| 华北地区重力场变化特征与孕震模型研究 |
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| 引用本文： | 徐伟民,石磊,陈石,卢红艳.华北地区重力场变化特征与孕震模型研究[J].地震学报,2021,43(4):441-452. |
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| 作者姓名： | 徐伟民 石磊 陈石 卢红艳 |
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| 作者单位： | 1.中国北京 100081 中国地震局地球物理研究所 |
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| 基金项目： | 国家重点研发计划（2018YFC1503806，2018YFC1503201）、国家自然科学基金（42004069，41874097）和中国地震科学实验场专项（2019CSES0105）联合资助 |
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| 摘 要： | 本文采用基于贝叶斯原理的重力平差方法对华北地区2009—2017年的16期陆地流动重力观测资料进行了统一处理，结合研究区内2009年以来4次M≥4.5 地震活动，分析区域重力场动态演化特征。基于华北地区均衡重力异常、布格重力异常、沉积层重力异常和莫霍面重力异常，研究华北地区三维密度结构特征，分析区域重力场变化与深部密度结构之间的关系。结果表明:研究区内近年来M≥4.5地震均位于区域差分重力场和累积重力场“零值”等值线附近、异常变化剧烈的梯度带及梯度带转弯部位，以及深部结构中理论均衡厚度与实际地壳厚度存在差异的非均衡区和三维密度结构的高低密度过渡带内。
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| 关 键 词： | 华北地区 重力场特征 陆地流动重力 均衡异常 三维密度结构 |
| 收稿时间： | 2020-09-01 |
Gravity field characteristics and seismogenic model in North China |
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| Xu Weimin,Shi Lei,Chen Shi,Lu Hongyan.Gravity field characteristics and seismogenic model in North China[J].Acta Seismologica Sinica,2021,43(4):441-452. |
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| Authors: | Xu Weimin Shi Lei Chen Shi Lu Hongyan |
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| Affiliation: | 1.Institute of Geophysics，China Earthquake Administration，Beijing 100081，China2.Beijing Baijiatuan Earth Science National Observation and Research Station，Beijing 100095，China |
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| Abstract: | In this paper, we use a Bayesian principle-based gravity leveling method to uniformly process 16 periods of land-based mobile gravity observations from 2009-2017 in North China, and study the dynamic characteristics of the regional gravity field in conjunction with four earthquakes （M≥4.5） that have struck the studied area since 2009. Further, we study the characteristics of the isostatic gravity anomaly in North China, and analyze the relationship between regional gravity field changes and deep density structure based on the Bouguer gravity anomaly, sedimentary sequences gravity anomaly and Moho gravity anomaly in the studied area to characterize the three-dimensional density structure in North China. The results show that, the four earthquakes （M≥4.5） in the studied area in recent years have been located near the contours of the regional differential gravity field and the zero-value of the cumulative gravity field, the abnormally shifting gradient zones and the bends of the gradient zones, the unbalanced zones in the deep structure where the theoretical equilibrium thickness differs from theactual crustal thickness, and the high and low densities of the three-dimensional density structure inside the transition zone. |
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