首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Repeated fluid-transfer episodes as a mechanism for the recent dynamics of Campi Flegrei caldera (1989-2010)
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Repeated fluid-transfer episodes as a mechanism for the recent dynamics of Campi Flegrei caldera (1989-2010)

机译:重复的液体转移事件是Campi Flegrei破火山口(1989-2010)近期动态的一种机制

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We have analyzed a multiparametric data set of seismological, geodetic and geochemical data recorded at Campi Flegrei caldera since 1982. We focus here on the period 1989-2010 that followed the last bradyseismic crisis of 1982-1984. Since then, there have been at least five repeated minor episodes of ground uplift accompanied by seismicity. We have reanalyzed old paper and digital seismic data sets dating back to 1982. The paper recordings show evidence of long-period events in January 1982 and March 1989, and we have digitized some of these significant waveforms. Furthermore, the revision of digital seismograms dating back to 1994 shows a significant swarm of long-period events in August 1994. Volcano-tectonic and long-period events hypocenters have been relocated in a three-dimensional velocity model. Statistical analysis of volcano-tectonic seismicity shows many similarities and few differences between 1982-1984 and the following period 1989-2010. Long-period waveforms have been analyzed using spectral analysis, which shows a grouping into three macrofamilies. Similarities in the seismic signature of episodes of minor uplift suggest that they originate from the injection of fluids into the deep part of a geothermal reservoir (about 2.5 km depth) and in its transfer toward a shallower part (about 0.75 km depth). Most of the observed geophysical signals are related to this second phase. The evidence consists of spatial and temporal connections between the ground deformation, long-period and volcano-tectonic seismicity and changes in the geochemical parameters of fumaroles. In this study we focused our analysis on two uplift episodes observed in 2000 and 2006. The joint inversion of Differential Synthetic Aperture Radar (DInSAR) and tiltmeter data show that during these periods the ground deformation was generated by at least two distinct sources located at different depths, with the shallower activated in the later stages of the uplift episodes. Our interpretation of the recent dynamics of Campi Flegrei is that the deep part of the geothermal reservoir inflates in response to mass and heat input from a magmatic source. When the pressure exceeds a threshold, fluids starts to migrate into the shallower part. During this transfer, long-period sources are activated in response to the fluid motion. The gradual diffusion of fluids in the surrounding rocks lowers the resistance of a pervasive fracture system generating shallow microseismicity. Finally, fluids reach the surface, which gives a distinct geochemical signature to the overlying fumaroles.
机译:我们分析了自1982年以来在Campi Flegrei破火山口记录的地震,大地测量和地球化学数据的多参数数据集。在此,我们重点介绍的是1982-1984年最后一次缓震危机之后的1989-2010年。从那时起,至少有五次重复的轻微地面隆起并伴有地震活动。我们重新分析了可追溯到1982年的旧纸张和数字地震数据集。这些纸张记录显示了1982年1月和1989年3月发生的长期事件的证据,并且我们已经数字化了其中一些重要波形。此外,可追溯到1994年的数字地震图的修订版显示了1994年8月发生的大量长期事件。火山构造和长期事件震源已在三维速度模型中重新定位。火山构造地震活动性的统计分析显示,1982年至1984年与随后的1989年至2010年之间有很多相似之处,几乎没有区别。长期波形已使用频谱分析进行了分析,显示出分为三个大家族。轻微隆起事件的地震特征相似,表明它们的产生是由于将流体注入地热储层的深部(约2.5 km深度),并向较浅的部分(约0.75 km深度)转移。大多数观测到的地球物理信号都与第二阶段有关。证据包括地面变形,长时期和火山构造地震活动性与喷气孔地球化学参数变化之间的时空联系。在这项研究中,我们将分析重点放在2000年和2006年观测到的两个隆起事件上。差分合成孔径雷达(DInSAR)和倾斜仪数据的联合反演表明,在这些时期,地面变形是由位于不同位置的至少两个不同源产生的。深度,在上升事件的后期激活浅层。我们对Campi Flegrei近期动态的解释是,地热储层的深部会因岩浆源的质量和热量输入而膨胀。当压力超过阈值时,流体开始迁移到较浅的部分。在该传输期间,响应于流体运动激活了长周期源。流体在围岩中的逐渐扩散降低了产生浅微地震的普遍裂缝系统的阻力。最后,流体到达地表,这为上覆的富马mar提供了独特的地球化学特征。

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