首页> 外文期刊>Geophysical Research Letters >Seismic image and its implications for an earthquake swarm at an active volcanic region off the Miyake-jima-Kozu-shima, Japan - art. no. 1548
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Seismic image and its implications for an earthquake swarm at an active volcanic region off the Miyake-jima-Kozu-shima, Japan - art. no. 1548

机译:日本三宅一岛-小津岛附近活跃火山区的地震图像及其对地震群的影响-艺术。没有。 1548

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1] An intensive earthquake swarm, which is proposed to be attributed to the magmatic activity, has continued in more than six months around the Miyake-jima-Kozu-shima. A wide-angle seismic survey was conducted immediately above the swarm. The purpose of this study is to map the seismic velocity structure of the swarm area, and to investigate structural evidence indicating magmatic activity. From the result of first arrival refraction tomography, we found a 5-8% decrease in P-wave velocity surrounding the swarm. A depth migration of the intra-crustal reflection phase also shows an existence of a reflector immediately below the swarm (10-13 km depth). Compared with the seismic imaging, geodetic data and earthquake focal mechanisms, the intra-crustal reflector we found might be the top of magmatic body which has caused the earthquake swarm between Miyake-jima and Kozushima. [References: 11
机译:[1]拟归因于岩浆活动的强烈地震群在三宅一岛-驹津岛周围持续了六个多月。在蜂群上方立即进行了广角地震勘测。这项研究的目的是绘制群体区域的地震速度结构图,并研究表明岩浆活动的结构证据。从首次到达折射层析成像的结果来看,我们发现群周围的P波速度降低了5-8%。地壳内反射相的深度偏移也表明在群下方(深度10-13 km)存在反射器。与地震成像,大地测量数据和地震震源机制相比,我们发现地壳内反射器可能是造成岩田三宅岛和小岛之间地震群的岩浆体顶部。 [参考:11

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