摘要
对中山站附近２个大地电磁测深点的数据处理结果表明，拉斯曼丘陵地区的岩石圈厚度为１４０ｋｍ。
This paper deals with the results of the MT observations in the region of Zhongshan Station,Larsemann Hills area, East Antarctica and points out that the Lithosphere thickness of the Larsemann Hills is 140 km and the crustal high conductivity layer is situated in 22 km.
出处
《南极研究》
CSCD
1994年第4期32-36,共5页
关键词
中山站
电磁测深
电性结构
南极地区
s Zhongshan Station, magnetotelluric deep sounding, electrical conductivity structure.
