铜矿资源前景与找矿方向[J].矿床地质,2002,21(S1):144-147.Li Guangming,Wang Gaoming,Gao Dafa,et al.Perspective of copper ore deposit and its exploration direction in Gangdese metallogenic belt,Tibet[J].Mineral Deposits,2002,21(S1):144-147(in Chinese with English abstract).
[12]唐菊兴,陈毓川,多吉,等.西藏冈底斯成矿带东段主要矿床类型、成矿规律和找矿评价[J].矿物学报,2009,29(S1):476-478.Tang Juxing,Chen Yuchuan,Duo Ji,et al.The main ore types,metallogenic regularities and prospecting evaluation in the east of Gangdese metallogenic belt,Tibet[J].Acta Mieralogica Sinica,2009,29(S1):476-478(in Chinese with English abstract).
[13]曲晓明,侯增谦,李振清.冈底斯铜矿带含矿斑岩的40Ar/39Ar年龄及地质意义[J].地质学报,2003,77(2):245-252.Qu Xiaoming,Hou Zengqian,Li Zhenqing.40Ar/39Ar Ages of the ore-bearing porphyries of the Gangdese porphyry copper belt and their geological significanses[J].Acta Geologica Sinica,2003,77(2):245-252(in Chinese with English abstract).
[14]侯增谦,曲晓明,王淑贤,等.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用[J].中国科学(D辑),2003,33(7):609-618.Hou Zengqian,Qu Xiaoming,Wang Shuxian,et al.Re-Os dating of molybdenite from the Gangdese metallogenic belt,Tibet:applications of mineralization time and dynamic background[J].Science in China(Series D),2003,33(7):609-618(in Chinese).
[15]周详,曹佑功.西藏板块构造-建造图及说明书[M].北京:地质出版社,1984,1-20.Zhou Xiang,Cao Yougong.Tibet Plate Tectonics-construction Plans and Specifications[M].Beijing:Geological Publishing House,1984:1-20.
[16]潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533.Pan Guitang,Mo Xuanxue,Hou Zengqian,et al.Spatialtemporal framework of the Gangdese orogenic belt and its evolution[J].Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
[17]杨德明,李才,王天武.西藏冈底斯东段南北向构造特征与成因[J].中国区域地质,2001,20(4):392-397.Yang Deming,Li Cai,Wang Tianwu.Features and genesis of the north-south-trending tectonic belt in the eastern sector of the Gangdese Mountains,Tibet[J].Regional Geology of China,2001,20(4):392-397(in Chinese with English abstract).
[18]秦克章,李光明,赵俊兴,等.西藏首例独立钼矿:冈底斯沙让大型斑岩钼矿的发现及其意义[J].中国地质,2008,35(6):1101-1112.Qin Kezhang,Li Guangming,Zhao Junxing,et al.Discovery of sharing large-scale porphyry molybdenum deposit,the first single Mo deposit in Tibet and its significance[J].Geology in China,2008,35(6):1101-1112(in Chinese with English abstract).
[19]杜安道,何红蓼,殷宁万,等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347.Du Andao,He Hongliao,Yin Ningwan,et al.A study on the rhenium-osmium geochronometry of molybdenites[J].Acta Geologica Sinica,1994,68 4):339-347(in Chinese with English abstract).
[20]杜安道,赵敦敏,王淑贤,等.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄[J].岩矿测试,2001,20(4):247-252.Du Andao,Zhao Dunmin,Wang Shuxian,et al.Precise Re-Os dating for molybdenite by ID-NTIMS with Carius Tube sample preparation[J].Rock and Mineral Analysis,2001,20(4):247-252(in Chinese with English abstract).
[21]屈文俊,杜安道.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄[J].岩矿测试,2003:22(4):254-257.Qu Wenjun,Du Andao.Highly Precise Re-Os Dating of Molybdenite by ICP-MS with Carius Tube Sample Digestion[J].Rock and Mineral Analysis,2003,22(4):254-257(in Chinese with English abstract).
[22]Du A D,Wu S Q,Sun D Z,et al.Preparation and certificat ion of Re-Os dating reference materials:Molybdenite HLP and JDC[J].Geostandard and Geoanalytical Research,2004,28(1):41-52.
