一种更加严密的GNSS台站位移热弹性效应模型

GNSS基准站天线观测墩及其所在基岩会随地表温度变化产生热弹性形变,并累积为GNSS台站的位移.热弹性效应的定量分析对于准确分离GNSS基准站坐标时间序列中的信号和噪声具有重要意义.基于弹性力学和热弹性力学的相关理论,给出一维温度场下轴对称观测墩热弹性形变的解析解.结果表明,观测墩的垂向位移由观测墩和基岩的泊松比、热膨...     

高频GNSS形变波的震相识别：模拟实验与实例分析

高频GNSS震时形变波震相及识别是GNSS地震学的重要内容.在实时数据处理基础上,本文利用振动台的高频GNSS观测实验,并结合近期部分大震的高频GNSS形变波震相特征进行研究.数据处理结果表明,实时处理与事后处理的精度在同一量级,且与采样率无关.通过与同址观测强震仪和地震计记录的对比及特定震相的频谱分析,发现高频GNSS可完整记录P波、S波、Love波及Rayleigh波震相,影响震相记录的主要因素是GNSS定位精度与震级,而仅当震中距很小时,采样率将产生一定影响.研究结果得出：基于地震波传播规律,利用高频GNSS台阵记录的形变波空间分段特征,结合震相运动轨迹及其他地震波记录,可实现实时高频GNSS形变波的震相识别.     

GNSS在断层形变研究中的应用

Great earthquakes often occur along or near active fault belts. Thus, monitoring and research on fault deformation are quite important. Methods such as short-leveling, short- baseline and integrated monitoring profile across fault belts have been used to monitor fault activities for many years. GNSS observations are mainly used to obtain the horizontal velocity field in large areas and to study the activities and deformation of major blocks. GNSS technology has been used to monitor and study the deformation of faults from a different aspects, In this paper, some applications and new explorations of GNSS are discussed. They are： （1） Research and monitoring of strike-slip activities of faults with GNSS. （2） Research and monitoring of vertical activities of faults with GNSS. （3） Investigating the laws of deformation of blocks on the sides of fault zone and setting up strain models to deduce the activities and deformation of faults with respective models and compare the deduced results with the actual measurements across fault. It is concluded that a larger discrepancy between the deduced and the observed deformation indicates a stronger interaction between the blocks, which can be important for predicting the location of a strong earthquake and assessing seismic hazard, as well as the seismicity trend.     

GNSS在断层形变研究中的应用

大地震多发生在主要活动断裂带及其附近, 因此断层形变的监测与研究非常重要。 多年来采用跨断层短水准、 短基线、 跨断裂带综合观测剖面等手段监测断层活动, 进而研究断层活动与变形规律。 GNSS多用于大面积地壳水平运动场和主要地块活动与变形的研究, 随着GNSS数据的积累和应用研究的深入, 已有学者用GNSS从不同角度开展断层形变的监测与研究。 本文介绍和论述了GNSS在断层形变研究中已有的部分应用和新的探索, 主要介绍以下几个方面: ① GNSS用于断层走滑活动的监测与研究; ② GNSS用于断层垂直活动的监测与研究; ③ 通过研究断层两边地块变形规律并建立应变模型, 可分别依据各自模型推测断层的活动与形变, 将推测结果与跨断层观测到的实际情况进行研究与比较。 研究分析认为, 由块体推测的变形与实测变形差异越大, 说明块体相互作用越强烈。 这可能对强地震地点预测、 地震危险性判定及地震趋势预测均有重要意义。     

基于GNSS和定点形变观测分析日本Mw 9.0地震对黑龙江地区地壳形变的影响

结合GNSS和黑龙江地区定点形变观测,分析日本2011年3月11日Mw9.0地震对黑龙江地区地壳形变的影响.结果显示:日本Mw9.0地震引起哈尔滨站、绥阳站震后2年内运动速率明显增加(哈尔滨站增大4 mm/a,绥阳站速率增大6 mm/a);定点形变与GPS观测到的同震效应至少在4个台站多种仪器均具有较好的一致性;日本Mw 9.0地震不仅引起区域水平向应变变化,对垂直向也产生一定影响;长基线变化反映出日本Mw9.0地震引起的大空间尺度应变变化与黑龙江地区长期构造应力场背景一致,该地震对黑龙江地区地表应变积累可能有增强影响.     

���ػ�׼վ�����������ڱ仯����

???ü???GNSS????10??????????????????GPS????????????????????????仯???μ????????仯???????????????????????????仯????????????????????????????????С?????????м?????????п??????Ч?????????????????????????????????????????????     

���ʸ�ƵGNSS���ݹ���ʱ�շֲ�����

???????6?????л?????????GNSS?????????????????????????????????????????GNSS??????????????о??е???á?     

����ȱʧ��GNSSʱ�����з�����Ӱ��

??GNSS?????????????????????????????????????????????????????GNSS??????з??????????????????????????????????????????????????????????????????????????????????????????????????????????????????????￡??????????????????????????????????????岹??????????????????????????????????????????????????????????????????????????????????????????????????????????仯??????￡?????????????????й????????????????????10%??????統???????9 mm???????????????????11???????????????12?????????GNSS????????????????о???????????????GNSS??????????????????????????     

DOPֵ����GNSS��Զ�λԤ�����������о�

????GNSSα????λ??????λ?????????????????λ????????DOP???????λ????????RDOP??????????????????????????????????仯?????????????DOP????GNSS????λ????????÷?Χ??????????????DOP??RDOP?????????仯??????????????￡????????????????????????????????????????????????DOP?????????λ????????????????????RDOP?????????λ?????????     

������������������JPL DE�����ļ򻯼�Ӧ���о�

????JPL DE?????????洢??????????????????????????????????DE??????????????????????????20???DE406?????????????369 kb????????1/6????GPS??????????ü???DE????????????????????飬?????????60?????????????????????3 m???ü??????????????????????????????????????????????С?????????洢??????????????????????Ч???