| 内蒙古西部银根-额济纳旗盆地及邻区二叠纪火山岩的地球化学特征和构造环境 |
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| 引用本文： | 党 犇1,2, 赵 虹1,2, 林广春1,2, 仵康林1, 康晓燕1, 葛海影1, 吴 斌1, 刘少红1. 内蒙古西部银根-额济纳旗盆地及邻区二叠纪火山岩的地球化学特征和构造环境[J]. 地质通报, 2011, 30(06): 923-931. |
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| 作者姓名： | 党 犇1 2 赵 虹1 2 林广春1 2 仵康林1 康晓燕1 葛海影1 吴 斌1 刘少红1 |
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| 作者单位： | 1. 长安大学地球科学与资源学院, 陕西 西安 710054;2. 西部矿产资源与地质工程教育部重点实验室, 陕西 西安 710054 |
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| 摘 要： | 银-额（银根-额济纳旗）盆地及其邻区二叠纪火山岩分布广泛，目前对其成因和构造背景研究还很薄弱。对该区火山岩岩石学和元素地球化学特征进行研究，为恢复二叠纪盆地性质与古构造环境提供了岩石地球化学约束。分析的二叠纪火山岩主要岩石类型为玄武岩、玄武安山岩和安山岩，显示亚碱性系列的特征。Mg#介于0.53～0.86之间，高场强元素Nb、Ta、Ti明显亏损，岩石轻度富集轻稀土元素(LREE)，(La/Yb)N=1.68~6.10，Eu亏损不明显(δEu=0.64～0.99)，稀土元素配分曲线右倾较缓。总体上既显示了板内构造环境的特征，又具有俯冲带地球化学的印记。综合沉积建造特征和邻区的研究结果，认为银-额盆地二叠纪火山岩形成于板内裂谷环境，且很可能与地幔柱事件有关，岩浆在上升过程中受到地壳物质不同程度的混染。
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| 关 键 词： | 二叠纪 火山岩 地球化学 构造环境 额济纳旗地区 |
Geochemistry and tectonic setting of Permian volcanic rocks in Yingen-Ejin Banner basin and its neighboring areas,western Inner Mongolia |
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| DANG Ben1,2, ZHAO Hong1,2, LIN Guang-chun1,2, WU Kang-lin1,KANG Xiao-yan1, GE Hai-ying1, WU Bin1, LIU Shao-hong1. Geochemistry and tectonic setting of Permian volcanic rocks in Yingen-Ejin Banner basin and its neighboring areas, western Inner Mongolia[J]. Geological Bulletin of China, 2011, 30(06): 923-931. |
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| Authors: | DANG Ben1 2 ZHAO Hong1 2 LIN Guang-chun1 2 WU Kang-lin1 KANG Xiao-yan1 GE Hai-ying1 WU Bin1 LIU Shao-hong1 |
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| Affiliation: | 1. College of Earth Sciences and Resources, Chang′an University, Xi′an 710054, Shaanxi, China; 2. Key Laboratory of Western China′s Mineral Resources and Geological Engineering,Ministry of Education, Xi′an 710054, Shaanxi, China |
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| Abstract: | Permian volcanic rocks are widespread in Yingen-Ejin Banner basin and its neighboring areas, and their genesis and tectonic setting remain a problem of much controversy. Based on a petrologic and geochemical analysis of Permian volcanic rocks in the study area, this paper attempts to clarify the palaeo-tectonic setting and provides independent evidence for understanding the nature of the basin. The volcanic rocks are dominated by basalts, basaltic-andesite and andesite, which fall into the sub-alkaline series. Mg# content of this suite ranges from 0.53 to 0.86, exhibiting strong depletion of the high field strength elements Nb, Ta and Ti and slight enrichment of LREE. In terms of REE, (La/Yb)N content ranges from 1.68 to 6.10, showing insignificant Eu depletion (δEu=0.64～0.99) and slightly right-oblique REE distribution patterns. These data show not only the characteristics of an intraplate setting on the whole but also the signature of a subduction zone. Combined with the sedmentary formation characteristics, the authors have reached the conclusion that the Permian magmatic activity of the study area was generated in an intraplate setting, with variable degrees of contamination of the crust during magmatic ascending, related probably to the mantle plume event. |
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| Keywords: | Permian volcanic rocks geochemistry tectonic setting Ejin Banner area |
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