伊犁盆地三道河河流阶地沉积物粒度特征及其古气候响应

李建刚; 刘晓燕; 袁四化; 陈诗哲; 李瑛; 赵振宏; 姜纪沂

doi:10.19751/j.cnki.61-1149/p.2020.04.002

伊犁盆地三道河河流阶地沉积物粒度特征及其古气候响应

李建刚^1,2,3,
刘晓燕^1,2, ,,
袁四化^1,2,
陈诗哲^1,2,
李瑛³,
赵振宏³,
姜纪沂^1,2

1. 防灾科技学院, 河北三河 065201;
2. 河北省地震动力学重点实验室, 河北三河 065201;
3. 中国地质调查局西安地质调查中心, 陕西西安 710054

基金项目:

国家自然科学基金项目“新生代伊犁盆地与周缘山脉耦合关系研究”（41772200），中国地质调查局项目“伊犁河谷西部平原区1：5万水文地质调查”（121201011000150021，No.DD20190351），防灾科技学院地貌与第四纪地质学精品课程建设项目（JPJS2018005）联合资助

详细信息

作者简介:
李建刚(1995-),男,硕士,构造地质学专业。E-mail:1061916371@qq.com

通讯作者:
刘晓燕(1982-),女,讲师,主要从事第四纪与新构造运动研究。E-mail:xiaoyanliu818@126.com

中图分类号: P54
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出版历程
- 收稿日期: 2019-10-08
- 修回日期: 2020-06-20
- 网络出版日期: 2022-07-28
- 发布日期: 2020-12-04

Grain-size Characteristics and Paleoclimate Response of Terrace Sediments in Sandaohe River of Yili Basin

1. Institute of Disaster Prevention, Sanhe 065201, Hebei, China;
2. Hebei Key Laboratory of Earthquake Dynamics, Sanhe 065201, Hebei, China;
3. Xi'an Center of China Geological Survey, CGS Xi'an 710054, Shaanxi, China

摘要

摘要: 河流成因沉积物中携带了古气候变化和古环境变迁的关键信息。笔者利用三道河剖面的粒度、磁化率特征及光释光（OSL）年龄对其沉积环境进行了探讨。结果表明：粒度频率曲线包括单峰和双峰2种，频率累积曲线以三段式为主，粒度特征反映三道河一级阶地沉积经历了由低能湖泊相→高能河流相→中高能河流相的演变过程；磁化率结果显示H1期间存在最低值，在B-A暖期迅速升高，在YD期间降低-升高-降低。三道河一级阶地形成于晚更新世—全新世早期，完整记录了末次冰消期以来的YD、B-A以及H1三次重大气候变化事件。
- 伊犁盆地 /
- 粒度分析 /
- 沉积环境 /
- 古气候
Abstract: Fluvial sediments carry some key information on paleoclimate and paleoenvironment changes. In this paper, the sedimentary environment of the Sandaohe section is discussed according to the grain size, magnetic susceptibility and OSL age. The results show that the frequency curve of the grain size includes single peak and double peak, and the accumulation frequency curve is mainly three-section type. The characteristics of grain size reflect that the deposition of the first terrace has experienced the evolution process from low-energy lake facies, high-energy river facies to medium-high energy river facies. The results of magnetic susceptibility show that a minimum value appears in H1, a rapid increase in B-A warm period and a decrease-increase-decrease in YD period. The first terrace of Sandaohe formed in late Pleistocene to early Holocene, being the evidence of three major climate change events (YD, B-A and H1) since the last deglaciation.
- Yili basin /
- grain-size analysis /
- sedimentary environment /
- paleoclimate

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