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| 张家口—渤海地震带岩石圈磁场时空变化特征 | |
| 引用本文： | 张海洋,李博,苏树朋,王朝景,刘德强,赵慧琴,毛丰龙.张家口—渤海地震带岩石圈磁场时空变化特征[J].地震,2022,42(1):133-144. |
| 作者姓名： | 张海洋 李博 苏树朋 王朝景 刘德强 赵慧琴 毛丰龙 |
| 作者单位： | 1.河北红山巨厚沉积与地震灾害国家野外科学观测研究站, 河北 邢台 054000; 2.河北省地震局保定地震监测中心站, 河北 保定 071000 |
| 基金项目： | 河北省地震局地震科技星火计划重点项目(DZ20190422046); 河北省地震局地震科技星火计划(DZ2021121600003, DZ2021121400007) |
| 摘 要： | 利用2016—2018年3期华北地区流动地磁矢量原始测量资料, 经数据计算获得2期华北地区和张家口—渤海地震活动带及邻区岩石圈磁场时空变化模型。 研究结果显示: 张家口—渤海地震带岩石圈磁场变化空间分布不均匀, 具有明显的分区特征, 在张家口段(西段)与北京段(中西段)分界处和北京段(中西段)与唐山段(中东段)分界处岩石圈磁场各要素具有明显的异常变化, 如水平矢量存在转向和幅值变化, 磁偏角与磁倾角具有正负异常高梯度带的特征, 这与张家口—渤海地震带构造分段性特征密切相关。 张家口—渤海地震带位于燕山块体与华北平原块体之间, 两者运动的平动速率之差是张家口—渤海地震带左旋走滑的直接动力来源, 而各断裂带左旋走滑速率之差很可能是岩石圈磁场空间变化分段性分布的主要原因。 |
| 关 键 词： | 张家口—渤海地震带 流动地磁 岩石圈磁场 地应力方向 |
| 收稿时间： | 2020-03-08 |
| 修稿时间： | 2021-11-16 |
Tempo-spatial Variation Characteristics of Lithospheric Magnetic Field in Zhangjiakou-Bohai Seismic Belt |
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| ZHANG Hai-yang,LI Bo,SU Shu-peng,WANG Zhao-jing,LIU De-qiang,ZHAO Hui-qin,MAO Feng-long.Tempo-spatial Variation Characteristics of Lithospheric Magnetic Field in Zhangjiakou-Bohai Seismic Belt[J].Earthquake,2022,42(1):133-144. | |
| Authors: | ZHANG Hai-yang LI Bo SU Shu-peng WANG Zhao-jing LIU De-qiang ZHAO Hui-qin MAO Feng-long |
| Institution: | 1. Hebei Hongshan National Observatory on Thick Sediments and Seismic Hazards, Xingtai 054000, China; 2. Baoding Earthquake Monitoring Center Station, Hebei Earthquake Agency, Baoding 071000, China |
| Abstract: | Using the original geomagnetic vector measurements in North China during the periods from 2016 to 2018, the tempo-spatial variation models of the magnetic field in the lithosphere in North China and in the Zhangjiakou—Bohai seismicity belt have been obtained. The results show that there are obvious anomalies at the boundary between Zhangjiakou section and Beijing section, as well as between Beijing section and Tangshan section, the horizontal vector has the characteristics of direction turning and amplitude variation, magnetic declination angle and magnetic dip angle show the characteristics of positive and negative abnormally high gradient band. This is closely related to the tectonic segmentation of the Zhangjiakou—Bohai seismic belt. The Zhangjiakou—Bohai seismic belt is located between the Yanshan block and the North China plain block. The relative movement of Yanshan block and North China plain block is the direct reason of left-lateral strike-slip in the Zhangjiakou-Bohai seismic belt, and the difference of the left-lateral strike-slip rates between several fault belts maybe is the main reason why the spatial variation of lithospheric magnetic field is characterized by piecewise distribution. |
| Keywords: | Zhangjiakou—Bohai seismic belt Mobile geomagnetic observation Lithosphere magnetic field Crustal stress direction |
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