【摘 要】
：
使用第21次中国南极科学考察(CHINARE 21,2004/05)期间获取的东南极中山站-DomeA(昆仑站)长为1183km的冰盖断面车载冰雷达数据。首次揭示了该断面的冰盖内部环境要素-内部等时层结构,显示出沉积不同深度上的古冰盖表面的几何特征。对整个断面冰盖内部的连续层、断裂层和信号空白区(Echo Free Zone)进行了识别及分类,给出其空间分布。找出从雷达断面上Lambert裂谷的表
【机 构】
：
国家海洋局极地科学重点实验室,中国极地研究中心,上海,200136
论文部分内容阅读
使用第21次中国南极科学考察(CHINARE 21,2004/05)期间获取的东南极中山站-DomeA(昆仑站)长为1183km的冰盖断面车载冰雷达数据。首次揭示了该断面的冰盖内部环境要素-内部等时层结构,显示出沉积不同深度上的古冰盖表面的几何特征。对整个断面冰盖内部的连续层、断裂层和信号空白区(Echo Free Zone)进行了识别及分类,给出其空间分布。找出从雷达断面上Lambert裂谷的表面高程、快速冰流区。讨论了内部等时层形态及其分布与冰盖动力学性质的关系。
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