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准噶尔盆地西北缘石炭系火山岩地球化学特征及其成因机制

牛花朋 何晓 刘姗 焦小芹 张关龙 王千军 周健 赵贤 于洪洲 熊峥嵘

现代地质2025,Vol.39Issue(3):588-597,10.
现代地质2025,Vol.39Issue(3):588-597,10.DOI:10.19657/j.geoscience.1000-8527.2025.039

准噶尔盆地西北缘石炭系火山岩地球化学特征及其成因机制

Geochemical Characteristics and Petrogenesis of Carboniferous Volcanic Rocks in the Northwestern Margin of the Junggar Basin

牛花朋 1何晓 1刘姗 1焦小芹 2张关龙 3王千军 3周健 3赵贤 1于洪洲 3熊峥嵘3

作者信息

  • 1. 中国石油大学(北京)油气资源与工程全国重点实验室,北京 102249||中国石油大学(北京)地球科学学院,北京 102249
  • 2. Department of Geosciences,University of Padova,Padua,Italy
  • 3. 中国石油化工股份有限公司胜利油田分公司勘探开发研究院,山东东营 257015
  • 折叠

摘要

Abstract

This study investigates Carboniferous volcanic rocks(basalt,basaltic andesite,and andesite)from the Hara Arat Mountain(Hashan)area on the northwestern margin of the Junggar Basin to elucidate their petro-genesis and tectonic setting.Results indicate that these three rock types exhibit moderate MgO content(3.21%-6.82%),moderate to high Al2O3 content(11.30%-17.78%),and elevated total alkali content(K2O+Na2O=4.24%-7.24%).Basalt samples show relatively low K2O content,reflecting Na-enrichment relative to K,and are classified as low-K tholeiitic basalts.In contrast,basaltic andesites and andesites display high calc-alkaline element contents,consistent with island arc volcanic rock characteristics.Isotopic analyses reveal medium-low 87Sr/86Sr ratios(0.702877-0.706620)and high εNd(t)values(+4.59 to+9.85),indicating magma interaction between crustal and mantle components in a deep magma chamber.Compared to basalts,ba-saltic andesites and andesites show enrichment in large ion lithophile elements(e.g.,Ba),relative enrichment in high field strength elements(e.g.,U,Pb),and depletion in Nb,typical of subduction-related island arc magmatism.Trace element and rare earth element patterns suggest that basalts originated from depleted mantle melts under a convergent tectonic regime,while intermediate volcanic rocks record the subduction of oceanic plates beneath continental plates.This process involved the replacement of the depleted mantle wedge by sedi-ments or melts derived from the dehydrating subducting slab,followed by partial melting to form basaltic andes-ites and andesites.Combined with regional geological data,the subduction of the oceanic plate persisted until the late Carboniferous.

关键词

准噶尔盆地/哈山/石炭系/火山岩/岩石成因

Key words

Junggar Basin/Hashan/Carboniferous/volcanic rock/petrogenesis

分类

天文与地球科学

引用本文复制引用

牛花朋,何晓,刘姗,焦小芹,张关龙,王千军,周健,赵贤,于洪洲,熊峥嵘..准噶尔盆地西北缘石炭系火山岩地球化学特征及其成因机制[J].现代地质,2025,39(3):588-597,10.

基金项目

中国石油大学(北京)2024年度"学科前沿交叉探索专项"(2462024XKQY004) (北京)

国家科技重大专项(2024ZD14049-004) (2024ZD14049-004)

中国石油化工股份公司项目(P22067). (P22067)

现代地质

OA北大核心

1000-8527

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