[23]蒋少涌,杨竞红,赵葵东,等.金属矿床Re-Os同位素示踪与定年研究[J].南京大学学报(自然科学版),2000,36(6):669-677.Jiang Shaoyong,Yang Jinghong,Zhao Kuidong,et al.Re-Os isotope tracer and dating methods in ore deposits research[J].Journal of Nanjing University(Natural Sciences),2000,36(6):669-677(in Chinese with English abstract).
[24]Shen J J,Papanastassiou D A,Wasserburg G J.Precise Re-Os determinations and systematics of iron meteorit es[J].Geochim.Cosmochim.Acta,1996,60:2887-2900.
[25]Smoliar M I,Walker R J,Morgan J W.Re-Os ages of groupⅡA,ⅢA,ⅣA andⅥB iron meteorites[J].Science,1996,271:1099-1102.
[26]Ludwig K R.User’s Manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center Special Publication,2003:1-70.
[27]Deng J,Wang Q F,Yang S J,et al.Genetic relationship between the Emeishan plume and the bauxite deposits in western Guangxi,China:Constraints from U-Pb and Lu-Hf isotopes of the detrital zircons in bauxite ores[J].Journal of Asian Earth Sciences,2010,37(5/6):412-424.
[28]孟健寅,杨立强,吕亮,等.滇西北红山铜钼矿床辉钼矿Re-Os同位素测年及其成矿意义[J].岩石学报,2013,4:1214-1222.Meng Jianyin,Yang Liqiang,Lv Liang,et al.Re-Os dating of molybdenite from the Hongshan Cu-Mo deposit in Northwest Yunnan and ite implications for mineralization[J].Acta Petrologica Sinica,2013,4:1214-1222(in Chinese with English abstract).
[29]聂凤军,张万益,杜安道,等.内蒙古小东沟斑岩型钼矿床辉钼矿铼-锇同位素年龄及地质意义[J].地质学报,2007,81(7):898-905.Nie Fengjun,Zhang Wanyi,Du Andao,et al.Re-Os isotopic dating on molybdenite separates from the Xiaodonggou porphyry Mo deposit,Hexigten Qi,inner Mongolia[J].Acta Geologica Sinica,2007,81(7):898-905(in Chinese with English abstract).
[30]李超,屈文俊,杜安道,等.含有普通锇的辉钼矿Re-Os同位素定年研究[J].岩石学报,2012,2:702-708.Li Chao,Qu Wenjun,Du Andao,et al.Study on Re-Os isotope in molybdenite containing common Os[J].Acta Petrologica Sinica,2012,2:702-708(in Chinese with English abstract).
[30]Stein H J.Low-rhenium molybdenite by metamorphism in northern Sweden:Recognition,genesis,and global implications[J].Lithos,2006,87:300-327.
[31]黄勇,唐菊兴,丁俊,等.西藏雄村斑岩铜矿床辉钼矿Re-Os同位素体系[J].中国地质,2013,40(1):302-311.Huang Yong,Tang Juxing,Ding Jun,et al.The Re-Os isotope system of the Xiongcun porphyry copper-gold deposit,Tibet[J].Geology in China,2013,40(1):302-311(in Chinese with English abstract).
[32]Mao J W,Wang Y T,Lehmann B,et al.Molybdenite Re-Os and albite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications[J].Ore Geology Reviews,2006,29:307-324.
[33]王登红,陈郑辉,陈毓川,等.我国重要矿产地成岩成矿年代学研究新数据[J].地质学报,2010,84(7):1030-1040.Wang Denghong,Chen Zhenhui,Chen Yuchuan,et al.New Data of the Rock-Foeming and Ore-Forming Chronology for China’s Important Mineeal Resources Areas[J].Acta Geologica Sinica,2010,84(7):1030-1040(in Chinese with English abstract).
[34]Wang L Q,Chen Y C,Tang J X,et al.LA-ICP-MS zircon U-Pb dating of intermediate-acidic intrusive rocks and molybdenite Re-Os dating from the Bangpu Mo(Cu)deposit,Tibet and its geological implication[J].Acta Geologica Sinica,2012,86(5):1225-1240.
[35]Stein H J,Morgan J W,Markey R J,et al.An introduction to ReOs:What's in it for the mineral industry?[J].SEG Newsletter,1998,32(1):8-15.
[36]Stein H J,Markey R J,Morgan J W,et al.The remarkable Re-Os chronometer in molybdenite:How and why it works[J].Terra Nova,2001,13(6):479-486.
