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主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    阿拉伯地盾地质构造演化与关键地质矿产问题浅析

    查显锋, 计文化, 辜平阳, 吕鹏瑞, 王国强, 陈锐明, 康磊, 李猛, 孙吉明, 荆德龙, 王凯, 罗克勇

    查显锋, 计文化, 辜平阳, 等. 阿拉伯地盾地质构造演化与关键地质矿产问题浅析[J]. 西北地质, 2023, 56(5): 204-213. DOI: 10.12401/j.nwg.2023075
    引用本文: 查显锋, 计文化, 辜平阳, 等. 阿拉伯地盾地质构造演化与关键地质矿产问题浅析[J]. 西北地质, 2023, 56(5): 204-213. DOI: 10.12401/j.nwg.2023075
    ZHA Xianfeng, JI Wenhua, GU Pingyang, et al. Tectonic Evolution and Key Geological Mineral Issues of Arabian Shield[J]. Northwestern Geology, 2023, 56(5): 204-213. DOI: 10.12401/j.nwg.2023075
    Citation: ZHA Xianfeng, JI Wenhua, GU Pingyang, et al. Tectonic Evolution and Key Geological Mineral Issues of Arabian Shield[J]. Northwestern Geology, 2023, 56(5): 204-213. DOI: 10.12401/j.nwg.2023075

    阿拉伯地盾地质构造演化与关键地质矿产问题浅析

    基金项目: 沙特地质调查局国际合作项目“Detailed Geological Mapping of the Arabian Shield, Kingdom of Saudi Arabia”(RFP#SGS-411-007),中国地质调查局项目(DD20221636),国家自然科学基金项目(92055314)和陕西省自然科学基金项目(2023-JC-YB-249)联合资助。
    详细信息
      作者简介:

      查显锋(1984−),男,高级工程师,从事构造地质学与区域地质调查工作。E–mail:zha_xianfeng@126.com

    • 中图分类号: P541;P544

    Tectonic Evolution and Key Geological Mineral Issues of Arabian Shield

    • 摘要:

      阿拉伯地盾位于阿拉伯板块的西南部,与红海西岸的努比亚地盾共同组成努比亚−阿拉伯地盾,是新元古代东、西冈瓦纳大陆汇聚过程中形成的泛非造山带的重要组成部分。在“沙特阿拉伯地盾精细地质填图”技术标编制过程中,笔者综合分析了该区的地质调查和研究成果,总结了阿拉伯地盾8个次级地体、主要蛇绿岩构造混杂岩带及新元古代沉积盆地的地质特征,并将阿拉伯地盾的地质演化细分为4个构造演化阶段。其中,在新元古代洋−陆转化过程中阿拉伯地盾形成了一系列重要的矿产资源。在此基础上,系统梳理了区内地层、构造、岩浆作用及与成矿相关的地质问题,提出了未来精细地质填图过程中的工作建议。

      Abstract:

      The Arabian Shield, located in the southwestern Arabian Plate, constitutes the Nubia–Arabian Shield with the Nubia to the west of the Red Sea, and is an important part of the Pan–Africa Orogeny that formed during the convergence of eastern and western Gondwana in Neoproterozoic. During compiling the technical bid of “Detailed Geological Mapping of the Arabian Shield, Kingdom of Saudi Arabia”, both progress on geological survey and researches of the Arabian Shield has been comprehensively analyzed. The geological structure of the Arabian Shield is characterized by eight terrenes and ophiolitic mélange zones or shearing zones between them, and is overlain by Neoproterozoic sedimentary basins. Based on these analyses, the tectonic evolution of the Arabian Shield can be classified into four tectonic stages, and a series of metal deposits have been formed during the ocean–continent tectonic transformational process in Neoproterozoic. Moreover, the geological problems related to strata, magmatism, tectonic evolution, and mineralization of the Arabian Shield have been sorted out, as well as suggestions have been put forward for the detailed geological mapping in the future.

    • 图  1   阿拉伯板块大地构造位置图(a)(据Stern et al.,2010)和阿拉伯地盾构造单元划分图(b)(据Johnson et al.,2011Surour et al.,2014Abd-Allah et al.,2014Hamimi et al.,2014El-Sawy et al.,2019Abuamarah,2020

      1. 地体名称及年代学(单位为Ma);2. Jibalah拉分盆地;3. Murdama碰撞后磨拉石盆地;4. 蛇绿构造混杂带及名称;5. 蛇绿岩;6. 边界断裂;7. 主要断裂;①. Qazaz剪切带;②. Ar Rika断裂;③.Halaban–Zarghat断裂;④. Ruwah断裂;⑤. Nabitah断裂;⑥. Junaynah断裂;⑦. Umm Farwah剪切带;⑧. Al Amar断裂;⑨. Ad Damm断裂带;⑩. Sukhaybarat断裂

      Figure  1.   (a) Tectonic location of the Arabian Plate and (b) tectonic divisions for the Arabian Shield

      图  2   新元古代阿拉伯地盾东部构造格局示意图(据Doebrich et al.,2007修改)

      Figure  2.   Schematic diagram showing tectonic framework of the eastern Arabian Shield

      图  3   阿拉伯–努比亚地盾构造背景及缝合带和断裂带对比图(据Stern et al.,2010Abd-Allah et al.,2014修改)

      Figure  3.   Tectonic setting of the Arabian–Nubian Shield showing the comparison of sutures and faults

      图  4   Fatima缝合带形成过程示意图(据Abd-Allah et al.,2014

      a. Fatima蛇绿岩形成;b. Jiddah和Asir地体碰撞形成增生楔

      Figure  4.   Schematic cartons showing formation of Fatima suture zone

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    • 收稿日期:  2022-12-09
    • 修回日期:  2023-04-09
    • 网络出版日期:  2023-04-27
    • 刊出日期:  2023-10-19

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