Abstract

This paper presents the results of areal seismic studies in the deep structure of the Dzhau Tepe mud volcano, which is the largest of its kind on the Kerch Peninsula. It is the first time that data has been obtained concerning nearly vertical fluid-conducting structures beneath the volcano that supply material onto the ground during more active periods. A new approach is proposed for interpretation of measured relative amplitudes of microseismic noise based on numerical simulation of plane-stratified media. The results derived in this study are compared with previous geological and geophysical data on the area.

中文翻译：

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Dzhau-Tepe泥火山深层结构的新证据

摘要

本文介绍了Dzhau Tepe泥火山深部结构的区域地震研究结果，该火山是刻赤半岛上最大的火山。这是首次获得有关火山下的近乎垂直的导流结构的数据，该结构在更活跃的时期向地面供应物质。提出了一种基于平面分层介质数值模拟解释微震噪声相对振幅的新方法。这项研究得出的结果与该地区以前的地质和地球物理数据进行了比较。