诱发地震

Nathalie Casas, G. Mollon
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引用次数: 0

摘要

地热技术的主要障碍之一是地震断层或裂缝中的滑动重新激活。用于提高渗透率的增产措施可能引起地震或地震滑动,从而导致微地震活动。研究和认识断层滑动的触发机制,有助于减轻微震活动性。诱发地震活动性既具有挑战性又有趣,它仍然是世界各地所有地能应用和建设的重要研究领域。在这次小型研讨会上,我们希望通过微宏观地震的影响因素和触发机制来关注诱发地震活动的物理学。人们开发了许多方法、模型和实验来重现或预防地震活动。我们邀请来自理论、实验和数值领域的论文分享与本主题相关的发现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Induced Seismicity
One of the principal drags of the geothermal technologies is the slip reactivation in seismic faults or fractures. Stimulation processes used to improve permeability can induce seismic or aseismic slips which can lead to micro-seismic activity. Studying and understanding the triggering mechanisms of slips in faults could make it possible to mitigate micro-seismicity. Both challenging and interesting, induced seismicity remains an important research field for all the geo-energy applications and constructions around the world. In this mini-symposium, we want to focus on the physics of induced seismicity trough the influent factors and triggering mechanisms of micro-macro earthquakes. Lots of methods, models and experiments have been developed to reproduce or prevent seismicity. We invite papers from theoretical, experimental and numerical fields to share findings related to this topic.
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