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引用本文:申亮,赵胜金,于海洋,柳志辉,周颖帅,张猛,朴丽丽. 大兴安岭哈达陶勒盖组火山岩年龄、地球化学特征及其陆缘弧构造背景[J]. 中国地质, 2020, 47(4): 1041-1055.
SHEN Liang,ZHAO Shengjin,YU Haiyang,LIU Zhihui,ZHOU Yingshuai,ZHANG Meng,PIAO Lili. Zircon age and geochemical characteristics of Hadataolegai Formation volcanic rocks in Da Hinggan Mountains and its continental marginal arc setting[J]. Geology in China, 2020, 47(4): 1041-1055(in Chinese with English abstract).
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大兴安岭哈达陶勒盖组火山岩年龄、地球化学特征及其陆缘弧构造背景
申亮1, 赵胜金2,3,4, 于海洋2,3, 柳志辉2,3, 周颖帅2,3, 张猛2,3, 朴丽丽2,3
1.中国地质调查局发展研究中心, 北京 100037;2.内蒙古自治区第十地质矿产勘查开发院, 内蒙古 赤峰 024005;3.内蒙古第十地质矿产勘查开发有限责任公司, 内蒙古 赤峰 024005;4.中国地质大学(北京)地球科学与资源学院, 北京 100083
摘要:
根据野外调查,将大兴安岭北段新巴尔虎右旗地区的一套火山岩归属为哈达陶勒盖组。通过SHRIMP锆石U-Pb测年,获得哈达陶勒盖组绿帘石化安山岩的年龄加权平均值为(254.3±7.9)Ma(MSWD=4.7),结合区域地层对比,将该组的形成时代置于早三叠世。根据元素地球化学分析,可将哈达陶勒盖组火山岩划分为中基性和酸性火山岩两类。其中,中基性火山岩岩浆可能来源于受俯冲作用影响的岩石圈地幔,并遭受到地壳物质的混染;而酸性火山岩岩浆则形成于地壳。结合区域地质特征,通过构造环境判别,该组火山岩的形成可能与蒙古—鄂霍茨克板块向南俯冲引起的陆缘弧背景密切相关。哈达陶勒盖组的厘定丰富了大兴安岭北段地层层序,也为大兴安岭地区区域构造演化和岩浆活动提供了证据。
关键词:  锆石U-Pb测年  哈达陶勒盖组  陆缘弧背景  蒙古-鄂霍茨克缝合带  大兴安岭
DOI:10.12029/gc20200410
分类号:P597
基金项目:中国地质调查局项目(DD20160048-15、12120114086201、DD20190405和DD20190406)资助。
Zircon age and geochemical characteristics of Hadataolegai Formation volcanic rocks in Da Hinggan Mountains and its continental marginal arc setting
SHEN Liang1, ZHAO Shengjin2,3,4, YU Haiyang2,3, LIU Zhihui2,3, ZHOU Yingshuai2,3, ZHANG Meng2,3, PIAO Lili2,3
1.Development and Research Center of China Geological Survey, Beijing 100037, China;2.No. 10 Institute of Geological Exploration, Inner Mongolia Bureau of Geology and Mineral Resources, Chifeng 024005, Inner Mongolia, China;3.Inner Mogolia Tenth Geological Mineral Exploration and Development Co., Ltd., Chifeng 024005, Inner Mongolia;4.School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
Abstract:
A series of volcanic rocks, such as basalt, andesite and rhyolite, were determined in Xin Barag Right Banner of northern Da Hinggan Mountains. Geological survey reveals that these volcanic rocks should be assigned to Hadataolegai Formation. SHRIMP zircon U-Pb dating indicates that the epidotized andesite from Hadataolegai Formation was formed at(254.3±7.9)Ma(MSWD=4.7). According to geochemical researches, these volcanic rocks of Hadataolegai Formation can be divided into two types, i.e., intermediate-basic rocks and acidic rocks. The magma of intermediate-basic rocks was derived from the lithospheric mantle affected by the southward subduction of Mongolia-Okhotsk plate. The acidic volcanic rocks have a crustal-derived magma source features. Based on tectonic setting analysis, the authors hold that the Hadataolegai Formation volcanic rocks were formed under the continental marginal arc environment and related to southward subduction of Mongolia-Okhotsk plate. The determination of Hadataolgegai Formation improves the stratigraphic sequence of northern Da Hinggan Mountains and provides a favorable evidence for regional tectonic evolution of Da Hinggan Mountains.
Key words:  zircon U-Pb ages  Hadataolegai Formation  continental marginal arc setting  Mongolia-Okhotsk suture  Da Hinggan Mountains