[37]Stein H J,Scherstén A,Hannah J L,et al.Subgrain-scale decoupling of Re and187Os and assessment of laser ablation ICPMS spot dating in molybdenite[J].Geochimica et Cosmochimica,2003,67:3673-3686.
[38]Martin C E,Carlson R W,Shirey S B,et al.Os isotopic variation in basalts from Haleakala Volcano,Maui,Hawaii:a record of mamgmatic processes in oceanic mantle and crust[J].Earth Planet.Sci.Lett.,1994,128:287-301.
[39]Mao J W,Zhang Z C,Zhang Z H,et al.Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo)deposit in the northern Qilian Mountains and its geological significance[J].Geochimica et Cosmochimica Acta,1999,63(11/12):1815-1818.
[40]Mao J W,Du A D,Seltmann R,et al.Re-Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite,central Urals,Russia[J].Mineralium Deposita,2003,38:251-257.
[41]王富春,陈静,谢志勇,等.东昆仑拉陵灶火钼多金属矿床地质特征及辉钼矿Re-Os同位素定年[J].中国地质,2013,40(4):1209-1217.Wang Fuchun,Chen Jing,Xie Zhiyong,et al.Geological features and Re-Os isotopic dating of the Lalingzaohuo molybdenum polymetallic deposit in East Kunlun[J].Geology in China,2013,40(4):1209-1217(in Chinese with English abstract).
[42]曲晓明,侯增谦,李佑国.S、Pb同位素对冈底斯斑岩铜矿带成矿物质来源和造山带物质循环的指示[J].地质通报,2002,21(11):768-776.Qu Xaioming,Hou Zengqian,Li Youguo.Implications of S and Pb isotopic compositions of the Gangdese porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt[J].Geological Bulletin of China,2002,21(11):768-776(in Chinese with English abstract).
[43]Chang K.Review of Sino-Tibetan:A Conspectus(Benedict).JAS,1973,32:335-337.
[44]Pearce J A,Mei H.Volcanic rocks for the 1985 Tibet Geotraverse Lhasa to Golmud[J].Phil.Trans.Roy.Soc.Load.A,1988,327:203-213.
[45]莫宣学,董国臣,赵志丹,等.西藏冈底斯带花岗岩的时空分布特征及地壳生长演化信息[J].高校地质学报,2005,11(3):281-290.Mo Xuanxue,Dong Guochen,Zhao Zhidan,et al.Spatial and temporal distribution and characteristics of granitoids in the Gangdese,Tibet and implication for crustal growth and evolution[J].Geological Journal of China Universities,2005,11(3):281-290(in Chinese with English abstract).
[46]朱弟成,潘桂棠,王立全,等.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境[J].地质通报,2008,27(4):458-466.Zhu Dicheng,Pan Guitang,Wang Liquan,et al.Spatial-temporal distribution and tectonic setting of Jurassic magmatism in the Gangdese belt,Tibet,China[J].Geological Bulletin of China,2008,27(4):458-468(in Chinese with English abstract).
[47]唐菊兴,黄勇,李志军,等.西藏谢通门县雄村同金矿床元素地球化学特征[J].矿床地质,2009,28(1):15-28.Tang Juxing,Huang Yong,Li Zhijun,et al.Element geochemical characteristics of Xiongcun Cu-Au deposit in Xaitongmoin County,Tibet[J].Mineral Deposits,2009,28(1):15-28(in Chinese with English abstract).
[48]闫学义,黄树峰,杜安道.冈底斯泽当大型钨铜钼矿Re-Os年龄及陆缘走滑转换成矿作用[J].地质学报,2010,84(3):398-405.Yan Xueyi,Huang Shufeng,Du Andao.Re-Os ages of large tungsten,copper and molybdenum deposit in the Zetang orefield,Gangdese and marginal strike-slip transforming metallogenesis[J].Acta Geoloica Sinica,2010,84(3):398-405(in Chinese with English abstract).
[49]应立娟,王登红,唐菊兴,等.西藏甲玛铜多金属矿辉钼矿ReOs定年及其成矿意义[J].地质学报,2010,84(8):1165-1174.Ying Lijuan,Wang Denghong,Tang Juxing,et al.Re-Os Dating of Molybdenite from the Jiama Copper Polymetallic Deposit in Tebet and its Metallogenic Significance[J].Acta Geologica Sinica,2010,84(8):1165-1174(in Chinese with English abstract).
