内蒙古东乌旗沙麦钨矿床的成矿时代
The metallogenic age of the Shamai wolframite deposit in Dong Ujimqin Banner, Inner Mongolia
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摘要: 内蒙古东乌旗沙麦钨矿位于贺根山断裂带以北的兴蒙造山系二连-东乌旗弧盆带内,为岩浆期后高温热液黑钨矿石英脉型矿床。采用黑钨矿Sm-Nd同位素分析获得黑钨矿的形成年龄为137.9±1.7Ma,采用TIMS锆石U-Pb同位素定年获得赋矿黑云母花岗岩的形成年龄为139.1±0.93Ma,据此提出,沙麦钨矿床的形成时代为燕山晚期,这与区域上大兴安岭西坡主要金属矿床的形成年龄数据相吻合。黑钨矿的初始εNd值为正值,与中亚造山带内大量花岗岩的εNd值均为正值的特点相一致,表明其来源于亏损地幔源。Abstract: The Shamai wolframite deposit in Dong Ujimqin Banner of Inner Mongolia is located within the Erlian-Dong Ujimqin Banner arc-basin belt in the Da Hinggan Mountains-Inner Mongolia orogenic belt south of the Ergenshan fault. It is a postmagmatic high-temperature hydrothernal deposit. In this paper, wolframite Sm-Nd isotope analysis of the deposit yielded an ore formation age of 137.9±1.7Ma, whereas TIMS zircon U-Pb dating of samples from the wall rock biotite granite yielded a petrogenetic age of 139.1±0.93Ma. These isotopic ages indicate that the mineralization of Shamai wolframite deposit occurred in late Yanshanian, consis-tent with the age of the formation of the main ore deposits on the west slope of the Da Hinggan Mountains regionally. Consistent with the positive initial εNd value of granites scattered in central Asian orogenic belt, the initial εNd value of the wolframite is posi-tive, indicating a depleted mantle source.
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Key words:
- wolframite /
- biotite granite /
- zircon U-Pb age /
- Sm-Nd isotope age /
- Shamai
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[1] 潘桂堂,肖庆辉,陆松年,等.中国大地构造单元划分[J].中国地质, 2009,36(1):1-28.
[2] 李俊建,韩九曦,唐文龙,等.蒙古地质矿产概况[M].天津:天津科学技术出版社,2013:1-273.
[3] 徐志刚,陈毓川,王登红,等.中国成矿区带划分方案[M].北京:地质出版社,2008:1-11.
[4] 李俊建,张峰,任军平,等.中蒙边界地区构造单元划分[J].地质通报,2015,34(4):636-662.
[5] 胡朋,聂凤军,赫英, 等. 内蒙古沙麦岩体:正εNd(t)值的过铝质花岗岩[J].岩石学报, 2006,22(11):2781-2790.
[6] 胡朋,聂凤军,赫英,等. 内蒙古沙麦钨矿床地质及流体包裹体研究[J].矿床地质, 2005,24(6):203-212.
[7] 聂凤军,胡朋,江思宏, 等.中蒙边境沙麦-玉古兹尔地区钨和钨(钼)矿床地质特征,形成时代和成因机理[J].地球学报,2010,3:383-394.
[8] Fryer B J, Taylor R P. Sm-Nd derect dating of the Collins Bay hy-drothermal uranium deposit,Saskatchewan[J].Geology,1984,12:479-482.
[9] Halliday A N, Shepherd T J, Dicken A P, et al. Sm-Nd evidence for the age and origin of a Mississippi Valley ore deposit[J].Nature, 1990,344:54-56.
[10] Chesley J T, Halliday A N, Scrivener R C. Samarium-Neodymi-um direct dating of fluorite mineralization[J].Science,1991,252:949-951.
[11] 李志昌,王建华,杜国民.萤石Sm-Nd等时线[J].地质地球化学, 1987,15(9):67-68.
[12] 李华芹,刘家齐,杜国民,等.内生金属矿床成矿作用年代学研究-以西华山钨矿为例[J].科学通报,1992,37(12):10-15.
