东田纳西州300公里长的地震区域的地震构造模型
概括
在田纳西州东部进行了十年的地震监测,发现了微型地震活动的线性区域. 这个区域显示了显著的地震应变能量释放,集中在地块边界附近.
科学领域:
- 地球科学 地球科学 地球科学
- 地震学 地震学
- 地质物理学 地质物理学
背景情况:
- 一个区域地震网络已经监测了田纳西州东部的微型地震十年.
- 了解地震活动模式对于评估区域构造压力和地动态至关重要.
研究的目的:
- 确定和描述田纳西州东部地震活动区域.
- 分析该地区内的地震应变能量释放情况.
- 研究地震性和底层地结构之间的关系.
主要方法:
- 来自区域地震网络的十年微型地震数据的分析.
- 计算地震应变能量释放,按地面积正常化.
- 地震活动与地下地块的地质数据的相关性.
主要成果:
- 在田纳西州东部确定了一个明确的线性地震活动区域.
- 在过去的十年中,该区域在落基山脉以东释放的地震应变能量是第二高的 (按区域正常化).
- 地震性集中在强弱地下地块之间的边界附近.
结论:
- 已确定的地震区域代表着一个重要的板块内构造应力区域.
- 地震性的度表明地块边界充当管道或应力度器.
- 这些发现有助于理解在稳定的大陆内部驱动地震性的机制.
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