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柯林斯冰帽雷达测厚和冰下地形研究
引用本文:朱国才,井晓平,韩建康,高新生,康建成,温家洪.柯林斯冰帽雷达测厚和冰下地形研究[J].极地研究,1994,6(2):43-48.
作者姓名:朱国才  井晓平  韩建康  高新生  康建成  温家洪
作者单位:中国科学院兰州冰川冻土研究所,中国极地研究所
基金项目:国家自然科学基金,国家南极考察委员会资助,中国科学院特别资助,中国科学院兰州冰川冻土研究所所长基金
摘    要:使用一台300MHz高频脉冲雷达,对柯林斯冰帽150个测点进行冰厚探测,描绘出15km冰床雷达回波剖面。该冰帽小冰穹最大冰厚125-131m,位于其顶部,小冰穹顶至主冰穹顶脊线上的平均厚度约109m;主冰穹顶部附近50-85m深度处有一被钻探证实为含水界面的雷达回波;小冰穹近乎南北向的冰下地形与该岛北方台地地形相似。

关 键 词:柯林斯冰帽  雷达测厚  冰下地形

RADAR SOUNDING AND STUDY OF THE BEDROCK TOPOGRAPHY ON COLLINS ICE CAP
Zhu Guocai,Jing Xiaoping,Han Jiankang and Gao Xinsheng.RADAR SOUNDING AND STUDY OF THE BEDROCK TOPOGRAPHY ON COLLINS ICE CAP[J].Chinese Journal of Polar Research,1994,6(2):43-48.
Authors:Zhu Guocai  Jing Xiaoping  Han Jiankang and Gao Xinsheng
Abstract:Using a high frequency pulse radar of 300MHz, radar sounding was carried out at 150 points on Collins Ice Cap and the echo profile of bedrock in 15km distance was given. The maximum ice thickness, 125-131m, at Small Dome of this ice cap was located on the summit; the average thickness on the ridge from summit of Small Dome to summit of Main Dome was about 109m; a radar echo was observed at the depth of 50-85m around the summit of Main Dome, which was proven a water table by ice coring; the bedrock topography of Small Dome in the direction near south to north was similar to that of Northern Terrace.
Keywords:s  Collins Ice Cap  radar sounding  bedrock topography  ice  thickness    
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