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首页|期刊导航|华东地质|扬子陆块西南缘东川大窑湾古元古代晚期辉长岩年代学、地球化学特征及地质意义

扬子陆块西南缘东川大窑湾古元古代晚期辉长岩年代学、地球化学特征及地质意义

胡创 王子正 危隆隆 詹宏宇 李宸 刘宝嵩 魏云虓

华东地质2026,Vol.47Issue(1):82-97,16.
华东地质2026,Vol.47Issue(1):82-97,16.DOI:10.16788/j.hddz.32-1865/P.2025.10.013

扬子陆块西南缘东川大窑湾古元古代晚期辉长岩年代学、地球化学特征及地质意义

Geochronology,geochemical characteristics and geological implications of the Late Paleoproterozoic gabbro in Dayaowan,Dongchuan southwestern margin of the Yangtze Block

胡创 1王子正 2危隆隆 1詹宏宇 1李宸 1刘宝嵩 3魏云虓3

作者信息

  • 1. 成都理工大学 地球与行星科学学院,四川 成都 610059
  • 2. 中国地质调查局成都地质调查中心,四川 成都 610082
  • 3. 西藏大学,西藏 拉萨 850000
  • 折叠

摘要

Abstract

The southwestern margin of the Yangtze Block is extensively intruded by Paleoproterozoic mag-matic rocks;however,significant controversy persists regarding their tectonic setting and dynamic mechanisms.Gabbro,as the direct crystallization product of mafic magma,provides zircon U-Pb isotopic chronology data that can precisely constrain the timing of tectonothermal events.Furthermore,its major and trace element composi-tions effectively record the material exchange and energy transfer processes between the lithosphere and astheno-sphere,offering critical geochemical constraints for discriminating tectonic environments.This paper presents a systematic isotopic chronological and geochemical study of the Dayaowan gabbro in the Dongchuan area.The re-sults show that the zircon U-Pb age of the gabbro is(1 674±16)Ma,indicating its emplacement during the Late Paleoproterozoic.The rock belongs to the subalkaline series,exhibiting flat or slightly right-inclined patterns in chondrite-normalized rare earth element(REE)diagrams.In primitive mantle-normalized trace element spider dia-grams,it displays enrichment in large-ion lithophile elements(LILEs)including Ba,Sr,and La,along with rela-tive depletion in high-field-strength elements(HFSEs)such as Nb,Ta,and Hf.These geochemical characteristics share affinities with both within-plate basalts(WPB)and enriched mid-ocean ridge basalts(E-MORB).Compre-hensive analysis suggests that this magmatic activity likely formed in an intracontinental rift setting associated with mantle plume activity,representing a tectonic-magmatic thermal event response on the southwestern margin of the Yangtze Block during the breakup of the global Columbia Supercontinent.

关键词

大窑湾辉长岩/Columbia超大陆/地球化学/同位素年代学/东川

Key words

Dayaowan gabbro/Columbia Supercontinent/geochemistry/isotopic geochronology/Dongchuan

分类

天文与地球科学

引用本文复制引用

胡创,王子正,危隆隆,詹宏宇,李宸,刘宝嵩,魏云虓..扬子陆块西南缘东川大窑湾古元古代晚期辉长岩年代学、地球化学特征及地质意义[J].华东地质,2026,47(1):82-97,16.

基金项目

中国地质调查局"滇东北铝磷矿大型资源基地综合地质调查(编号:DD20242114)""上扬子西缘成矿带战略性矿产调查(编号:DD20240071)"和四川省科技计划项目"川西甘孜—理塘成矿带金矿成矿规律与富集机制(编号:2024NSF-SC1954)""川西甘孜—理塘金矿带成矿物质来源限定:来自Hg-Ag同位素的联合制约(编号:2025ZNSFSC1196)"项目联合资助. (编号:DD20242114)

华东地质

2096-1871

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