横断山区第四纪冰期的划分与对比
文献类型:期刊论文
作者 | 李钟武; 陈治荣; 王明龙 |
刊名 | 地质论评
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出版日期 | 1991 |
卷号 | 37期号:2页码:125-133 |
关键词 | 第四纪冰期 第四纪冰川 横断山区 古冰川遗迹 冰进 贡嘎山 新冰期 |
ISSN号 | 0371-5736 |
其他题名 | CLASSIFICATION AND CORRELATION OF THE QUATERNARY GLACIAL EPOCH IN THE HENGDUAN (TRANSVERSE) MOUNTAINS |
通讯作者 | 李钟武 |
中文摘要 | 横断山区是我国第四纪冰川发育期次较多、古冰川遗迹也最多的地区之一。本文着重介绍了作者近10年来在该区考察中取得的大量新资料,特别是14C年代资料,在此基础上对该区第四纪冰期划分出8期(次)冰期(冰进、间冰阶段),并进行了对比。作者认为该区冰川具有明显的区域性规律,其与青藏高原抬升有关;横断山区第四纪冰川活动范围可至北纬26°线以北。 |
英文摘要 | There are many Quaternary glacial development stages in the Hengduan(Transverse) Mountains, southwestern China, and palaeoglacial remnants of this area are well developed. This paper presents many new data which were obtained from field observations during the past 10 years, of which related 14C age data are vcry valuable. Based on the above data, the Quaternary glacial epoch of the area can be divided into the following from early to later: l) Yajiageng glacial stage of the Middle Pleistocene; 2) Early Hailuogou glacial stage of the Late Plcistocene; 3) Qingshiban interglacial stage of the Late Pleistocene; 4) Late Hailuogou glacial stage of the Late Pleistocene; 5) Zhituoda glacial advance of the Holocene; 6) Dayanwo glacial advance of the Holocene; 7) Hailuogou glacial advance of the Holocene and 8) Glacial advance of the 17th to 19th centuries.Two conclusions are drawn in the end of this paper: 1) Quaternary glaciers were developed first in the Qinghai-Xizang(Tibet)Plateau and its activity then progressively migrated toward the Hengduan Mountains area. This regional regularity corresponds to uplifting of the Qinghai-Xizang Plateau. 2) The southern boundary of the activity of Quaternary glaciers goes as far as north of latitude 26°N. |
语种 | 中文 |
源URL | [http://ir.imde.ac.cn/handle/131551/10958] ![]() |
专题 | 成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前) |
作者单位 | 中国科学院成都地理研究所 |
推荐引用方式 GB/T 7714 | 李钟武,陈治荣,王明龙. 横断山区第四纪冰期的划分与对比[J]. 地质论评,1991,37(2):125-133. |
APA | 李钟武,陈治荣,&王明龙.(1991).横断山区第四纪冰期的划分与对比.地质论评,37(2),125-133. |
MLA | 李钟武,et al."横断山区第四纪冰期的划分与对比".地质论评 37.2(1991):125-133. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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