地震地质 ›› 2019, Vol. 41 ›› Issue (2): 499-520.DOI: 10.3969/j.issn.0253-4967.2019.02.015

• 专题综述 • 上一篇    下一篇

江汉和洞庭盆地与周缘造山带盆山耦合研究进展

林旭1,2, 刘静2   

  1. 1. 湖南文理学院, 洞庭湖生态经济区建设与发展湖南省协同创新中心, 常德 415000;
    2. 中国地震局地质研究所, 北京 100029
  • 收稿日期:2018-12-05 修回日期:2019-01-23 出版日期:2019-04-20 发布日期:2019-05-21
  • 作者简介:林旭,男,1984年生,2016年于中国科学院地质与地球物理研究所获第四纪地质学专业博士学位,副教授,主要从事新生代构造、大河演化研究,电话:13325135055,E-mail:hanwuji-life@163.com。
  • 基金资助:
    国家自然科学基金(41702178,41671011)和湖南省自然科学基金(2019JJ40198)共同资助

A REVIEW OF MOUNTAIN-BASIN COUPLING OF JIANGHAN AND DONGTING BASINS WITH THEIR SURROUNDING MOUNTAINS

LIN Xu1,2, ZENG Jing2   

  1. 1. Hunan Province Cooperative Innovation Center for the Construction & Development of Dongting Lake Ecological Economic Zone, Hunan University of Arts and Science, Changde 415000, China;
    2. Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2018-12-05 Revised:2019-01-23 Online:2019-04-20 Published:2019-05-21

摘要: 沉积盆地与造山带是大陆构造的2个重要的组成单元,具内在成因联系。对其耦合关系进行研究,可以恢复和重建岩石圈深部运动过程,了解近地表构造与气候之间的相互作用。江汉和洞庭盆地位于长江中游,与周缘造山带具有清晰的盆山边界,盆内河流水系十分发育,是一个多物源沉积盆地,是探讨从山(源)到盆(汇)沉积过程的天然实验室。文中对江汉盆地盆山耦合的研究结果进行了总结和梳理,介绍了造山带基岩、盆地和河流沉积物低温热年代学的应用方法,提出了新的研究切入点,建议今后在江汉和洞庭盆地开展盆山耦合研究时,将造山带基岩和河流碎屑矿物低温热年代学结果相结合,同时开展同一目标矿物的物源示踪研究,综合分析造山带隆升信息与物源信息,并与周缘构造和沉积学研究结果相互检验,可得到详细的盆山耦合演化过程。

关键词: 江汉盆地, 洞庭盆地, 盆山耦合, 低温热年代学

Abstract: Sedimentary basin and orogenic belt are two important components of continental structure with internal genetic links. The study of the basin-mountain coupling can reconstruct and restore the coupling relationships between the deep lithosphere process, near-surface structure and climate change over time. The Jianghan-Dongting Basin locates in the middle reaches of the Yangtze River, presenting a clear basin and mountain boundary with the Qinling-Dabie Shan to the north, the Mufu Shan to the southeast, the Wuling Shan to the southwest, and the E'xi Mountain to the west, respectively.
The Meso-Cenozoic Jianghan-Dongting Basin was affected by the subduction and collision of the Pacific plate and the Indian Ocean plate on the Eurasian continent, resulting in multiple tectonic evolution processes. There are some big rivers pouring into the Jianghan-Dongting Basin, such as the Yangtze River, Hanjiang River, Ba River, Xiangjiang River, and Yuanjiang River, etc. to serve as the material transport belts linking between the orogenic belt denudation and basin deposition. Therefore, the Jianghan-Dongting Basin has become a multi-source sedimentary basin, which makes it a natural laboratory to explore the geological processes from source to sink. Because the low-temperature thermochronology(e.g. fission-track and(U-Th)/He)can record the recent uplift time of mountains, they are widely used on the bedrock samples and the detrital synorogenic sediments in basins to constrain the surface uplift time of the orogenic belt. Hence, in the first parts of the paper we summarize and sort out the research results of basin-mountain coupling process in the Jianghan-Dongting Basin, evaluate the research results, identify the existing problems, and propose new research directions. After that, we introduce the applications of low-temperature thermochronology on the bedrock within the orogenic belt, basin and river sediments, combined with the actual situation of Jianghan-Dongting Basin, and put forward a new research breakthrough point. It is found that the Jianghan-Dongting Basin is very suitable for the study of low-temperature thermalchronology on detrital minerals. However, it should combine the low-temperature thermochronology results of both orogenic belt and river sediments with the provenance analysis on the same target minerals, building the connection between the exhumation and provenance information on the orogenic belt, thus providing the detailed evolution of mountain-basin coupling process.

Key words: Jianghan Basin, Dongting Basin, mountain-basin coupling, low-temperature thermochronology

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