格连吉克黑海沿岸段地表低频形变的现场观测

作者

  • I. S. Podymov Shirshov Institute of Oceanology, Russian Academy of Sciences
  • T. M. Podymova Shirshov Institute of Oceanology, Russian Academy of Sciences

DOI:

https://doi.org/10.29006/1564-2291.JOR-2026.54(2).4

关键词:

氡-222, 地表, 局部形变, 黑海沿岸, 测地定位, 地球物理过程, 氡体积活度

摘要

本文介绍了对近地表大气中氡波动进行长期连续监测的成果。所获数据已成为区域地震稳定性研究以 及地表当前和长期形变过程研究的重要组成部分。为评估地表垂直形变幅度与氡体积活度变化之间的关 系,采用了卫星测地定位站的数据。通过分析长期实验资料,构建了关联这些参数的数学模型。数据记录 方法的特点是采用氡体积活度变化光谱测量法。上述研究的硬件和软件系统能够实现氡变化的逐小时记 录,并以毫米级精度测量地表垂直形变幅度。

参考


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已出版

2026-06-30

期次

栏目

海洋地质学、地球物理学与地球化学

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