首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Large-scale relocation of two decades of Northern California seismicity using cross-correlation and double-difference methods
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Large-scale relocation of two decades of Northern California seismicity using cross-correlation and double-difference methods

机译:使用互相关和双差方法对北加州二十年地震活动进行大规模搬迁

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We simultaneously reanalyzed two decades (1984–2003) of the digital seismic archive of Northern California using waveform cross-correlation (CC) and double-difference (DD) methods to improve the resolution in hypocenter locations in the existing earthquake catalog generated at the Northern California Seismic Network (NCSN) by up to three orders of magnitude. We used a combination of ~3 billion CC differential times measured from all correlated pairs of events that are separated by less than 5 km and ~7 million P wave arrival-time picks listed in the NCSN bulletin. Data were inverted for precise relative locations of 311,273 events using the DD method. The relocated catalog is able to image the fine-scale structure of seismicity associated with active faults and revealed characteristic spatiotemporal structures such as streaks and repeating earthquakes. We found that 90% of the earthquakes have correlated P wave and S wave trains at common stations and that 12% are colocated repeating events. An analysis of the repeating events indicates that uncertainties at the 95% confidence level in the existing network locations are on average 0.7 km laterally and 2 km vertically. Correlation characteristics and relative location improvement are remarkably similar across most of Northern California, implying the general applicability of these techniques to image high-resolution seismicity caused by a variety of plate tectonic and anthropogenic processes. We show that consistent long-term seismic monitoring and data archiving practices are key to increase resolution in existing hypocenter catalogs and to estimate the precise location of future events on a routine basis.
机译:我们同时使用波形互相关(CC)和双差(DD)方法重新分析了北加利福尼亚州的二十个十年(1984-2003年)的数字地震档案,以提高北部地区现有地震目录中震源位置的分辨率。加州地震台网(NCSN)的数量最多增加了三个数量级。我们使用了从相距不到5公里的所有相关事件对中测得的〜30亿个CC差动时间和NCSN公告中列出的〜700万个P波到达时间的组合。使用DD方法对311,273个事件的精确相对位置进行数据反转。重新定位的目录能够对与活动断层有关的地震活动的精细尺度结构进行成像,并揭示出特征性的时空结构,例如条纹和重复地震。我们发现90%的地震在公共站点关联了P波和S波列,而12%是同一地点的重复事件。对重复事件的分析表明,现有网络位置的95%置信水平上的不确定性平均在侧向0.7 km,在垂直2 km。在北加州的大部分地区,相关特征和相对位置的改善非常相似,这意味着这些技术普遍适用于成像由各种板块构造和人为过程引起的高分辨率地震活动。我们表明,一致的长期地震监测和数据归档做法对于提高现有震源目录中的分辨率并按常规估算未来事件的精确位置至关重要。

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