极地研究（英文版）2005，Vol.16Issue(1)：55-58,4.
Evidence for warmer event from quartz grains in the soil of Grove Mountains, East Antarctica
Evidence for warmer event from quartz grains in the soil of Grove Mountains, East Antarctica
Yan Xin 1Li Xiaoli 1Liu Xiaohan 1Zhang Ru-fan1
作者信息
- 1. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029, China
- 折叠
摘要
Abstract
The cold desert soil has been discovered at first time in southern ridgeof Mount Harding, Grove Mountains of interior East Antarctica Ice Sheet. Based on the micro structural observation, dominant characteristics of quartz grains include: distinct surface stria and fractures, and clean features of frost action at both of crystal margins and micro crannies of quartz grains. These features show a pedogenesis environment of few water, short transportation and frost action, revealing a warmer climatic event existed in this region.关键词
Grove Mountains/soil/quartzKey words
Grove Mountains/soil/quartz分类
天文与地球科学引用本文复制引用
Yan Xin,Li Xiaoli,Liu Xiaohan,Zhang Ru-fan..Evidence for warmer event from quartz grains in the soil of Grove Mountains, East Antarctica[J].极地研究（英文版）,2005,16(1):55-58,4.
