双贝尼奥夫区的全球流行情况
Michael R Brudzinski1, Clifford H Thurber, Bradley R Hacker
1Geology Department, Miami University, Oxford, OH 45056, USA. brudzimr@muohio.edu
概括
双贝尼奥夫带,表示两个层的深度地震,是固有的压力板. 它们的分离随着板的年龄增加而增加,这表明抗原石的脱水是可能的原因.
科学领域:
- 地震学 地震学
- 构造学 构造学 构造学 构造学
- 地质物理学 地质物理学
背景情况:
- 双贝尼奥夫带,以两层不同的深度地震为特征,为理解地震发生提供了一个难题.
- 解释这些双重地震层背后的机制和它们的分离对于提高我们对俯冲区动态的了解至关重要.
研究的目的:
- 使用地震性数据来描述潜流板内部的层分离.
- 调查双贝尼奥夫区的全球发生和控制因素.
主要方法:
- 利用坐标旋转来分析地震的平板正常分布.
- 采用全球地震性目录来量化层分离.
- 在已知的例子上进行基准测试,以验证方法.
主要成果:
- 仅使用全球地震性目录精确量化层分离.
- 在全球30个俯冲区段中确定了双贝尼奥夫区.
- 观察到,层分离随着降温板的年龄增加而增加.
结论:
- 双贝尼奥夫带是一个常见的特征,固有于各种年龄和应力条件下的引板.
- 随着年龄的增长观察到的层分离的增加支持抗戈的脱水作为一种比化物脱水更合理的机制.
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