首页|乌什MS7.1地震重力场变化特征分析研究

乌什MS7.1地震重力场变化特征分析研究

扫码查看
利用南天山地区乌什MS7.1地震发生后的流动重力观测数据,获取乌什MS7.1地震前后南天山地区重力场变化,对该地区地震前后的一年和多年尺度重力变化、测段和测点重力变化特征进行研究.结果表明,乌什地震发生后,重力变化零等值线穿过震中地区,并出现重力变化的高梯度带.重力变化零等值线出现的区域,物质密度正在经历增加和减少的过渡过程.物质的增减差异导致强烈运动、能量积累.强震前的重力异常可能持续较长时间,有可能出现重力场变化较小的情况,因此提取和分析强震前的重力异常信号时,需要考虑较长时间跨度的重力观测数据.震后观测的流动重力数据能够较好反映发震断层的应力释放特征,有助于分析余震发展趋势.
CHARACTERIZATION AND ANALYSIS OF GRAVITY FIELD CHANGES BEFORE AND AFTER THE JANUARY 23,2024 Wushi MS7.1 EARTHQUAKE
Using the mobile gravity observation data after Wushi MS7.1 earthquake in the South Tianshan area,the gravity field changes in the South Tianshan area before and after Wushi MS7.1 earthquake were obtained,and the 1-year and multi-year scale gravity changes before and after the earthquake in the area were studied.The results show that after the Wushi earthquake,the zero iso-line of gravity change passes through the epicenter area and a high gradient zone of gravity change appears.In the area where the zero contour of gravity change appears,the material density is under-going a transition process of increasing and decreasing.The difference in material increase and de-crease leads to strong movement and energy accumulation.The gravity anomaly before strong earth-quakes may last for a long time,and there may be a small change in the gravity field.Therefore,when extracting and analyzing the gravity anomaly signal before strong earthquakes,it is necessary to consider the gravity observation data with a long time span.The mobile gravity data observed after the earthquake can better reflect the stress release characteristics of the seismogenic fault,which is helpful to analyze the development trend of aftershocks.

Southern TianshanWushi MS7.1 earthquakeBayesian methodGravity field varia-tion

李秉烨、艾力夏提·玉山、刘代芹、陈丽、阿卜杜塔伊尔·亚森、阿尔达克·卡德尔别克、赵磊

展开 >

新疆维吾尔自治区地震局,新疆乌鲁木齐 830011

南天山 乌什MS7.1地震 贝叶斯平差 重力场变化

2024

内陆地震
新疆维吾尔自治区地震局

内陆地震

影响因子:0.495
ISSN:1001-8956
年,卷(期):2024.38(4)