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现代地质 ›› 2022, Vol. 36 ›› Issue (01): 27-47.DOI: 10.19657/j.geoscience.1000-8527.2021.067

• 海洋地质学 • 上一篇    下一篇

塔里木地块西北缘阿克苏地区新元古代冰碛岩年代与冰期事件

李王鹏1(), 王毅1, 李慧莉1, 张仲培1, 刘少峰2, 杨伟利1, 蔡习尧1, 聂海宽1, 钱涛3, 李晓剑4   

  1. 1. 中国石油化工股份有限公司 石油勘探开发研究院,北京 100083
    2. 中国地质大学(北京) 地球科学与资源学院,北京 100083
    3. 中国地质科学院 地质力学研究所,北京 100081
    4. 东华理工大学 地球科学学院,江西 南昌 330013
  • 收稿日期:2021-03-04 修回日期:2021-11-22 出版日期:2022-02-10 发布日期:2022-03-08
  • 作者简介:李王鹏,男,博士,副研究员,1986年出生,构造地质学专业,主要从事含油气盆地构造分析及冰期事件等方面研究。Email: liwp.syky@sinopec.com
  • 基金资助:
    国家自然科学基金项目(41902149);国家自然科学基金项目(41702238);中国石化科技部项目(P17046-3);中国地质科学院基本科研业务费项目(DZLXJK202004)

Geochronology and Glaciation of the Neoproterozoic Diamictite in Aksu Area, Northwestern Margin of the Tarim Block

LI Wangpeng1(), WANG Yi1, LI Huili1, ZHANG Zhongpei1, LIU Shaofeng2, YANG Weili1, CAI Xiyao1, NIE Haikuan1, QIAN Tao3, LI Xiaojian4   

  1. 1. Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083, China
    2. School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
    3. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
    4. School of Earth Sciences,East China University of Technology,Nanchang,Jiangxi 330013,China
  • Received:2021-03-04 Revised:2021-11-22 Online:2022-02-10 Published:2022-03-08

摘要:

塔里木地块新元古代冰期事件等时性对比存在争议,获得可靠的新元古代冰碛岩沉积时代意义重大。塔里木地块西北缘阿克苏地区出露2套新元古代冰碛岩沉积,通过对其进行岩石学、同位素年代学、岩石地球化学等分析,明确其沉积物岩石组合特征、限定其沉积时代、讨论其古气候风化条件等。化学蚀变指数(CIA)指示研究区的2套新元古代冰碛岩代表了2次寒冷的冰川气候记录,分别为巧恩布拉克冰期和尤尔美那克冰期,其中巧恩布拉克冰期中出现2次次级冰期旋回。冰川沉积及其相邻层位的碎屑锆石U-Pb年代学数据显示,塔里木地块西北缘阿克苏地区巧恩布拉克冰期的起始年龄晚于(719±10) Ma;尤尔美那克冰期的起始年龄不会早于(685±11) Ma,其结束年龄可由南华系顶界年龄635 Ma或上覆震旦系苏盖特布拉克组内玄武岩层年龄(615±5) Ma限定。已有年代学、地球化学、沉积学等证据表明:巧恩布拉克冰期(阿克苏地区)与阿勒通沟冰期(库鲁克塔格地区)、江口冰期(华南地区)和Sturtian冰期(国际)相对应,尤尔美那克冰期(阿克苏地区)与特瑞爱肯冰期(库鲁克塔格地区)、南沱冰期(华南地区)和Marinoan冰期(国际)相对应。冰期事件、同位素年代学及地球化学数据可为塔里木地块新元古界的划分与对比提供依据。

关键词: 塔里木地块, 新元古代, 冰碛岩, 碎屑锆石, 化学蚀变指数

Abstract:

Age correlation of the Neoproterozoic glaciation events in the Tarim Block remains controversial, and obtaining reliable deposition time for the Neoproterozoic diamictite is crucial.Two sets of the Neoproterozoic diamictite were developed in Aksu area along the northwestern margin of the Tarim Block. Petrologic and whole-rock geochemical analyses and radiometric dating were conducted to define the sedimentary rock assemblages,deposition time, and paleoclimatic weathering conditions. The chemical index of alteration (CIA) indicates that the Qiaoenbrak and Yuermeinak Formations represent two distinct glaciation episodes, and two secondary glaciation events exist in the Qiaoenbrak glaciation.Detrital zircon U-Pb dating of the glacial deposits and their adjacent beds indicate that the Qiaoenbrak glaciation in Aksu started along the northwestern margin of the TarimBlock after (719±10) Ma, whilst the Yuermeinak glaciation did not start before (685±11) Ma, and its cessation timing can be constrained by the top boundary age of the Nanhua System (635 Ma) or the U-Pb age of the overlying Sinian Sugetbrak Formation basalt (615±5 Ma).Comprehensive analyses of isotope geochronology, geochemistry, and sedimentology indicate that the Qiaoenbrak glaciation (Aksu area) corresponded to the Altungol glaciation (Quruqtagh area), the Jiangkou glaciation (South China), and the Sturtian glaciation (global). Meanwhile, the Yuermeinak glaciation (Aksu area) corresponded to the Tereekan glaciation (Quruqtagh area), the Nantuo glaciation (South China), and the Marinoan glaciation (global). Glaciation, isotopic geochronology, and geochemistry can provide a basis for the division and comparison of the Neoproterozoic sequences in the Tarim Block.

Key words: Tarim Block, Neoproterozoic, diamictite, detrital zircon, chemical index of alteration

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