太原盆地第四纪地质研究进展  

Research Progress of Quaternary Geology in Taiyuan Basin

作　　者：王利康 杨振京[1] 毕志伟[1] 杨庆华[1] 付晓芬[1,2] 

机构地区：[1]中国地质科学院水文地质环境地质研究所,河北石家庄050061 [2]成都理工大学,四川成都610059

出　　处：《中国锰业》2017年第3期54-57,共4页China Manganese Industry

基　　金：中国地质科学院水文地质环境地质研究所基本业务费(SK201609)

摘　　要：太原盆地第四纪以来沉积了巨厚的河湖相地层,边缘区中更新世以来在湖相地层上部覆盖了数十米厚的黄土,是研究第四纪地层和气候环境演化的良好载体。通过搜集前人第四纪地质相关资料,对前人成果从湖相地层、古湖泊变迁、新构造运动与地貌演化3个方面加以总结,确定下一步研究方向。In the middle of Taiyaun basin deposited, there is a huge lacustrine strata in Quaternary. In the upper part of the basic, we find that it is covered with tens of meters loess deposits. It＇ s worth to studying the evolution of Quaternary strata and paleoclimate. The author tries to analyze and summarize the previous research in three aspects of lacustrine strata, namely, Palaeo -Lake changes, neotectonic movement and Geomorphic evolution. The result will determine the direction of the next step.

关 键 词：湖相地层 古湖泊变迁 新构造运动 地貌演化 

分 类 号：P534.63[天文地球—第四纪地质学]