首页|中-新元古界标准剖面蓟县系首获高精度年龄制约——蓟县剖面雾迷山组和铁岭组斑脱岩锆石SHRIMP U-Pb同位素定年研究

中-新元古界标准剖面蓟县系首获高精度年龄制约——蓟县剖面雾迷山组和铁岭组斑脱岩锆石SHRIMP U-Pb同位素定年研究

扫码查看
原文链接
  • NETL
  • NSTL
  • 万方数据
  • 维普
近期在蓟县中-新元古界标准剖面铁岭组和雾迷山组首次发现斑脱岩、并测得其锆石SHRIMP U-Pb同位素年龄为～ 1440Ma(1439±14Ma)和～ 1485Ma(1483±13Ma和1487±16Ma),这标志着这条传统的标准剖面上以碳酸盐岩为主体的蓟县系上部的两个重要组,从此也获得了直接的、高精度的锆石U-Pb同位素年龄约束.这是华北中-新元古界标准剖面蓟县系相关地层单位首次获得直接而精确的锆石U-Pb同位素年龄约束,也是在整个华北北缘燕山地区雾迷山组内部首次获得精确的直接定年.这一进展为闻名中外的天津蓟县剖面中-新元古界年代地层格架的正确厘定、以及今后继续作为华北该阶段的标准剖面,并与国内外其他地区相关地层的正确对比等,提供了新的、精确的年代学“锚点”,因而具有重要的科学和实际意义.
The first precise age constraints on the Jixian System of the Meso-to Neoproterozoic Standard Section of China: SHRIMP zircon U-Pb dating of bentonites from the Wumishan and Tieling formations in the Jixian Section, North China Craton
Although known as the Meso-to Neoproterozoic Standard Section of China for more than half a century,the age of the famous Jixian Section (Jixian County,Tianjin City) has been rather poorly constrained,mainly by Rb-Sr and K-Ar ages that have proven unreliable and inaccurate in most cases.In recent years,significant progress has been made in studying the Meso-to Neoproterozoic geochronology of the North China Craton.To date,however,only one accurate U-Pb zircon age of 1625 ± 6Ma from volcanic rocks of the Dahongyu Formation,and two duplicate zircon U-Pb ages of about 1635Ma from mafic sills crosscutting the Chuanlinggou Formation of the Changchengian System in the lower part of the Jixian Section,has been reported.In addition,no one until now has obtained this kind of age dates directly from carbonate-dominated parts of the succession at the Jixian Section.Fortunately,bentonite beds were recently discovered for the first time in the Tieling and Wumishan formations at the Jixian Section,and ages of ～ 1440Ma (1439 ± 14Ma) and ～ 1485Ma (1483 ± 13Ma and 1487 ± 16Ma) for the bentonite beds were obtained by means of SHRIMP zircon U-Pb dating.This achievement means that the shallow-marine,carbonate-dominated Tieling and Wumishan formations,the upper two stratigraphic units of the conventional Jixian System at the Jixian Standard Section,are now temporally constrained by direct zircon U-Pb dating.Furthermore,it is the first time that the Wumishan Formation from the entirety of the North China Craton has been precisely dated.Moreover,the current SHRIMP zircon age of about 1440Ma for the bentonite in the Tieling Formation at the Jixian Standard Section is the same as the age reported earlier in Pingquan County,Hebei Province,in the east Yanshan Mountains on the northern margin of the NCC.Consequently,this progress in age dating of the bentonite beds in the carbonate-dominated succession provides new,accurate,benchmark ages for further clarification of the chronostratigraphic framework of the well-known Jixian Meso-to Neoproterozoic Standard Section and helps to consolidate its position for correct correlation with relevant strata,both regionally and internationally.

Jixian SectionBentoniteTieling FormationWumishan FormationSHRIMP U-Pb datingMesoproterozoicNorth China Craton

李怀坤、苏文博、周红英、相振群、田辉、杨立公、Warren D HUFF、Frank R ETTENSOHN

展开 >

中国地质调查局天津地质矿产研究所,天津300170

中国地质大学地球科学与资源学院,北京100083

天津市蓟县中上元古界国家自然保护区管理中心,天津301900

Department of Geology, University of Cincinnati, Cincinnati, OH 45221-0013

Department of Earth and Environment Sciences, University of Kentucky, Lexington, KY 40506-0053

展开 >

蓟县剖面 斑脱岩 铁岭组 雾迷山组 SHRIMP U-Pb同位素测年 中元古界 华北克拉通

中国地质调查局项目中国地质调查局项目国家自然科学基金国家自然科学基金

1212011301390012120111201424077207641272046

2014

岩石学报
中国矿物岩石地球化学学会,中国科学院地质地球物理研究所

岩石学报

CSTPCDCSCD北大核心SCI
影响因子：2.74
ISSN：1000-0569
年,卷(期)：2014.30(10)
  • 58
  • 38