留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS

施雅风 郑本兴 李士杰

施雅风, 郑本兴, 李士杰. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. 中国地理科学, 1992, 2(4): 293-311.
引用本文: 施雅风, 郑本兴, 李士杰. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. 中国地理科学, 1992, 2(4): 293-311.
Shi Yafeng, Zheng Benxing, Li Shijie. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. Chinese Geographical Science, 1992, 2(4): 293-311.
Citation: Shi Yafeng, Zheng Benxing, Li Shijie. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. Chinese Geographical Science, 1992, 2(4): 293-311.

LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS

LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS

计量
  • 文章访问数:  770
  • HTML全文浏览量:  41
  • PDF下载量:  926
  • 被引次数: 0
出版历程
  • 刊出日期:  1992-12-20

LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS

摘要: Since the late 1950's, many Chinese scientists have explored the remains of the Quaternary glaciation in the Qinghai-Xizang (Tibet) Plateau and its surrounding mountains. In the main, 3-4 glaciations have been recognized. The largest one occurred in the Late Middle Pleistocene with piedmont glaciers, ice caps and trellis valley glaciers in many high peak regions. But here is no evidence of a unified ice sheet covering the whole plateau as described by M. Kuhle. Due to the further uplifting of the Himalayas and Qinghai-Xizang Plateau the climate became progressively drier, diminishing the extension of glaciers during the Late Pleistocene. The elevation of the snow line during the Last Glaciation was about 4,000 m on the south, east and northeast edges of the plateau and ascended to 5500 m on the hinder northwest of the plateau. The thermal effect of the big plateau massif, the sharp increase of aridity from the southeast rim to the northwest inland area and the abrupt decrease of precipitation during the Ice Age largely account for the distribution of the Quaternary glaciers in the Qinghai-Xizang Plateau. The neglect of Chinese literature may be one of the causes accounting for M. Kuhle's misinterpretation on the environment of the Quaternary glaciations in the Qinghai-Xizang Plateau.

English Abstract

施雅风, 郑本兴, 李士杰. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. 中国地理科学, 1992, 2(4): 293-311.
引用本文: 施雅风, 郑本兴, 李士杰. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. 中国地理科学, 1992, 2(4): 293-311.
Shi Yafeng, Zheng Benxing, Li Shijie. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. Chinese Geographical Science, 1992, 2(4): 293-311.
Citation: Shi Yafeng, Zheng Benxing, Li Shijie. LAST GLACIATION AND MAXIMUM GLACIATION IN THE QINGHAI-XIZANG(TIBET)PLATEAU:A CONTROVERSY TO M. KUHLE, S ICE SHEET HYPOTHESIS[J]. Chinese Geographical Science, 1992, 2(4): 293-311.

目录

    /

    返回文章
    返回