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首页> 外文期刊>Bollettino di Geofisica Teorica ed Applicata >On the origin of micro-earthquakes in geothermal areas (OMEGA): first results from a seismic experiment at Mt. Amiata (Italy)
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On the origin of micro-earthquakes in geothermal areas (OMEGA): first results from a seismic experiment at Mt. Amiata (Italy)

机译:关于地热地区的微地震起源(Omega):Mt. Amiata(意大利)的地震实验中的首先结果

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摘要

In a joint project called OMEGA, between GFZ-Potsdam and the Istituto Nazionale di Geofisica e Vulcanologia (INGV), an experimental seismic monitoring system was installed in 2015 near the power plants of the geothermal area of Mt. Amiata (central Italy). The main objectives of this three-year experiment are: i) to monitor the seismic activity connected to any type of seismicity inside the geothermal field, ii) to verify if the low local seismicity rate near Mt. Amiata reported by the INGV bulletin is natural, or due to the sparse distribution of the INGV network, and iii) to discriminate natural from possibly induced seismicity. The eight-station network was extended by a sevenelement seismic array for the first four weeks. The aim of this paper is to present the first automatic hypocentre locations of the joint network/array analysis.
机译:在一个名为Omega的联合项目中,GFZ-Potsdam和Istituto Nazionale di Geofisica u ulcanologia(Ingv)之间,2015年安装了一个实验地震监测系统,附近Mt.Mt.Amiata(意大利中部)的电力厂。 这个三年实验的主要目标是:i)监测连接到地热场中的任何类型的地震性的地震活动,ii)以验证在山INGV公告附近的近型局部地震性率是否是天然的。 ,或由于INGV网络的稀疏分布和III)以可能诱导的地震性区分自然。 前四周的七个地震阵列延伸了八站网络。 本文的目的是介绍联合网络/阵列分析的第一个自动低频期子位置。

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