地震与地热能

S. Kapoor, B. Chauhan
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引用次数: 1

摘要

地震的起源长期以来被认为是由于沿断层线的板块构造的走滑不稳定造成的。全球发生的几次地震都不能用这个理论来解释。在这项工作中,我们调查了地震数据以及其他观察到的事实,如热流剖面等。位于印度次大陆。在我们的研究中,我们发现了地震事件、地震易发区、热流区和地热温泉之间的高质量相关性。因此,我们提出了一个可以充分解释全球所有地震事件以及整体地球动力学的假设。基本上是地热能,使板块静止、撞击和滑动。板块只是一个工作固体,而驱动力是地热能。这种能量的剧烈流动和巨大压力会沿着板块边界震动地球,也会引发板块内地震活动。根据加州能源委员会对正在进行的加州大间歇泉地热发电项目的报告结果,我们进一步提出,通过利用剩余的地热能源,可以大大降低即将发生地震的强度和风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Earthquake and Geothermal Energy
The origin of earthquake has long been recognized as resulting from strike-slip instability of plate tectonics along the fault lines. Several events of earthquake around the globe have happened which cannot be explained by this theory. In this work we investigated the earthquake data along with other observed facts like heat flow profiles etc... of the Indian subcontinent. In our studies we found a high-quality correlation between the earthquake events, seismic prone zones, heat flow regions and the geothermal hot springs. As a consequence, we proposed a hypothesis which can adequately explain all the earthquake events around the globe as well as the overall geo-dynamics. It is basically the geothermal power, which makes the plates to stand still, strike and slip over. The plates are merely a working solid while the driving force is the geothermal energy. The violent flow and enormous pressure of this power shake the earth along the plate boundaries and also triggers the intra-plate seismicity. In the light of the results reported by the California Energy Commission from the ongoing geothermal power project at the Big Geysers in California, we further propounded that by harnessing the surplus geothermal energy the intensity and risk of the impending earthquakes can be substantially reduced.
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