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内蒙古科尔沁右翼中旗晚古生代碎屑锆石定年及其意义
引用本文:张辰昊,寇晓威,颜林杰,徐 备.内蒙古科尔沁右翼中旗晚古生代碎屑锆石定年及其意义[J].地质通报,2015,34(8):1482-1492.
作者姓名:张辰昊  寇晓威  颜林杰  徐 备
作者单位:1.北京大学造山带和地壳演化教育部重点实验室/北京大学地球与空间科学学院,北京100871;2.吉林省第三地质调查所,吉林 四平136000
基金项目:国家重点基础研究发展计划(编号:2013CB429806)和中国地质调查局项目(编号:1212011220906)
摘    要:对科尔沁右翼中旗地区晚古生代地层进行碎屑锆石U-Pb定年研究。样品130909-01为凝灰质砂岩,130910-15为岩屑石英砂岩。碎屑锆石年龄可分为4组,由新到老依次为:252~278Ma、286~359Ma、381~462Ma和500Ma之前。碎屑锆石的最小年龄(256.5±1.7Ma)限定了地层沉积下限为晚二叠世。样品中出现大量残留锆石,记录了前寒武纪基底、早古生代岛弧岩浆岩和石炭纪—二叠纪岩浆活动事件。

关 键 词:碎屑锆石  科尔沁右翼中旗  晚古生代

Dating of late Paleozoic detrital zircon in Horqin Right Wing Middle Banner of Inner Mongolia and its significance
ZHANG Chenhao,KOU Xiaowei,YAN Linjie,XU Bei.Dating of late Paleozoic detrital zircon in Horqin Right Wing Middle Banner of Inner Mongolia and its significance[J].Geologcal Bulletin OF China,2015,34(8):1482-1492.
Authors:ZHANG Chenhao  KOU Xiaowei  YAN Linjie  XU Bei
Abstract:The detrital zircon U-Pb geochronology of the Late Paleozoic strata in Horqin Right Wing Middle Banner was studied in this paper. Sample 130909-01 and 130910-15 were tuffaceous sandstone and lithic quartz sandstone samples, respectively. The detrital zircon ages can be divided into four groups: 252~278Ma, 286~359Ma, 381~462Ma and older than 500Ma. The youngest zircon age (256.5±1.7Ma) constrains the maximum sedimentary age of the Late Permian. A large number of relict zircons were existent in the samples, which kept a record of Precambrian basement, early Paleozoic arc magmatic rocks and magmatic activity event during Permian-Carboniferous period.
Keywords:detrital zircons  Horqin Right Wing Middle Banner  Late Paleozoic
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