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贺兰山地区三叠系延长组沉积时限及形成环境:来自凝灰岩与玄武岩锆石U-Pb年龄的约束

张熠埕 张晓磊 赵红格 侯云超 马彪 李星辰 张孙玄琦 王晨杨

地质科学2026,Vol.61Issue(4):1080-1093,14.
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地质科学2026,Vol.61Issue(4):1080-1093,14.DOI:10.12017/dzkx.2026.073

贺兰山地区三叠系延长组沉积时限及形成环境:来自凝灰岩与玄武岩锆石U-Pb年龄的约束

Depositional timing and tectono-sedimentary setting of the Triassic Yanchang Formation in the Helan Mountains:Constraints from zircon U-Pb ages of tuffs and basalts

张熠埕 1张晓磊 2赵红格 1侯云超 2马彪 1李星辰 1张孙玄琦 3王晨杨1

作者信息

  • 1. 西北大学地质学系,大陆演化与早期生命全国重点实验室 西安 710069
  • 2. 中国石油长庆油田分公司勘探开发研究院 西安 710018
  • 3. 淏泰土地规划咨询有限公司 西安 710000
  • 折叠

摘要

Abstract

The Helan Mountains lie along the northwestern margin of the Ordos Basin,where the Triassic Yanchang Formation is widely exposed but still lacks tight geochronologic control.This uncertainty limits regional correlation and hinders reconstruction of depositional systems and basin paleogeography.Here we bracket the depositional interval of the Yanchang Formation using paired zircon U-Pb ages from two thin tuff beds(lower and upper Yanchang)and the basalt that caps the succession.We integrate petrography,whole-rock major and trace element geochemistry,and LA-ICP-MS zircon U-Pb dating,and we use tectonic discrimination diagrams to evaluate magma provenance and tectonic setting.Zircons from the lower and upper tuffs yield weighted mean ages of 244.1±1.7 Ma and 201.9±2.2 Ma,respectively,whereas the youngest magmatic zircons from the capping basalt give ages of 201.5~194.1 Ma.Geochemical signatures indicate that the tuffs were sourced from arc-related,calc-alkaline volcanism,and that the basalt is tholeiitic,derived from an enriched mantle source overprinted by subduction-related modification,yet emplaced during intracontinental extension.Together,these ages constrain deposition of the Yanchang Formation in the Helan Mountains to the Middle-Late Triassic,broadly comparable to the depositional timing of the Yanchang Formation in the basin interior.The combined geochronologic and geochemical data further point to a regional tectonic shift from a subduction-related active continental margin arc setting to post-orogenic intracontinental extension.These results provide a firm temporal framework for stratigraphic correlation and for reconstructing depositional architecture and tectonic evolution along the northwestern Ordos Basin margin.

关键词

贺兰山/延长组/凝灰岩/玄武岩/锆石U-Pb定年/中-晚三叠世

Key words

Helan Mountains/Yanchang Formation/Tuff/Basalt/Zircon U-Pb dating/Middle-Late Triassic

分类

天文与地球科学

引用本文复制引用

张熠埕,张晓磊,赵红格,侯云超,马彪,李星辰,张孙玄琦,王晨杨..贺兰山地区三叠系延长组沉积时限及形成环境:来自凝灰岩与玄武岩锆石U-Pb年龄的约束[J].地质科学,2026,61(4):1080-1093,14.

基金项目

国家自然科学基金重点项目"盆地晚期—后期差异隆升改造及其油气成藏效应——以鄂尔多斯盆地为例"(编号:42230815)和中国石油天然气股份有限公司长庆油田分公司勘探开发研究院科研项目(编号:2025-1305)资助 (编号:42230815)

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