GUO Jun, MA Fucai, YANG Wen, CHENG Linqiang, LI Peng, GUO Xuefeng. LA-ICP-MS zircon U-Pb ages of quartz-andesite in Daqingshan area, Inner Mongolia and its tectonic significance[J]. Geological Bulletin of China, 2016, 35(9): 1517-1521.
Citation: |
GUO Jun, MA Fucai, YANG Wen, CHENG Linqiang, LI Peng, GUO Xuefeng. LA-ICP-MS zircon U-Pb ages of quartz-andesite in Daqingshan area, Inner Mongolia and its tectonic significance[J]. Geological Bulletin of China, 2016, 35(9): 1517-1521.
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LA-ICP-MS zircon U-Pb ages of quartz-andesite in Daqingshan area, Inner Mongolia and its tectonic significance
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1. Academy of Regional Geological Survey and Mineral Resources Exploration of Shaanxi, Xianyang 712000, Shaanxi, China;
2. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China
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Abstract
Weighted average zircon 207Pb/206Pb age of 1870±19Ma was obtained from the quartz-andesite cut by the thrusting structure in Daqingshan area, Inner Mongolia. The quartz-andesite is the product of a breakup event between multi-stage rifting in the late Paleoproterozoic to Neoproterozoic period in North China. At the same time, according to the 206Pb/238U age of 436±4Ma from the concordant zircon (No. 06) of the basalt-andesite and the 206Pb/238U ages of 153±2Ma and 160±2Ma from the concordant zircons (No. 15 and 29) of the quartz-andesite, the structural revival and structural tracing phenomena exist in the thrusting tectonics in Daqingshan area. The results obtained by the authors have accumulated new information and provided new theoretical thinking for the study of thrusting tectonics in Daqingshan area.
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References
[1] |
王建平,杨玉东.大青山地区的冲断和推覆[J].中国地质科学院地质力学研究所所刊,1893, 4:43-57.
Google Scholar
|
[2] |
王建平,杨玉东.大青山及邻区冲断推覆构造形成机制的论讨[J].构造地质论丛,1986, 6:1-16.
Google Scholar
|
[3] |
郑亚东, Davis G A,王琮,等.内蒙古大青山大型逆冲推覆构造[J].内蒙古地质,1998, 4:13-19.
Google Scholar
|
[4] |
刘正宏,徐仲元,杨振升.论内蒙古大青山地区逆冲推覆构造[J].中国区域地质,1999,18(4):366-372.
Google Scholar
|
[5] |
刘正宏,徐仲元,杨振升.大青山逆冲推覆体系含义及地质特征[J]. 世界地质,2001,20(3):224-230.
Google Scholar
|
[6] |
徐仲元,刘正宏,杨振升.内蒙古大青山地区中生代造山运动及构造演化[J].长春科技大学学报,2001,31(4):317-322.
Google Scholar
|
[7] |
朱绅玉.内蒙古色尔腾山-大青山地区推覆构造[J].内蒙古地质, 1997, 1:41-47.
Google Scholar
|
[8] |
陈志勇,温长顺,张维杰.内蒙古色尔腾山的推覆构造[J].地球科学, 2000,25(3):237-242.
Google Scholar
|
[9] |
陈志勇,李玉玺,王新亮,等.包头-呼和浩特北部地区逆冲推覆构造[J].地质通报,2002,21(4/5):251-258.
Google Scholar
|
[10] |
Jackson S E,Pearson N J,Griffin W L,et al.The application of laser ablation-inductively coupled plasma-mass spectrometry to in site U-Pb zircon geochronology[J].Chemical Geology,2004,211:47-69.
Google Scholar
|
[11] |
Liu Y S,Gao S,Hu Z C,et al.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans North China Orogen:U-Pb dating,Hf is otopes and trace elements in Zircons from mantle xen oliths[J].Journal of Petrology,2009,51:537-571.
Google Scholar
|
[12] |
Ludwig K R.User's manual for Isoplot/Ex,version 3.00[M]//A Geochronological Toolkit for Microsoft Excel:Berkeley Geochronology Center Special Publication.2003,4:1-70.
Google Scholar
|
[13] |
Anderson T. Correction of com mon lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1/2):59-79.
Google Scholar
|
[14] |
翟明国,胡波,彭澎,等.华北中-新元古代的岩浆作用与多期裂谷事件[J].地学前缘,2014,21(1):100-119.
Google Scholar
|
-
-
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