东天山卡拉塔格晚石炭世岛弧火山岩发现的地质意义

马志杰, 柴凤梅, 许强奋, 王雯, 毛启贵, 祁冬梅. 2021. 东天山卡拉塔格晚石炭世岛弧火山岩发现的地质意义. 地质科学, 56(3): 683-700. doi: 10.12017/dzkx.2021.034
引用本文: 马志杰, 柴凤梅, 许强奋, 王雯, 毛启贵, 祁冬梅. 2021. 东天山卡拉塔格晚石炭世岛弧火山岩发现的地质意义. 地质科学, 56(3): 683-700. doi: 10.12017/dzkx.2021.034
Ma Zhijie, Chai Fengmei, Xu Qiangfen, Wang Wen, Mao Qigui, Qi Dongmei. 2021. The discovery of Low-Carboniferous arc volcanic rocks and its tectonic significance at the Kalatag area in the eastern Tianshan. Chinese Journal of Geology, 56(3): 683-700. doi: 10.12017/dzkx.2021.034
Citation: Ma Zhijie, Chai Fengmei, Xu Qiangfen, Wang Wen, Mao Qigui, Qi Dongmei. 2021. The discovery of Low-Carboniferous arc volcanic rocks and its tectonic significance at the Kalatag area in the eastern Tianshan. Chinese Journal of Geology, 56(3): 683-700. doi: 10.12017/dzkx.2021.034

东天山卡拉塔格晚石炭世岛弧火山岩发现的地质意义

  • 基金项目:

    国家自然科学基金联合项目(编号:U1403391)、国家重点研发计划项目(编号:2017YFC0601201)和新疆维吾尔自治区天山青年计划——青年博士科技人才培养项目(编号:2019Q070)资助。

详细信息
    作者简介:

    马志杰,男,1995年生,硕士研究生,矿物学、岩石学、矿床学专业。E-mail:1140301941@qq.com

    通讯作者: 柴凤梅,女,1971年生,博士,教授,矿物学、岩石学、矿床学专业。本文通讯作者。E-mail:chaifengmei@163.com
  • 中图分类号: P584;P588.14+1

The discovery of Low-Carboniferous arc volcanic rocks and its tectonic significance at the Kalatag area in the eastern Tianshan

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  • 东天山大南湖岛弧带内古生代火山岩地层时代一直存在争议,其北部卡拉塔格地区核部火山岩尤为复杂。本研究通过详细的野外工作,在该区识别出一套晚石炭世(299.6±2.1 Ma)流纹岩地层。地球化学研究表明:流纹岩具有高SiO2(75.83%~77.96%)、低Al2O3(10.41%~11.94%)和TiO2(0.30%~0.34%)含量,富钠贫钾(Na2O/K2O=52~215),莱特碱度率(A.R.)为2.84~3.28,属钙碱性低钾系列岩石;所有岩石显示轻微富集大离子亲石元素和轻稀土元素(La/Yb)N=2.12~2.43、亏损髙场强元素Nb、Ta和Ti,并呈现Eu负异常(Eu/Eu*=0.64~0.82),与俯冲相关的钙碱性岛弧岩浆岩特征相似。结合区域研究成果,本文认为该流纹岩是北天山洋向北俯冲过程中岩浆活动的产物,晚石炭世北天山洋尚未闭合。本研究成果为东天山大南湖岛弧带岩浆活动时限和构造演化提供了新资料。
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出版历程
收稿日期:  2021-02-21
修回日期:  2021-04-20
刊出日期:  2021-09-01

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