火山构造主动振动地震方法的实验研究与模拟

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
B. M. Glinskiy, V. V. Kovalevsky, M. S. Khairetdinov, A. G. Fatyanov, V. N. Martynov, D. A. Karavaev, A. F. Sapetina, A. L. Sobisevich, L. E. Sobisevich, L. P. Braginskaya, A. P. Grigoryuk
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引用次数: 0

摘要

本文综述了利用振动器作为弹性波源的火山构造地震场的实验研究和模拟工作。本文回顾了俄罗斯科学院西伯利亚分院计算数学与数学地球物理研究所(ICM&MG)开展的泥火山实验研究成果;地球物理研究所(IPE);以及塔曼泥火山省的库班国立大学使用振动器进行的研究。我们在非均质地球物理介质中进行了数学模拟,以完善被调查对象的结构信息,以及地震场的显著特征。我们已经开发了一种数学方法来处理模拟具有任意几何形状的泥火山的振动地震探测,包括深部断层,重叠层等知识。数值技术用于求解弹性理论中的方程组,开发并行算法,程序包,以及在高性能计算系统中进行数值实验。本文介绍了蜀谷泥火山震源带的地震场计算结果。本文介绍了为本研究建立的三维和二维地球物理模型,以及对卡拉别托娃戈拉泥火山和厄尔布鲁士岩浆火山地震场的模拟结果。结果表明,本文采用主动振动地震技术开发的方法可以成功地用于实际中,以改进地震场,地球物理模型的深部结构,并研究岩浆房的几何形状和喷发通道的存在对地面观测系统获得的数据的影响。这些研究证明,具有较高周期激发精度的地震震源可以用于火山构造研究和火山活动的主动监测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The Experimental Study and Simulation of Volcanic Structures Using Active Vibroseismic Methods

The Experimental Study and Simulation of Volcanic Structures Using Active Vibroseismic Methods

This paper is a review of our work, an experimental study and simulation of seismic fields in volcanic structures using vibrators as sources of elastic waves. We review the results of experimental studies of mud volcanoes carried out by the Institute of Computational Mathematics and Mathematical Geophysics (ICM&MG) of the Siberian Branch (SB), Russian Academy of Sciences (RAS); by the Institute of Physics of the Earth (IPE), RAS; and by the Kuban State University in the Taman mud-volcanic province using vibrators. We have carried out mathematical simulation in heterogeneous geophysical media to refine the information on the structure of the object under investigation, as well as on the distinguishing features of the seismic field. We have developed a mathematical approach to deal with the simulation of vibroseismic probing of mud volcanoes with arbitrary geometries incorporating knowledge of deep-seated faults, overlapping layers, and so on. Numerical techniques were used to solve sets of equations in elasticity theory and to develop parallel algorithms, program packages, as well as carrying out numerical experiments in high-performance computational systems. We present results from calculations of the seismic field for the source zone of the Shugo mud volcano. This paper describes 3D and 2D geophysical models developed for this study and the results of simulation for the seismic field of the Karabetova Gora mud volcano and for the Elbrus magmatic volcano. It is shown that the approach developed here using active vibroseismic techniques can be successfully used in practice to refine the seismic field, the deep structure of geophysical models, and to study the effects exerted by the geometry of a magma chamber and by the presence of erupting channels on data acquired by an observation system on the ground surface. These studies prove that vibroseismic sources with high accuracies of periodic excitation can be used to study volcanic structures and to conduct active monitoring of volcanic activity.

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来源期刊
Journal of Volcanology and Seismology
Journal of Volcanology and Seismology 地学-地球化学与地球物理
CiteScore
1.50
自引率
28.60%
发文量
27
审稿时长
>12 weeks
期刊介绍: Journal of Volcanology and Seismology publishes theoretical and experimental studies, communications, and reports on volcanic, seismic, geodynamic, and magmatic processes occurring in the areas of island arcs and other active regions of the Earth. In particular, the journal looks at present-day land and submarine volcanic activity; Neogene–Quaternary volcanism; mechanisms of plutonic activity; the geochemistry of volcanic and postvolcanic processes; geothermal systems in volcanic regions; and seismological monitoring. In addition, the journal surveys earthquakes, volcanic eruptions, and techniques for predicting them.
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