利用北天山地区2016～2019年观测的4期流动重力观测资料，分析研究一年尺度的重力场动态变化特征，并利用小波分析方法，将不同场源深度的重力异常进行分离。通过功率谱分析，获取各阶小波重力细节对应的场源深度。研究结果表明，2017年8月9日精河M_S6.6地震前，震中位于负值集中区，四阶小波重力细节显示震中附近出现明显的四象限分布；2020年1月16日库车M_S5.6地震前，震中位于负值区，小波重力细节整体量值较小；功率谱估算的场源近似深度与2次地震的震源深度相近。

Using the four-period mobile gravity observation data from 2016 to 2019 in Northern Tianshan mountain we analyze the dynamic characteristics of one year scale gravity field,and defined the gravitational anomalies at different depths with the wavelet decomposition method. Utilizing the power spectrum analysis we obtained the depth of field source corresponding to each order of wavelet gravity details. The results show that there existed negative gravity changes with high value around the epicenter before Jinghe M_S6.6 earthquake on August 9,2017,in which the 4th order wavelet details showed an obvious four-quadrant distribution near the epicenter. Moreover,the epicenter of Kuqa M_S5.6 earthquake on January 16,2020 was also located in negative gravity area,and the values of wavelet details were relatively small. The depth of the field source estimated by the power spectrum is close to the focal depth of two earthquakes.

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震情跟踪定向工作任务（2020010222）、国家自然科学基金（41874015）、地震科技星火计划（XH18054、XH20069Y）、新疆维吾尔自治区自然科学基金（2020D01A85）、中国地震局“监测、预报、科研”三结合课题（3JH-202002024）和新疆杰出青年自然科学基金项目（2017Q010）共同资助