LA-ICP-MS zircon U-Pb ages and geological significance of the meta-intermediate-acidic volcanic rocks in Mangui area of Da Hinggan Mountains
LI Zhonghui1, LI Ruijie1, LI Yang2, SHA Huanyu1
1. Heilongjiang Institute of Geological Survey, Harbin 150036, China; 2. Heilongjiang Qiqihar Institute of Geological Exploration, Qiqihar 161006, China
Abstract:Through the zircon U-Pb isotopes chronology research of the meta-intermediate-acidic volcanic rocks of Neoproterozoic-Lower Cambrian Dawangzi Formation in Mangui area of Da Hinggan Mountains, the authors explored the forming age and geological significance of the rocks. Dawangzi Formation is composed of meta-andesite, meta-dacite, rhyolite and a small amount of meta-crystalline tuff, and lacks interbeds of sedimentary rocks such as slate, metasandstone and schist. The authors determined the zircon U-Pb isotopes age of the meta-andesite, and the zircon 206Pb/238U weighted mean age is (199±1) Ma, indicating that the forming age of Dawangzi Formation meta-intermediate-acidic volcanic rocks is the early stage of Early Jurassic, not Neoproterozoic-Early Cambrian as in previous research. Early Jurassic volcanic rocks distributed in Erguna Block provide a provenance for Mohe Basin. Erguna Block was in the volcano-magmatic arc tectonic background in Early Jurassic. This research supplies new data for the geodynamics study during the closure of Mongolia-Okhotsk Ocean.
李中会, 李睿杰, 李阳, 沙环宇. 大兴安岭满归地区变中酸性火山岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 中国地质调查, 2020, 7(1): 47-52.
LI Zhonghui, LI Ruijie, LI Yang, SHA Huanyu. LA-ICP-MS zircon U-Pb ages and geological significance of the meta-intermediate-acidic volcanic rocks in Mangui area of Da Hinggan Mountains. , 2020, 7(1): 47-52.
[1] 黑龙江省地质矿产局.黑龙江省岩石地层[M].武汉:中国地质大学出版社,1997:1-298. [2] 黑龙江省地质矿产局.前进林场幅、林海幅、柯多蒂河幅、塔源幅1∶5万区调报告[R].哈尔滨:黑龙江省地质矿产局,1995. [3] 黑龙江省地质矿产局第二区域地质调查大队.1∶20万六十林场、阿里河幅区域地质调查报告[R].齐齐哈尔:黑龙江省地质矿产局第二区域地质调查大队,1994. [4] 黑龙江省地质调查总院齐齐哈尔分院.漠河幅、漠河县幅1∶25万区域地质调查报告[R].齐齐哈尔:黑龙江省地质调查总院齐齐哈尔分院,2013. [5] 李锦轶,莫申国,和政军,等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘,2004,11(3):157-168. [6] 黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993:1-734. [7] Wu F Y,Sun D Y,Ge W C,et al.Geochronology of the Phanerozoic granitoids in northeastern China[J].J Asian Earth Sci,2011,41(1):1-30. [8] 耿建珍,李怀坤,张健,等.锆石Hf同位素组成的LA-MC-ICP-MS测定[J].地质通报,2011,30(10):1508-1513. [9] Liu Y S,Hu Z C,Zong K Q,et al.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J].Chin Sci Bull,2010,55(15):1535-1546. [10] Ludwig K R.User’s Manual for Isoplot/EX,Version 3.00,A GeoChronological Toolkit for Microsoft Excel[M].Berkeley:Berkeley Geochronology Center,Special Publication,2003:1-55. [11] 黑龙江省地质调查研究总院.十六站幅1∶5万区域地质调查报告[R].哈尔滨:黑龙江省地质调查研究总院,2014. [12] 黑龙江省地质矿产局第二区域地质调查大队.L-51-(21)(漠河幅)、L-51-(22)(连崟幅)、L-51-(27)(老沟幅)、L-51-(28)(二十五站幅)部分1∶20万区域地质调查报告[R].齐齐哈尔:黑龙江省地质矿产局第二区域地质调查大队,1988. [13] 李锦轶,和政军,莫申国,等.大兴安岭北部绣峰组下部砾岩的形成时代及其大地构造意义[J].地质通报,2004,23(2):120-129. [14] 侯伟,刘招君,何玉平,等.漠河盆地上侏罗统物源分析及其地质意义[J].地质论评,2010,56(1):71-81. [15] 陈衍景,张成,李诺,等.中国东北钼矿床地质[J].吉林大学学报:地球科学版,2012,42(5):1223-1268. [16] 吴福元,孙德有,林强.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报,1999,15(2):181-189. [17] 林强,吴福元,孙德有,等.大兴安岭中生代花岗岩类的地球化学[J].岩石学报,2004,20(3):403-412. [18] 林强. 东北亚中生代火山岩研究若干问题的思考[J].世界地质,1999,18(2):14-22.