由于海底山脉和重复的M大约有7次地震造成的薄弱的板块间合
Kimihiro Mochizuki1, Tomoaki Yamada, Masanao Shinohara
1Earthquake Research Institute, University of Tokyo, 1-1-1, Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan. kimi@eri.u-tokyo.ac.jp
概括
沉降海底山可能不会像预期的那样加强板合. 来自日本海沟的地震数据表明,在沉降的海面上存在弱合,影响地震破裂区域.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 传统上,人们认为海底山的降压会增加板间应力.
- 最近的地震和实验室数据表明,合板之间的合可能很弱.
- 了解海底沉降对于地震危险评估至关重要.
研究的目的:
- 为了研究海底浮标对板块间合和地震性的影响.
- 为了分析与海底沉降相关的日本海沟的地震数据.
- 评估海底山脉在地震破裂动态中的作用.
主要方法:
- 在日本沟进行了地震调查.
- 分析了地震性模式,包括重复的地震.
- 在特定的地震事件 (1982 M 7.0) 中检查了破裂传播.
主要成果:
- 观测到弱的交叉板合在一个沉降的海面上.
- 确定了一个大的破裂区域,在海底山前发生的滑动最小.
- 暗示,沉浮海面的宽度可能会影响破裂区域的范围.
结论:
- 沉降海底山不一定会增强板间合.
- 海底层的沉降可以导致复杂的破裂模式,并影响地震的行为.
- 沉降海底山的几何结构在定义地震断裂特征方面发挥着重要作用.
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