[13] 聂凤军,江思宏,白大明,等.北京密云沙厂环斑花岗杂岩体黑钨矿钐-钕同位素研究[J].地质论评,2002,48(1):29-33.
[14] 李俊建,燕长海,谢汝斌,等. 华北陆块主要成矿区带成矿规律和找矿方向[M].天津:天津科学技术出版社,2006:1-381.
[15] Angin C D, Jonasson I R, Franklin J M. Sm-Nd dating of scheelite and tourmaline:Implications oof the genesis of Archean gold depos-its, Vald'or, Canada[J]. Economical Geology, 1996, 91:1372-1382.
[16] Jiang S Y, Slack J F, Palmer M R. Sm-Nd dating of the giant Sulli-van Pb-Zn-Ag deposit,British Columbia[J].Geology,2000,28:751-754.
[17] Nie F J, Bjorlykke A B, Nilsen K S.The origen of the Proterozoic Bidjovagge gole-copper deposit, Finnmark, Northern Norway, as deduced from rare earth element anf Nd isotopeevidences on cal-cite[J]. Resource Geology,1999,49(1):13-25.
[18] 彭建堂,胡瑞忠,赵军平, 等.湘西沃溪Au-Sb-W矿床中白钨矿Sm-Nd和石英Ar-Ar定年[J].科学通报,2003,48(18):1976-1981.
[19] 彭建堂,胡瑞忠,林源贤,等.锡矿山锑矿床热液方解石的Sm-Nd同位素定年[J].科学通报,2002,47(10):789-792.
[20] 李惠民,李怀坤,陆松年.用矿脉中热液错石的U-Pb定年确定东坪金矿的成矿时代[J].地球学报,1997,18(增刊):176-178.
[21] Ludwig K R. Squid 1.02:a user's manual[J]. Berkeley Geochronol-ogy Centre, Special Publication 2,2001:19.
[22] 洪大卫,王式光,谢锡林, 等.试析地幔来源物质成矿域——以中亚造山带为例[J].矿床地质,2003,22(1):41-55.
[23] 洪大卫,王式光,谢锡林,等.兴蒙造山带正εNd(T)值花岗岩的成因和大陆地壳生长[J].地学前缘,2000,7(2):441-456.
[24] Cathles L M, Erendi A H J, Barrie T. How long can a hydrother-mal system be sustained by a single intrusive event?[J]. Econo. Ge-ol., 1997, 92(7/8):766-771.
[25] Henry C D, Elson H B, McIntosh W C. Brief Duration of Hydro-thermal activity at Round Mountain,Nvvada,Determined from 40Ar-39Ar Geochronology[J]. Economical Geology,1997,92(7/8):807-826.
[26] 聂凤军,张万益,杜安道, 等.内蒙古朝不楞矽卡岩型铁多金属矿床辉钼矿铼-锇同位素年龄及地质意义[J].地球学报,2007,28(4):315-323.
[27] 徐克勤,胡受奚,孙明志, 等.华南两个成因系列花岗岩及其成矿特征[J].矿床地质,1982,1(2):1-14.
[28] 陈毓川, 王登红, 朱裕生, 等.中国成矿体系与区域成矿评价[M]. 北京:地质出版社,2007:1-1005.
[29] 郝英. 关于"碱质交代成矿模式"的几点看法[J]. 矿床地质,1989, 8(3):90-96.
[30] 赫英,岳可芬,董振信, 等.中国东部地幔岩中的钨含量及其意义[J].地球化学,2003,32(6):561-565.
[31] 刘家远.西华山钨矿的花岗岩组成及与成矿的关系[J]. 地质找矿论丛,2005,25(1):1-7.
[32] 华仁民,李光来,张文兰, 等.华南钨和锡大规模成矿作用的差异及其原因初探[J]. 矿床地质,2010,29(1):9-23.
[33] 毛景文,谢桂青,郭春丽, 等. 南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,2007,23(10):2329-2338.
[34] 张作衡,毛景文,杨建民, 等.北祁连加里东造山带塔儿沟矽卡岩-石英脉型钨矿床地质及成因[J]. 矿床地质,2002,21(2):200-211.
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