华北中部岩石圈电性结构——应县—商河剖面大地电磁测深研究

魏文博; 谭捍东; 金胜; 邓明; 叶高峰; 邓靖武; 万战生

华北中部岩石圈电性结构——应县—商河剖面大地电磁测深研究

中国地质大学地球物理系, 北京 100083

基金项目:

国土资源部“十五”专项计划 200101

详细信息

作者简介:
魏文博(1945-), 男, 教授, 博士生导师, 长期从事地球物理学的教学与研究

中图分类号: P631.3
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出版历程
- 收稿日期: 2002-07-29
- 刊出日期: 2002-09-25

Conductivity Structure of Lithosphere in Central North China: Magnetotelluric Study of Yingxian-Shanghe profile

Department of Geophysics, China University of Geosciences, Beijing 100083, China

摘要

摘要: 20 0 1年, 沿着山西应县到山东商河, 重新布置大地电磁测深剖面进行研究.采用现代先进的大地电磁数据处理技术和快速松弛二维反演方法获得该剖面二维电性结构模型, 从而充分展示了华北地区岩石圈电性结构的特点.从电性特征上讲, 华北岩石圈以太行山前断裂为界划分为东、西两区, 东区为低阻区, 西区为高阻区.在东区, 上地壳电性结构基本与华北裂谷系的隆、坳构造格局相对应, 岩石圈的电导最高达3× 10⁴ S, 远远大于强烈活动的安第斯山岩浆弧区和西藏高原岩石圈的电导.这里, 在构造连接部位的地壳中有不连续的高导体存在, 电导率大约0.1~ 0.8S/m.在西区, 太行山和恒山的岩石圈为高阻块体, 表现出稳定大陆区岩石圈导电性结构的特点.但恒山高阻块体之下发现一组向西缓倾的高导层, 其电导率为0.0 4~0.2 5S/m, 顶面在2 0km深处, 底面深度大约40km.
- 华北 /
- 大地电磁测深 /
- 岩石圈 /
- 电性结构
Abstract: In 2001, an MT sounding profile was relocated from Yingxian, Shanxi Province to Shanghe, Shandong Province. The advanced MT data processing method and rapid release inversion (RRI) were employed to establish a 2D model of conductivity structure showing fully the features of conductivity structure of the lithosphere in North China. In terms of conductivity, the North China lithosphere is classified as eastern and western parts with the frontal fault in the Taihang mountain as the corresponding boundary line. The eastern part is characterized by the low resistance conductivity, and the western part is characterized by the high resistance conductivity. In the eastern part, the conductivity structure in the upper crust corresponds roughly to the uplift and depression tectonic structure of the North China rift system, with the maximum conductivity of the lithosphere reaching 3×10⁴ S, far greater than that of magma arc area in Andes and the lithosphere of the Tibet plateau where the volcanic activities are violent. Here, discontinuous highly conductive bodies, whose conductivity is about 0.1-0.8 S/m, are present in the crust of the contact zone. In the western part, the lithosphere of the Taihang and Hengshan mountains, composed of high resistance conductivity bodies, is characterized by the conductivity structure of a stable continental lithosphere. However, a group of westward inclined highly conductive layers, whose conductivity is 0.04-0.25 S/m, whose top layer is located at the depth of 20 km and whose bottom layer is located at the depth of around 40 km, were discovered under the Hengshan high resistance conductivity body
- North China /
- magnetotelluric /
- lithosphere /
- conductivity structure

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图 1 应县—商河大地电磁测深剖面位置

Fig. 1. Location of Yingxian-Shanghe MT profile

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图 2 HB08号点大地电磁测深曲线

a₁, a₂分别为HB08号点XY极化模式视电阻率和阻抗相位; b₁, b₂分别为HB08号点YX极化模式视电阻率和阻抗相位

Fig. 2. MT sounding curves of HB08 survey station

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图 3 MT二维反演时TM模式的拟合结果

Fig. 3. Comparison between theoretical response of inversion model and real data

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图 4 应县—商河大地电磁二维反演模型

红色表示“低阻体”, 蓝色表示“高阻体”; “色标”表示的是电阻率的常用对数值, 单位为Ω·m

Fig. 4. Model from 2-D inversion of MT data along Yingxian-Shanghe profile

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图 5 应县—商河岩石圈电导剖面曲线

Fig. 5. Distribution curve of lithospheric electric conductance along Yingxian-Shanghe profile

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参考文献(8)

[1]	邓晋福, 赵海玲, 莫宣学, 等. 中国大陆根-柱构造———大陆动力学的钥匙[M]. 北京: 地质出版社, 1996.30-39. DENG J F, ZHAO H L, MO X X, et al. Continental roots-plume tectonics of China—key to the continental dynamis[M]. Beijing: Geological Publishing House, 1996, 30-39.
[2]	秦馨菱, PedersenLB, 赵玉林, 等. 唐山地震区地壳电性结构及MT探索潜在震源的可能性[J]. 地震学报, 1991, 13 (3): 354-363. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXB199103009.htm QIN X L, Pedersen L B, ZHAO Y L, et al. Conductivity structure of crust in the Tangshan seismic area and the possibility of exploring potential seismic sources by mag-netotelluric method[J]. Chinese Journal of Acta Seismologica Sinica, 1991, 13 (3): 354-363. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXB199103009.htm
[3]	邓前辉, 张木生, 詹艳, 等. 邢台震区地壳上地幔电性结构及其构造意义[J]. 地震地质, 1997, 19 (2): 155-163. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ702.007.htm DENG Q H, ZHANG M S, ZHAN Y, et al. Geoelectrical structure of the crust and upper mantle in the Xingtai earthquake area and its tectonic implications[J]. Chinese Journal of Seismology and Geology, 1997, 19 (2): 155-163. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ702.007.htm
[4]	赵国泽, 刘铁胜, 江钊, 等. 山西阳高—河北容城剖面大地电磁资料的二维反演解释[J]. 地球物理学报, 1997, 40 (1): 38-45. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWX199701004.htm ZHAO G Z, LIU T S, JIAN G Z, et al. Two-dimensional inversion of MT data along Shanxi Yanggao-Hebei Rongcheng profile[J]. Acta Geophysica Sinica, 1997, 40 (1): 38-45. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWX199701004.htm
[5]	Egbert G D, Booker J R. Robust estimation of geomagnetic transfer functions, geophysics[J]. J Roy Astr Soc, 1986, 87: 175-194.
[6]	Smith J T, Booker J R. Rapid inversion of two- and three-dimensional magnetotelluric data[J]. J Geophys Res, 1996, 96 (B3): 3905-3922.
[7]	Wenbo W, Martyn U, Jones A, et al. Detection of widespread fluids in the Tibetan crust by magnetotelluric studies[J]. Science, 2001, 292: 716-718, . doi: 10.1126/science.1010580
[8]	石应骏, 刘国栋, 吴广耀, 等. 大地电磁测深法教程[M]. 北京: 地震出版社, 1985.23-34. SHI Y J, LIU G D, WU G Y, et al. A course in magnetotelluric method[M]. Beijing: Seismology Publishing House, 1985.23-34.