地理学报 ›› 2011, Vol. 66 ›› Issue (5): 698-708.doi: 10.11821/xb201105012
范天来, 范育新, 魏国孝
收稿日期:
2011-03-07
修回日期:
2011-03-22
出版日期:
2011-05-20
发布日期:
2011-05-20
通讯作者:
范育新(1975-), 男, 副教授, 主要从事干旱区湖泊和沙漠的光释光年代学研究。E-mail: yxfan@lzu.edu.cn
作者简介:
范天来(1984-), 男, 博士研究生. E-mail: fantl2004@hotmail.com
基金资助:
973 项目(2010CB950202); 国家自然科学基金项目(40972116)
FAN Tianlai, FAN Yuxin, WEI Guoxiao
Received:
2011-03-07
Revised:
2011-03-22
Online:
2011-05-20
Published:
2011-05-20
Supported by:
973 Project, No.2010CB950202; National Natural Science Foundation of China, No.40972116
摘要: 在位于河套盆地内部的西山咀凸起区发现了典型的湖滩岩、湖蚀平台和一套较完整的湖相沉积地层。基于海拔高程的推断,地貌和地层沉积记录指示西山咀地区曾经存在过一个海拔达到1080 m上下的古湖面。完整的沉积地层反映西山咀凸起区经历了深湖相—滨湖相—冲洪积相—风成堆积的演变过程。光释光测年结果表明,在距今65 ka 前后,“吉兰泰—河套”古大湖在西山咀地区曾经连通;但在距今约50~30 ka 湖面再没有上涨。这一研究表明:在MIS 3 阶段某一时期,该地区的古湖面发生衰退。随后,再没有发育高于“吉兰泰—河套”古大湖最高湖面的湖泊。
范天来, 范育新, 魏国孝. 河套盆地西山咀凸起区湖相地层的发现及其测年[J]. 地理学报, 2011, 66(5): 698-708.
FAN Tianlai, FAN Yuxin, WEI Guoxiao. New Findings and Dating of Lacustrine Sediments in the Xishanzui Subuplift, Hetao Basin[J]. Acta Geographica Sinica, 2011, 66(5): 698-708.
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