磁力勘探与岩性测深理论基础的对比  

A COMPARISON OF THE THEORETICAL BASIS BETWEEN MAGNETIC EXPLORATION AND LITHOLOGIC SOUNDING

作　　者：杨凌[1] 杨庆锦[2] 

机构地区：[1]中国地震应急搜救中心,北京100049 [2]中国地质科学院地球物理地球化学勘查研究所,河北廊坊065000

出　　处：《物探与化探》2007年第B10期51-52,共2页Geophysical and Geochemical Exploration

摘　　要：首先概括了岩性测深技术的理论基础和物性基础要点,强调电偶极子场是岩性测深技术的基本理论。然后通过电偶极子场与磁偶极子场的类比,以及岩性测深与磁力勘探的对比,提出了一条研究岩性测深技术理论基础及正演计算的思路。This paper sums up the theoretical and physical basis of the lithologic sounding, and points out that the electrical dipole field is the basic theory of the lithologic sounding. Based on an analogy of the electrical dipole field with the electrical dipole field as well as a comparison between the lithologic sounding and the magnetic exploration, this paper puts forward the theoretical basis for lithologic sounding research and the train of thought for forward calculation.

关 键 词：岩性测深 磁法勘探 电偶极子场 磁偶极子场 

分 类 号：P631[天文地球—地质矿产勘探]