摘要
叙述了连续电磁剖面法(CEMP)测深在青藏高原北羌塘盆地龙尾湖区块构造详测勘查中,其数据采集和数据处理方法;给出了CEMP测深结果及其解释成果;并将CEMP测深成果与二维反射地震和大地电磁测深剖面资料及羌-资1井钻探验证资料进行比照,说明了CEMP测深勘查浅层地质构造的有效性。
Using the Continuous Electromagnetic Profiling method（CEMP）,the author performed a survey in Longwei lake area of northern Qiangtang basin within Qinghai-Tibet plateau.This paper deals with the technique of data collection and data processing,gives the result of CEMP section and its interpretation.A comparison with the results obtained by such means as 2D reflection seismic survey,magnetotelluric sounding and verification of No.Qiang-Zi 1 borehole shows that the result of CEMP is effective and the method can be used in the investigation of shallow geological structures.
出处
《物探与化探》
CAS
CSCD
北大核心
2010年第3期303-307,319,共6页
Geophysical and Geochemical Exploration
关键词
连续电磁剖面测量
张量测量
青藏高原北羌塘盆地
二维反演
穹窿构造
Continuous Electromagnetic Profiling
tensor survey
2D inversion
domal structure
northern Qiangtang basin of Qinghai-Tibet plateau
