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首页> 外文期刊>Earth sciences research journal >ACTIVITY AND Vp/Vs RATIO OF VOLCANO-TECTONIC SEISMIC SWARM ZONES AT NEVADO DEL RUIZ VOLCANO, COLOMBIA
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ACTIVITY AND Vp/Vs RATIO OF VOLCANO-TECTONIC SEISMIC SWARM ZONES AT NEVADO DEL RUIZ VOLCANO, COLOMBIA

机译:哥伦比亚内瓦多·德尔·鲁伊斯火山的火山构造地震带的活动性和Vp / Vs比

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An analysis of the seismic activity for volcano-tectonic earthquake (VT) swarms zones at Nevado del Ruiz Volcano (NRV) was carried out for the interval 1985- 2002, which is the most seismic active period at NRV until now (2010). The swarm-like seismicity of NRV was frequently concentrated in very well defined clusters around the volcano. The seismic swarm zone located at the active crater was the most active during the entire time. The seismic swarm zone located to the west of the volcano suggested some relationship with the volcanic crises. It was active before and after the two eruptions occurred in November 1985 and September 1989. It is believed that this seismic activity may be used as a monitoring tool of volcanic activity. For each seismic swarm zone the Vp/Vs ratio was also calculated by grouping of earthquakes and stations. It was found that each seismic swarm zone had a distinct Vp/Vs ratio with respect to the others, except for the crater and west swarm zones, which had the same value. The average Vp/Vs ratios for the seismic swarm zones located at the active crater and to the west of the volcano are about 6-7% lower than that for the north swarm zone, and about 3% lower than that for the south swarm zone. We suggest that the reduction of the Vp/Vs ratio is due to degassing phenomena inside the central and western earthquake swarm zones, or due to the presence of microcracks inside the volcano. This supposition is in agreement with other studies of geophysics, geochemistry and drilling surveys carried out at NRV.
机译:在1985年至2002年之间对内瓦多·德尔·鲁伊斯火山(NRV)的火山构造地震(VT)震群进行了地震活动分析,这是迄今为止(2010年)NRV地震活动最活跃的时期。 NRV的群状地震活动经常集中在火山周围非常明确的集群中。在整个时间内,位于活动火山口的地震群带最为活跃。位于火山西侧的地震群带暗示了与火山危机的某种联系。它在1985年11月和1989年9月的两次喷发之前和之后都是活跃的。据信,这种地震活动可以用作火山活动的监测工具。对于每个地震群带,也通过对地震和台站进行分组来计算Vp / Vs比。结果发现,除了火山口区和西区群具有相同的值外,每个地震群区相对于其他地震区都具有不同的Vp / Vs比。位于活动火山口和火山西侧的地震群区的平均Vp / Vs比比北部群区低约6-7%,比南部群区低3%。 。我们认为,Vp / Vs比的降低是由于中西部地震群内部的脱气现象,或者是由于火山内部存在微裂纹。这种假设与在NRV进行的其他地球物理学,地球化学和钻探研究有关。

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