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Location of moderate-sized earthquakes recorded by the NARS-Baja array in the gulf of California region between 2002 and 2006

机译:NARS-Baja阵列记录的2002年至2006年加利福尼亚湾地区中度地震的位置

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We relocated the hypocentral coordinates of small to moderate-sized earthquakes reported by the National Earthquake Information Center (NEIC) between April 2002 and August 2006 in the Gulf of California region and recorded by the broadband stations of the network of autonomously recording seismographs (NARS-Baja array). The NARS-Baja array consists of 19 stations installed in the Baja California peninsula, Sonora and Sinaloa, Mexico. The events reported by the preliminary determinations of epicenters (PDE) catalog within the period of interest have moment magnitudes (Mw) ranging between 1.1 and 6.7. We estimated the hypocentral location of these events using P and S wave arrivals recorded by the regional broadband stations of the NARS-Baja and the RESBAN (Red Sismológica de Banda Ancha) arrays and using a standard location procedure with the HYPOCENTER code (LIENERT and HAVSKOV in Seism Res Lett 66:26-36, 1995) as a preliminary step. To refine the location of the initial hypocenters, we used the shrinking box source-specific station term method of LIN and SHEARER (J Geophys Res 110, B04304, 2005). We found that most of the seismicity is distributed in the NW-SE direction along the axis of the Gulf of California, following a linear trend that, from north to south, steps southward near the main basins (Wagner, Delfin, Guaymas, Carmen, Farallon, Pescadero and Alarcon) and spreading centers. We compared the epicentral locations reported in the PDE with the locations obtained using regional arrival times, and we found that earthquakes with magnitudes in the range 3.2-5.0 mb differ on the average by as much as 43 km. For the Mw magnitude range between 5 and 6.7 the discrepancy is less, differing on the average by about 25 km. We found that the relocated epicenters correlate well with the main bathymetric features of the Gulf.
机译:我们重新布置了2002年4月至2006年8月美国国家地震信息中心(NEIC)在加利福尼亚湾地区报告的中小型地震的震中坐标,并通过自动记录地震仪(NARS- Baja阵列)。 NARS-Baja阵列由19个台站组成,安装在加利福尼亚州下萨半岛,索诺拉和墨西哥锡那罗亚州。由震中的初步确定(PDE)目录所报告的事件在感兴趣的时间范围内的矩量级(Mw)在1.1到6.7之间。我们使用NARS-Baja和RESBAN(RedSismológicade Banda Ancha)阵列的区域宽带站记录的P和S波到达以及使用带有HYPOCENTER码(LIENERT和HAVSKOV)的标准定位程序,估算了这些事件的震中位置。 (Seism Res Lett 66:26-36,1995)作为初步步骤。为了优化初始震源的位置,我们使用了LIN和SHEARER的收缩盒源特定测站项方法(J Geophys Res 110,B04304,2005)。我们发现,大部分地震活动都沿着加利福尼亚湾的轴线沿NW-SE方向分布,呈线性趋势,即从北向南,在主要盆地(Wagner,Delfin,Guaymas,Carmen, Farallon,Pescadero和Alarcon)和传播中心。我们将PDE中报告的震中位置与使用区域到达时间获得的位置进行了比较,我们发现,震级在3.2-5.0 mb之间的地震平均相差43 km。对于介于5和6.7之间的Mw幅度范围,差异较小,平均差异约为25 km。我们发现,搬迁的震中与海湾的主要测深特征很好地相关。

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