首页> 外文期刊>Journal of Volcanology and Geothermal Research >Local earthquake tomography with the inclusion of full topography and its application to Kilauea volcano, Hawai'i
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Local earthquake tomography with the inclusion of full topography and its application to Kilauea volcano, Hawai'i

机译:包含完整地形的局部地震层析成像及其在夏威夷基拉韦厄火山中的应用

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摘要

We develop a new three-dimensional local earthquake tomography algorithm with the inclusion of full topography (LETFT). We present both synthetic and real data tests based on the P- and S-wave arrival time data for Kilauea volcano in Hawaii. A total of 33,768 events with 515,711 P-picks and 272,217 S-picks recorded by 35 stations at the Hawaiian Volcano Observatory are used in these tests. The comparison between the new and traditional methods based on the synthetic test shows that our new algorithm significantly improves the accuracy of the velocity model, especially at shallow depths. In the real data application, the P- and S-wave velocity models of Kilauea show several intriguing features. We observe discontinuous high Vp (>7.0 km/s) and Vs (>3.9 km/s) zones at 5-14 km depth below Kilauea caldera, its East Rift Zone (ERZ) and the Southwest Rift Zone, which may represent consolidated intrusive gabbro-ultramafic cumulates. At Kilauea caldera, Vp and Vs decrease from similar to 3.9 km/s and similar to 2.6 km/s from the surface to similar to 3.7 km/s and similar to 2.3 km/s at 2 km depth. We resolve a high Vp zone (>7.0 km/s) at 5-14 km depth and high Vs zone (>3.9 km/s) at 5-11 km depth. This high Vp and Vs zone extends to the north of the ERZ at 5-10 km depth and to the upper ERZ at 8-12 km depth. In the Hilina Fault System, there is a high Vp layer (similar to 7.0 km/s) at 4-6 km depth and a low Vp body of similar to 5.7 km/s at 6-11 km depth. The high Vp layer could be associated with the intrusive ultramafic gabbro sills. The velocity contrast on the north and south sides of the Koa'e Fault System indicates that the intrusive activities mainly occur to the north of the fault. Our new LETFT method performs well in both the synthetic and real data tests and we expect that it will reveal more robust velocity structures in areas with larger topographic variations. (C) 2016 Elsevier B.V. All rights reserved.
机译:我们开发了一种包含全地形(LETFT)的新型三维局部地震层析成像算法。我们基于夏威夷基拉韦厄火山的P波和S波到达时间数据,提供了合成和真实数据测试。这些测试总共使用了33,768个事件,其中35个站记录了515,711个P点和272,217个S点。基于综合测试的新方法与传统方法的比较表明,我们的新算法显着提高了速度模型的精度,尤其是在浅深度时。在实际数据应用中,基拉韦厄的P波和S波速度模型显示了几个有趣的特征。我们在基拉韦厄火山口,其东裂谷带(ERZ)和西南裂谷带以下5-14 km处观察到了不连续的高Vp(> 7.0 km / s)和Vs(> 3.9 km / s)区域,这可能代表了整合侵入性辉长岩超累加。在基拉韦厄火山口,Vp和Vs从地表下降到大约3.9 km / s和大约2.6 km / s,在2 km深度处下降到大约3.7 km / s和大约2.3 km / s。我们解析了5-14 km深度的高Vp区(> 7.0 km / s)和5-11 km深度的高Vs区(> 3.9 km / s)。高Vp和Vs区域延伸到ERZ的北部,深度为5-10 km,延伸到上部ERZ,深度为8-12 km。在Hilina断层系统中,在4-6 km深度处有一个高Vp层(约7.0 km / s),在6-11 km深度处有一个低Vp体(类似于5.7 km / s)。高Vp层可能与侵入性超镁铁辉长岩基岩有关。 Koa'e断层系统南北两侧的速度对比表明,侵入活动主要发生在断层以北。我们的新LETFT方法在综合和真实数据测试中均表现良好,我们希望它将在具有较大地形变化的区域中显示出更鲁棒的速度结构。 (C)2016 Elsevier B.V.保留所有权利。

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