摘要
We evaluated 2011-2015 mobile relative gravity data from the Hexi monitoring network that covers the epicenter of the 2016 Menyuan Ms6.4 earthquake, Qinghai Province, China and examined the spatiotemporal characteristics of the gravity field at the focal depth. In addition, we assessed the regional gravity field and its variation the half-year before the earthquake. We use first different interpolation algorithms to build a grid for the gravity data and then introduce potential field interpolation-cutting separation techniques and adaptive noise filtering. The results suggest that the gravity filed at the focal depth of 11.12 km separated from the total gravity field at about -400-150 ×10^-8 m/s^2 in the second half of 2015, which is larger than that in the same period in 2011 to 2014 （±30×10^-8 m/s^2）. Moreover, at the same time, the gravity field changed fast from September 2014 to May 2015 and May 2015 to September 2015, reflecting to some extent material migration deep in the crust before the Menyuan earthquake.
本文基于覆盖2016年1月21日中国青海省门源县M6.4级地震的河西地区2011年至2015年每年两期的流动重力网观测资料,根据不同的拟合插值算法进行了区域重力位场值网格化方法优选,并通过引人应用于资源勘探领域中的插值切割位场分离算法(改进了边缘点和角点的处理)和图像处理领域的自适应噪声滤除技术,解算了门源M6.4级地震发生前,在震源深度层附近的区域重力场时空演化特征及研究区域重力观测点的半年尺度变化量,解算结果发现,在震源深度范围(-11.12 km)分离的重力位场自2015年下半年,重力变化达到-400^+150x l0-8m/s^2量级左右,大于2011年至2014年同期的变化结果(±30xl0-8m/s^2);半年尺度(2014年9月至2015年5月以及2015年5月至2015年9月)重力观测点值变化趋势也验证了门源地震前重力加速变化的特征,这可能在一定程度上显示了门源地震发震前地壳内部物质运移等地质活动在地表重力场上的反映。
基金
supported by the Science for Earthquake Resilience(No.XH17058Y)
Science and Technology Innovation Fund of the First Crust Monitoring and Application Center,CEA(No.FMC2016004)
Special Program for Basic Work of the Ministry of Science and Technology,China(No.2015FY210403)
作者简介
Corresponding author： Liu Jin-Zhao （E-mail： whiggliujinzhao@126.com）
