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川北旺苍地区梁山组碎屑锆石物源分析及其大地构造背景

魏曦 邢凤存 古强 赵文瑜

沉积与特提斯地质2026,Vol.46Issue(1):17-36,20.
沉积与特提斯地质2026,Vol.46Issue(1):17-36,20.DOI:10.19826/j.cnki.1009-3850.2025.05003

川北旺苍地区梁山组碎屑锆石物源分析及其大地构造背景

Provenance analysis of detrital zircons from the Liangshan Formation in Wangcang area,northern Sichuan,and its geotectonic setting

魏曦 1邢凤存 2古强 2赵文瑜1

作者信息

  • 1. 成都理工大学 油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学 自然资源部深时地理环境重建与应用重点实验室,四川 成都 610059||成都理工大学地球与行星科学学院,四川 成都 610059
  • 2. 成都理工大学 油气藏地质及开发工程全国重点实验室,四川 成都 610059||成都理工大学 自然资源部深时地理环境重建与应用重点实验室,四川 成都 610059||成都理工大学沉积地质研究院,四川 成都 610059
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摘要

Abstract

The Early Permian is an important tectonic transition period for the Yangtze Block.This study explores the provenance and geotectonic setting of the Lower Permian Liangshan Formation in the Wangcang area of north Sichuan Basin,based on the geological survey,U-Pb dating,and trace element analysis of detrital zircons.Results show that:(1)Most of the detrital zircons from the Liangshan Formation in the Wangcang area have rounded shapes,clear zoning,and Th/U ratios between 0.01 and 2.9,enrichment of heavy rare earth elements,depletion of light rare earth elements,positive Ce anomalies,and negative Eu anomalies.Their U-Pb ages are mainly distributed in four intervals:1 100-850 Ma,850-700 Ma,600-500 Ma,and 500-400 Ma.(2)The detrital zircons of the Liangshan Formation are mostly of magmatic origin,with sources mainly derived from granitic and mafic rocks.The geotectonic setting of the source area is inferred as an island arc,with three stages of crustal thinning and two stages of thickening during 1 000-400 Ma.(3)The geotectonic setting of the Liangshan Formation in the study area reflects a collision-dominated environment transitioning to extensional,with primary provenance from recycled underlying sedimentary strata and the northern Hannan-Micangshan micro-block.No external plate sources are evident.Compared to southern Guizhou,the Wangcang detrital zircon ages are more diverse,indicating regional differences in provenance.This study establishes the detrital zircon age spectrum of the Liangshan Formation in the northwestern margin of the Upper Yangtze Block,clarifies its provenance and tectonic setting characteristics,and provides a basis for reconstructing Early Permian paleogeography and geotectonic evolution of the Yangtze Block.

关键词

四川盆地北部/下二叠统梁山组/碎屑锆石U-Pb定年/物源分析/大地构造背景

Key words

northern Sichuan Basin/Lower Permian Liangshan Formation/detrital zircon U-Pb dating/provenance analysis/geotectonic setting

分类

天文与地球科学

引用本文复制引用

魏曦,邢凤存,古强,赵文瑜..川北旺苍地区梁山组碎屑锆石物源分析及其大地构造背景[J].沉积与特提斯地质,2026,46(1):17-36,20.

基金项目

国家自然科学基金项目(41672103,41302089) (41672103,41302089)

沉积与特提斯地质

1009-3850

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