摘要
计算了对应于各个UT小时的24个经度带的Sq地下感应场对外部施感场的响应函数,应用Schmucker'sApproximateEuristic反演方法,计算了这些经度带的地下等效层及其电导率分布,得到了地壳-上地幔电导率经向分布的大致图案。对该结果的分析研究得出,全球电导率经向分布存在着极大的不均匀性,在0-400km深度范围内,太平洋和大西洋为低导区;欧亚大陆与美洲大陆为高导区。电导率分布特征与岩石层结构有明显的相关性:在俯冲带,低导区由海洋向大陆下插入;在大洋中脊表现为高导电性。反演结果与地震层析成像结果的比较表明,地下高电导区和低电导区的位置分别对应于地震波低速区和高速区。
On the basis of our previous sutdy on the longitudinal variation of the Sq-field, the response function is calculated for different longituinal regions corresponding to each UT hour. By means of Schmucker's Approximate Euristic Method, longitudinal distribution of the conductivity in the Earth's crust and upper-mantle is obtained. It shows a great longitudinal inhomogeneity of conductivity: relatively high conductivity in European-Asian and American regions and low in Pacific and Atlantic regions in the depth of 0-400km. The low conductivity layer in the upper mantle of Pacific region extends under the Asian mantle, while at mid-ocean ridges there are high conductivity layers, which agree with the idea of the plate-tectonic theory. The conductivity distribution is compared with the Earth's velocity structure from the global seismic tomography technique. A good correspondance between low (or high) conductivity with high (or low) velocity is obtained.
出处
《地球物理学报》
SCIE
EI
CSCD
北大核心
1996年第3期322-326,共5页
Chinese Journal of Geophysics
基金
国家自然科学基金
关键词
磁测深
电导率
地壳
上地幔
分布特征
Sq, Geomagnetic deep sounding, Response function, Substitute conductor, Conductivity, Plate-tectonic theory, Seismic velocity structure.