[50]孟祥金,侯增谦,高永丰,等.西藏冈底斯成矿带驱龙铜矿ReOs年龄及成矿学意义[J].地质论评,2003,49(6):660-666.Meng Xiangjin,Hou Zengqian,Gao Yongfeng,et al.Re-Os dating for molybdenite from Qulong porphyry copper deposit in Gangdese metallogenic belt,Tibet and its metallogenic significance[J].Geological Review,2003,49(6):660-666(in Chinese with English abstract).
[51]芮宗瑶,侯增谦,曲晓明,等.冈底斯斑岩铜矿成矿时代及青藏高原隆升[J].矿床地质,2003,22(3):217-225.Rui Zongyao,Hou Zengqian,Qu Xiaoming,et al.Metallogenetic epoch of Gangdese porphyry copper belt and uplift of QinghaiTibet Plateau[J].Mineral Deposits,2003,22(3):217-225(in Chinese with English abstract).
[52]芮宗瑶,李光明,张立生,等.西藏斑岩铜矿对重大地质事件的响应[J].地学前缘,2004,11(1):145-152.Rui Zongyao,Li Guangming,Zhang Lisheng,et al.The response of porphyry copper deposits to important geological events in Tibet[J].Earth Science Frontiers,2004,11(1):145-152(in Chinese with English abstract).
[53]李光明,芮宗瑶,王高明,等.西藏冈底斯成矿带甲马和知不拉铜多金属矿床的Re-Os同位素年龄及意义[J].矿床地质,2005,24(5):482-489.Li Guangming,Rui Zongyao,Wang Gaoming,et al.Molybdenite Re-Os dating of Jiama and Zhibula polymetallic copper deposits in Gangdese metallogenic belt of Tibet and its significance[J].Mineral Deposits,2005,24(5):482-489(in Chinese with English abstract).
[54]唐菊兴,陈毓川,王登红,等.西藏工布江达县沙让斑岩钼矿床辉钼矿铼-锇同位素年龄及其地质意义[J].地质学报,2009,83(5):698-702.Tang Juxing,Chen Yuchuan,Wang Denghong,et al.Re-Os dating of molybdenite from the Sharang porphyry molybdenum deposit in Gongbo’gyamda County,Tibet and its geological significance[J].Acta Geologica Sinica,2009,83(5):698-702(in Chinese with English abstract).
[55]高一鸣,陈毓川,唐菊兴,等.西藏工布江达地区亚贵拉铅锌钼矿床辉钼矿Re-Os测年及其地质意义[J].地质通报,2011,30(7):1027-1036.Gao Yiming,Chen Yuchuan,Tang Juxing,et al.Re-Os dating of molybdenite from the Yaguila porphyry molybdenum deposit in Gongbo’gyamada area,Tibet,and its geological significance[J].Geological Bulletin of China,2011,30(7):1027-1036(in Chinese with English abstract).
[56]李光明,刘波,佘宏全,等.西藏冈底斯成矿带南缘喜马拉雅早期成矿作用——来自冲木达铜金矿床的Re-Os同位素年龄证据[J].地质通报,2006,12:1481-1486.Li Guangming,Liu Bo,She Hongquan,et al.Early Himalayan mineralization on the southern margin of the Gangdese metallogenic belt,Tibet,China:Evidence from Re-Os ages of the Chongmuda skarn-type Cu-Au deposit[J].Geological Bulletin of China,2006,25(12):1481-1486(in Chinese with English abstract).
[57]张刚阳,郑有业,龚福志,等.西藏吉如斑岩铜矿:与陆陆碰撞过程相关的斑岩成岩成矿时代约束[J].岩石学报,2008,24(3):473-479.Zhang Gangyang,Zheng Youye,Gong Fuzhi,et al.Geochronolgic constraints on magmatic instusions and mineralization of the Jiru porphyry copper deposit,Tibet,associated with continent-continent collisional process[J].Acta Petrologica Sinica,24(3):473-479(in Chinese with English abstract).
