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程海峰,徐旭明,刘广,段炳鑫,徐翠,管诰.内蒙古北山地区盘陀山一带长城纪古硐井群碎屑锆石LA-ICP-MS U-Pb年龄及其地质意义[J].地质通报,2017,(8):1385-1392.
内蒙古北山地区盘陀山一带长城纪古硐井群碎屑锆石LA-ICP-MS U-Pb年龄及其地质意义    点此下载全文
程海峰1  徐旭明1  刘广1  段炳鑫1  徐翠1  管诰2
1. 河北省区域地质矿产调查研究所, 河北 廊坊 065000;
2. 有色金属矿产地质调查中心新疆地质调查所, 新疆 乌鲁木齐 830011
基金项目:中国地质调查局项目《内蒙古1:5万1524.6高地、二龙包西、1580.8高地、炮台山西幅区域地质矿产调查》(编号:1212011220464)
DOI:
摘要:
      长城纪古硐井群作为内蒙古北山地区古老褶皱基底之上的第一个沉积盖层,尚未获得可靠的年龄资料,前人只是根据其产出的层位和岩石组合特征与燕山地区的长城系对比后,将其置于中元古代长城纪。对古硐井群变质长石石英砂岩中碎屑锆石进行了LA-ICP-MS U-Pb测年,结果显示,锆石207Pb/206Pb年龄数据90%介于1.3~2.2Ga之间,其余年龄介于2.4~3.2Ga之间,峰期在1.6~2.0Ga之间,最年轻的碎屑锆石207Pb/206Pb年龄为1393±50Ma。通过对比碎屑锆石的年龄频谱和周围古地块的形成时代,碎屑锆石的U-Pb年龄限制了古硐井群的沉积时代,应为中元古代蓟县纪,古硐井群的沉积物可能来自北山-阿拉善和塔里木-敦煌地块。
关键词:碎屑锆石  LA-ICP-MS U-Pb年龄  古硐井群  内蒙古北山  盘陀山
LA-ICP-MS U-Pb geochronology of detrital zircons from the Gudongjing Complex-Group in Pantuoshan area of Beishan region within Inner Mongolia during Changchengian Period and its geological significance    Download Fulltext
CHENG Haifeng1  XU Xuming1  LIU Guang1  DUAN Bingxin1  XU Cui1  GUAN Gao2
1. Regional Geological and Mineral Resources Survey Institute of Hebei Province, Langfang 065000, Hebei, China;
2. Xinjiang Geological Survey, CNGS, Urumqi 830011, Xinjiang, China
Fund Project:
Abstract:
      Changchengian Period Gudongjing Complex-Group serves as the first sedimentary cover on the ancient folded base-ment in Beishan region of Inner Mongolia, but without reliable dating data. Previous researchers assigned it to Mesoproterozoic Changchengian Period only on the basis of the contrast with the Changchengian system of the Yanshan area in such aspects as for-mation layers and rock association characteristics. In this paper, the LA-ICP-MS zircon U-Pb method was used for the determi-nation of the age of the detrital zircon in metamorphic quartz sandstone of the Gudongjing Complex-Group, and the test results show that the 90% ages of zircon 207Pb/206Pb data are 1.3~2.2Ga, the rest of ages are 2.4~3.2Ga, peak period ages are 1.6~2.0Ga, and the youngest 207Pb/206Pb age of detrital zircon is 1393±50Ma. Based on comparing the age spectrum of the detrital zircon with the formation age of the surrounding massif, the dertital zircon limits the sedimentary age of the Gudongjing Complex-Group as the Mesoproterozoic Jixianian Period. The sediments of the Gudongjing Complex-Group might have come from Beishan-Alxa and Tarim-Dunhuang blocks.
Keywords:detrital zircon  LA-ICP-MS U-Pb ages  Gudongjing Complex-Group  Beishan area of Inner Mongolia  Pantuoshan area
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