使用地震速率的变化作为Kilauea火山的压力计
J Dieterich1, V Cayol, P Okubo
1US Geological Survey, Menlo Park, California 94025, USA. jdieterich@usgs.gov
Nature
|December 2, 2000
概括
地震发生率现在可以推断出地的压力变化. 在基拉韦亚火山成功应用的新方法证明了地震率作为实际的遥感应力计.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 火山学 火山学是一门学科.
背景情况:
- 估计地球地的应力变化通常依赖于近地表变形模型.
- 地震活动往往与压力变化相关,这表明地震性数据可以用于压力估计.
- 以前的方法面临挑战,因为地震速率和压力/时间之间的非线性关系.
研究的目的:
- 开发和验证从地震发生率推断压力变化的方法.
- 为了克服地震性数据分析中的非线性限制.
- 评估使用地震速率作为遥感应力测量工具的可行性.
主要方法:
- 开发了两种新的反转方法来分析地震速率数据.
- 包含了地震速率的应力和时间依赖性的配方.
- 将这些方法应用于 Kilauea 火山的地震性数据.
主要成果:
- 成功逆转地震速率数据以推断应力变化.
- 在基拉韦亚火山的推断压力变化和独立估计之间取得了良好的一致性.
- 证明了地震速率对于遥控应力传感的实际实用性.
结论:
- 地震发生率可以可靠地用于推断地的应力变化.
- 开发的方法为传统的压力估计技术提供了可行的替代方案.
- 地震的地震性作为一个有效的遥感压力计,特别是在火山地区.
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