首页> 外文期刊>Journal of Volcanology and Geothermal Research >Seismic velocity structure and earthquake relocation for the magmatic system beneath Long Valley Caldera, eastern California
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Seismic velocity structure and earthquake relocation for the magmatic system beneath Long Valley Caldera, eastern California

机译:加利福尼亚东部长谷火山口下岩浆系统的地震速度结构和地震迁移

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A new three-dimensional (3-D) seismic velocity model and high-precision location catalog for earthquakes between 1984 and 2014 are presented for Long Valley Caldera and its adjacent fault zones in eastern California. The simul2000 tomography algorithm is applied to derive the 3-D V-p and V-p/V-s models using first-arrivals of 1004 composite earthquakes obtained from the original seismic data at the Northern California Earthquake Data Center. The resulting V-p model reflects geological structures and agrees with previous local tomographic studies. The simultaneously resolved V-p/V-s model is a major contribution of this study providing an important complement to the V-p model for the interpretation of structural heterogeneities and physical properties in the study area. The caldera is dominated by low V-p anomalies at shallow depths due to postcaldera fill. High V-p and low V-p/V-s values are resolved from the surface to similar to 3.4 km depth beneath the center of the caldera, corresponding to the structural uplift of the Resurgent Dome. An aseismic body with low V-p and high V-p/V-s anomalies at 4.2-6.2 km depth below the surface is consistent with the location of partial melt suggested by previous studies based on V-p models only and the inflation source locations based on geodetic modeling. The Sierran crystalline rocks outside the caldera are generally characterized with high V-p and low V-p/V-s values. The newly resolved velocity model improves absolute location accuracy for the seismicity in the study area and ultimately provides the basis for a high-precision earthquake catalog based on similar-event cluster analysis and waveform cross-correlation data. The fine-scale velocity structure and precise earthquake relocations are useful for investigating magma sources, seismicity and stress interaction and other seismological studies in Long Valley. (C) 2015 Elsevier B.V. All rights reserved.
机译:针对长谷火山口及其附近断层带,提出了一个新的三维(3-D)地震速度模型和1984年至2014年之间地震的高精度位置目录。使用simul2000层析成像算法,使用从北加利福尼亚地震数据中心的原始地震数据获得的1004次复合地震的第一批到达来推导出3-D V-p和V-p / V-s模型。最终的V-p模型反映了地质结构,并与以前的局部层析成像研究一致。同时解析的V-p / V-s模型是这项研究的主要贡献,为解释研究区域的结构异质性和物理性质提供了重要的补充,为V-p模型提供了补充。由于火山口填充,火山口被浅层深度低的V-p异常所控制。高V-p和低V-p / V-s值从表面解析为破火山口中心下方约3.4 km的深度,这与Resurgent Dome的结构隆起相对应。在地表以下4.2-6.2 km深度处具有低V-p和高V-p / V-s异常的抗震体与先前仅基于V-p模型的研究以及基于大地测量模型的充气源位置所建议的部分熔融位置一致。破火山口外的Sierran晶体岩石通常具有高的V-p和低的V-p / V-s值。新近解析的速度模型提高了研究地区地震活动的绝对定位精度,并最终为基于相似事件聚类分析和波形互相关数据的高精度地震目录提供了基础。精细的速度结构和精确的地震定位对于调查Long谷的岩浆源,地震活动和应力相互作用以及其他地震学研究很有用。 (C)2015 Elsevier B.V.保留所有权利。

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