吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 425-441.doi: 10.13278/j.cnki.jjuese.20190292

• 沉积盆地分析 • 上一篇    下一篇

大兴安岭南段阿鲁科尔沁旗地区林西组沉积环境特征及其时限的地质意义

董清水1, 何春生1, 楼仁兴1,2, 任锡钢2, 张超3, 张渝金3, 许圣传4   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林大学应用技术学院, 长春 130012;
    3. 中国地质调查局沈阳地质调查中心, 沈阳 110034;
    4. 河北地质大学资源学院, 石家庄 050031
  • 收稿日期:2019-10-20 出版日期:2020-03-26 发布日期:2020-03-31
  • 通讯作者: 楼仁兴(1987-),男,讲师,主要从事沉积学与石油地质学方面的研究,E-mail:lourenxing@jlu.edu.cn E-mail:lourenxing@jlu.edu.cn
  • 作者简介:董清水(1963-),男,教授,博士,主要从事沉积学与石油地质学方面的研究,E-mail:dqs9518@163.com
  • 基金资助:
    国家自然科学基金项目（41972105）；中国地质调查局项目（DD20190042-03，DD20190039-06）

Geological Significance of Sedimentary Environment Characteristics and Time Limit of Linxi Formation in Arhorchin Banner, Southern Great Xing’an Range

Dong Qingshui1, He Chunsheng1, Lou Renxing1,2, Ren Xigang2, Zhang Chao3, Zhang Yujin3, Xu Shengchuan4   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. College of Applied Technology, Jilin University, Changchun 130012, China;
    3. Shenyang Center, China Geological Survey, Shenyang 110034, China;
    4. College of Resources, Hebei GEO University, Shijiazhuang 050031, China
  • Received:2019-10-20 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Natural Science Foundation of China(41972105)and Project of China Geological Survey(DD20190042-03,DD20190039-06)

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摘要： 针对兴蒙—松嫩地区林西组沉积环境、沉积时限及古亚洲洋最终闭合时间等争议问题，通过对阿鲁科尔沁旗罕庙地区林西组的岩性、古生物、微量元素及碎屑锆石U-Pb测年等综合研究认为：林西组发育淡水双壳类和叶肢介化石，微量元素Sr/Ba值主要分布在0.05~0.18之间（平均值为0.12），B/Ga值主要分布在1.84~3.22之间（平均值为2.50），V/Cr值介于1.36~2.21之间（平均值为1.81），其沉积时期应为缺氧或贫氧的淡水湖泊环境。结合林西组砂岩碎屑锆石具有多时代物源特征、最年轻年龄为251 Ma、沉积下限年龄为晚二叠世等特征推测，古亚洲洋在研究区的最终闭合时限应为中二叠世末期，晚二叠世时期研究区即已转化为陆相沉积。

关键词: 林西组, 沉积环境, 沉积时限, 古亚洲洋, 大兴安岭南段

Abstract: Aiming at the controversial issues such as the sedimentary environment, time-limit of Linxi Formation, and the final closing time of the Paleo-Asian Ocean in Xingmeng-Songnen area,a comprehensive analysis was conducted for the lithology and paleontology of Linxi Formation in Hanmiao area of Arhorchin Banner, in particular,the trace elements, and the U-Pb dating of detrital zircon. The ratio of trace elements Sr/Ba is mainly distributed between 0.05 and 0.18 (average 0.12), the ratio of B/Ga is mainly distributed between 1.84 and 3.22 (average 2.50), and the V/Cr value is between 1.36 and 2.21 (average 1.81), which indicate that the sedimentary period of Linxi Formation was an anoxic freshwater lake environment. The freshwater bivalves and leaf-lime fossils are developed in Linxi Formation. The sandstone clastic zircons of Linxi Formation have multi-epoch provenance. The youngest age is 251 Ma, reflecting the lower sedimentary age in Late Permian. Based on the above characteristics, it can be inferred that the final closing time of the Paleo-Asian Ocean in the study area is the end of the Middle Permian, and the study area transformed into continental sediments during the Late Permian.

Key words: Linxi Formation, sedimentary environment, sedimentary time-limit, Paleo-Asian Ocean, Southern Great Xing'an ranges

中图分类号: 

  • P588.2
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