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Analysis of Temporal and Spatial Variation of Crustal Strain Around Longmenshan Fault Based on GNSS Observation

机译:基于GNSS观测的龙门山断裂带地壳应变时空变化分析。

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The Longmenshan fault zone is located in the transition zone between the eastern margin of Qinghai-Xizang Plateau and Sichuan Basin. It is an important part of the north-south seismic belt in China, and the tectonic activity is frequent, and the 2008 Wenchuan earthquake and the 2013 Ya'an earthquake are all on the tectonic fault. In this paper, the coordinates' time series and velocity fields in the region with high precision are obtained based on GAMIT/GLOBK. The strain parameters in the region are calculated by using the strain model and the high-precision dynamic model of the fault zone and the surrounding crust are constructed, and the time-space distribution of the abnormal information of the fault zone is extracted and analyzed with the reference of the earthquake such as Wenchuan and Ya'an. The study in this paper can be used as a reference for the analysis of crustal movement characteristics and the assessment of geological hazards in Sichuan-Yunnan region.
机译:龙门山断裂带位于青藏高原东缘与四川盆地之间的过渡带。它是中国南北地震带的重要组成部分,构造活动频繁,2008年汶川地震和2013年雅安地震均处于构造断裂上。本文基于GAMIT / GLOBK,获得了该区域坐标的时间序列和速度场。利用应变模型计算出该区域的应变参数,构造了断层带及周围地壳的高精度动力学模型,提取了断层带异常信息的时空分布,并进行了分析。汶川,雅安等地震的参考。本文的研究可为川滇地区地壳运动特征分析和地质灾害评估提供参考。

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