十堰至洛阳大地电磁测深观测结果

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摘要

湖北十堰—河南洛阳QB－1剖面大地电磁测深较好地反映了剖面通过的华北地台和秦岭地槽褶皱系的地电特征, 圈出了壳内高导层和上地幔高导层, 反映了两条切入上地幔深部的大断裂, 推断嵩县大坪深部的低阻体可能为岩浆房, 为研究深部地质构造提供了重要资料。

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Abstract：

The telluric electromagnetic sounding performed along QB-1 profile fromShiyan of Hubei province to Luoyang of Henan province reflects quite clearlythe geoelectric characteristics of North China platform and Qinling geosynclinalfolded belt that this profile passes through, delineates high-conductive layersin the crust and in the upper mamtle, and reveals two great faults that cutthe deep part of the upper mantle; it is also inferred that the low-resistancebody at the depth of Daping (Songxian county) might be a magma chamber.All these results serve as important data for the study of deep geology.

出版日期: 1990-08-24

引用本文:

蒋洪堪, 战双庆, 王宏勋. 十堰至洛阳大地电磁测深观测结果[J]. 物探与化探, 1990, 14(4): 285-291.
Jiang Hongkan, Zhan Shuangqing, Wang Hongxun. OBSERVATIONS OF TELLURIC ELECTROMAGNETICSOUNDING PERFORMED ALONG SHIYAN-LUOYANG PROFILE. Geophysical and Geochemical Exploration, 1990, 14(4): 285-291.

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https://www.wutanyuhuatan.com/CN/ 或 https://www.wutanyuhuatan.com/CN/Y1990/V14/I4/285

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［3］ Ben K. Sternberg, James C. Washburne, Robert G. Anderson, 1985, Investigation of MT Static Shif Correction Methods.
［4］费栋宇、高锐:中国及相邻海域地温场分布规律的研究,中国区域地质第19辑,1985。