[58]王保弟,许继峰,陈建林,等.冈底斯东段汤不拉斑岩Mo-Cu矿床成岩成矿时代与成因研究[J].岩石学报,2010,26(6):1820-1832.Wang Baodi,Xu Jifeng,Chen Jianlin,et al.Petrogenesis and geochronology of the ore-bearing porphyritic rocks in Tangbula porphyry molybdenum-copper deposit in the eastern segment of the Gangdese metallogenic belt[J].Acta Petrologica Sinica,26(6):1820-1832(in Chinese with English abstract).
[59]郎兴海,唐菊兴,陈毓川,等.西藏冈底斯成矿带南缘新特提斯洋俯冲期成矿作用:来自雄村矿集区Ⅰ号矿体的Re-Os同位素年龄证据[J].地球科学——中国地质大学学报,2012,37(3):515-525.Lang Xinghai,Tang Juxing,Chen Yuchuan,et al.Neo-Tethys mineralization on the southern Margin of the Gangdese metallogenic belt,Tibet,China:Evidence from Re-Os ages of Xiongcun orebody No.Ⅰ[J].Earth Science—Journal of China University of Geosciences,2012,37(3):515-525(in Chinese with English abstract).
[60]郎兴海,唐菊兴,陈毓川,等.西藏谢通门县雄村斑岩型铜金矿集区Ⅱ号矿体中辉钼矿Re-Os年代学及地质意义[J].矿物岩石,2010,4:55-61.Lang Xinghai,Tang Juxing,Chen Yuchuan,et al.Re-Os dating of molybdenite from orebody No.Ⅱof the Xiongcun porphyry copper-gold metallogenic district,Xietongmen,Tibet and its geological significance[J].J.Mineral.Petrol.,2010,4:55-61(in Chinese with English abstract).
[61]Zhu D C,Pan G T,Chung S L,et al.SHRIMP zircon age and geochemical constraints on the origin of Lower Jurassic volcanic rocks from the Yeba Formation,southern Gangdese,south Tibet[J].International Geology Review,2008,50:442-471.
[62]唐菊兴,黎风佶,李志军,等.西藏谢通门县雄村铜金矿主要地质体形成的时限:锆石U-Pb、辉钼矿Re-Os年龄的证据[J].矿床地质,2010,29(3):461-472.Tang Juxing,Li Fengji,Li Zhijun,et al.Time limit for formation of main geological bodies in Xiongcun copper-gold deposit,Xietongmen County,Tibet:Evidence from zircon U-Pb ages and Re-Os age of molybdenite[J].Mineral Deposits,2010,29(3):461-472(in Chinese with English abstract).
[63]莫宣学,赵志丹,邓晋福,等.印度—亚洲大陆主碰撞过程的火山作用响应[J].地学前缘,2003,10(3):135-148.Mo Xuanxue,Zhao Zhidan,Deng Jinfu,et al.Response of volcanism to the India-Asia collision[J].Earth Science Frontiers,2003,10(3):135-148(in Chinese with English abstract).
[64]Miller C,Schuater R,Klotzli U,et al.Poat-collisional potassic and ultrapotassic magmatiam in SW Tibet:Geochemical and SrNd-Pb-O isotopic constraints for mantle source characteristics and petrogenesis[J].Journal of Petrology,1999,40:1399-1424.
[65]Mahéo G,Guillot S,Blichert-Tofa J,et al.A slab breakoff model for the Neogene thermal evolution of South Karakorum and South Tibet[J].Earth Science Letter,2002,195:45-58.
[66]侯增谦,高永丰,孟祥金,等.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制[J].岩石学报,2004,20(2):239-248.Hou Zengqian,Gao Yongfeng,Meng Xiangjin,et al.Genesis of adakitic porphyry and tectonic controls on the Gangdese Miocene porphyry copper belt in the Tibetan orogen[J].Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract).
[67]Hou Z Q,Gao Y F,Qu X M,et al.Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet[J].Earth and Planetary Science Letters,2004,220:139-155.
[68]侯增谦.大陆碰撞成矿论[J].地质学报,2010,84(1):30-58.Hou Zengqian.Metallogensis of continental collision[J].Acta Geologica Sinica,2010,84(1):30-58(in Chinese with English abstract).
1西藏自治区地质调查院.西藏达孜县拉抗俄铜矿调查评价报告(内部资料),2010.
1西藏自治区地质调查院.西藏达孜县拉抗俄铜矿调查评价报告.(内部资料),2010.