极地研究

极地研究 ›› 1994, Vol. 5 ›› Issue (1-English): 44-51.

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The elemental geochemical characteristics of Late Quaternary rock core from Yanwo Lake in the Great Wall Station area, King George Island, Southwest Antarctica

 Yu Suhua1, Zheng Honghan1, Chen Xiaobo2, Ma Shulan3, Ma Jianguo3 and Fang Hong3   

  1. 1Guangzhou New Technical Institute of Geology, Academia Sinica, Guangzhou 510640, China 2Lanzhou Institute of Glaciology and Geocryology, Academia Sinica, Lanzhou 730000, China 3Institute of High Energy Physics, Academia Sinica, Beijing 100080, China
  • 出版日期:1944-03-30 发布日期:1944-03-30
  • 通讯作者: Yu Suhua

The elemental geochemical characteristics of Late Quaternary rock core from Yanwo Lake in the Great Wall Station area, King George Island, Southwest Antarctica

 Yu Suhua1, Zheng Honghan1, Chen Xiaobo2, Ma Shulan3, Ma Jianguo3 and Fang Hong3   

  1. 1Guangzhou New Technical Institute of Geology, Academia Sinica, Guangzhou 510640, China 2Lanzhou Institute of Glaciology and Geocryology, Academia Sinica, Lanzhou 730000, China 3Institute of High Energy Physics, Academia Sinica, Beijing 100080, China
  • Online:1944-03-30 Published:1944-03-30
  • Contact: Yu Suhua

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摘要：

This paper is manily to treat the change regularity of the contens,distributions, enrich coefficients and correlative coefficients of some trace and constant elements in the sediments of Late Quaternary rock core from Yanwo Lake in the Great Wall Station area, King George Island and to discuss the sedimentary sources in Yanwo Lake and the periodical changes of Late Quaternary climate and the environment in the area. It is concluded that the elastic sedimentary rocks, including volcanic sedimentary rocks, around Yanwo Lake are the major sources of Yanwo Lake sedimentsi the mantle material is also one of its sources and what is more, the continent-sourced materials are transported by the Antarctic glacier.

关键词: elemental geochemistry, lacustrine deposits of Late Quaternary, Yanwo Lake, King George Island

Abstract:

This paper is manily to treat the change regularity of the contens,distributions, enrich coefficients and correlative coefficients of some trace and constant elements in the sediments of Late Quaternary rock core from Yanwo Lake in the Great Wall Station area, King George Island and to discuss the sedimentary sources in Yanwo Lake and the periodical changes of Late Quaternary climate and the environment in the area. It is concluded that the elastic sedimentary rocks, including volcanic sedimentary rocks, around Yanwo Lake are the major sources of Yanwo Lake sedimentsi the mantle material is also one of its sources and what is more, the continent-sourced materials are transported by the Antarctic glacier.

Key words: elemental geochemistry, lacustrine deposits of Late Quaternary, Yanwo Lake, King George Island