河北地区中生代标准地层剖面侏罗系/白垩系界线——SHRIMP锆石U-Pb年龄标定

    A discussion on Jurassic and Cretaceous boundary based on the SHRIMP zircon U-Pb dating of Mesozoic holitype section in Luanping basin

    • 摘要: 在全国地层委员会组织的滦平盆地中生代地层野外考察中,采集了大北沟组凝灰岩样品,其锆石年龄测定结果引发对陆相侏罗系/白垩系界线的思考。冀北滦平地区陆相侏罗系-白垩系发育,各类陆相生物化石极丰富,地层产出大量火山凝灰岩层,是通过岩石地层、生物地层、同位素测年和磁性年代地层综合研究侏罗系/白垩系界线的理想地区。根据生物地层研究,冀北滦平盆地侏罗系/白垩系界线附近的地层为大北沟组和大店子组。根据冀北-辽西地区同位素测年数据,侏罗系/白垩系界线年龄倾向于130Ma。获得榆树下标准剖面大北沟组顶部凝灰岩(斑脱岩)SHRIMP锆石U-Pb同位素年龄为129.9±1.1Ma。

       

      Abstract: This paper is the record of a field investigation of Mesozoic strata in Luanping County, Hebei Province, which was organized by the Commission on Stratigraphy of China. A tuff sample was collected in the Dabeigou Formation at the top of the Jurassic strata. According to the chronostratigraphic dating, the authors think over the terrestrial Jurassic/Cretaceous boundary based on the tuff zircon dating. The terrestrial Jurassic and Cretaceous strata are well developed in Luanping County, Hebei Province. Various terrestrial fossils are very abundant with a large amount of tuffeous rocks. It is an ideal province for the study of Jurassic/Cretaceous boundary and the Dabeigou Formation and Dadianzi Formation based comprehensively on lithogical stratigraphy, biostratigraphy, chronostratigraphy and magnetostratigraphy. According to the chronostratigraphy, the boundary age of Jurassic/Cretaceous tends to favor the era of 130Ma. This paper reports a SHRIMP U-Pb age of 129.9±1.1Ma for tuff of the holitype section of the Dabeigou Formation from Yushuxia Village, Luanping County.

       

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