发表机构
Schmidt Institute of Physics of the Earth RAS（俄罗斯科学院地球物理学施密特研究所）
机构由 AI 辅助整理，请以论文原文为准。AI 中文总结
本文提出基于震源失活和固有时间的余震现象学理论，推导出余震活动随固有时间衰减的整体性定律，并分析其逻辑结构与实验结果。
AI 中文摘要
本文致力于研究主震后构造地震震源区发生的余震的现象学理论。该理论由作者与A.D. Zavyalov和O.D. Zotov在长期余震研究过程中共同提出。该理论基于震源失活和震源固有时间的概念。由该理论推导出余震活动随固有时间衰减的整体性定律，其阻尼减缩量等于震源失活系数。本文主要关注该理论逻辑结构的分析，并简要介绍了利用该理论获得的实验结果。关键词：地震震源、余震、大森定律、宇津定律、失活系数、固有时间、地下时钟、前震收敛、余震发散。
英文摘要
The paper is devoted to the phenomenological theory of aftershocks occurring in the source of a tectonic earthquake following the main shock. The theory was developed by the author jointly with A.D. Zavyalov and O.D. Zotov during the course of a long-term study of aftershocks. The theory is based on the concepts of source deactivation and the source's proper time. The holistic law governing the decay of aftershock activity over proper time follows from the theory. The damping decrement is equal to the source deactivation coefficient. The main focus of this paper is the analysis of the logical structure of the theory. The paper also contains a brief description of the experimental results obtained using the theory. Keywords: earthquake source, aftershocks, Omori's law, Utsu's law, deactivation coefficient, proper time, underground clock, foreshock convergence, aftershock divergence.
Comments15 pages
