大震区的风学分离和偶发震动和滑动
Xiang Gao1,2, Kelin Wang3,4
1Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, 7 Nanhai Road, Qingdao 266071, China.
Nature
|March 7, 2017
概括
潜伏区的偶发震和缓慢滑动 (ETS) 是由一个新的模型解释的. 高温和孔流体压力形成了不同的地震和ETS区域,协调了断层行为的观察.
科学领域:
- 地质学
- 构造学
- 地震学
背景情况:
- 突发性震和缓慢滑动 (ETS) 发生在具有年轻,温暖板块的沉降区域.
- 排放交易体系的机制及其与地震带的关系尚不清楚.
- 现有的模型与地震带和ETS区域之间的空间分离相矛盾.
研究的目的:
- 为ETS的地质条件提出一个统一的模型.
- 解释地震和ETS区域之间的空间关系.
- 调查断层区域在ETS中的作用.
主要方法:
- 数字热模型.
- 检查热石矿学控制的断层区域形学 (摩擦与粘性剪切).
主要成果:
- 在温暖的沉积板中,高温结束了地幔角之前的地震带.
- 在地幔角附近的高孔流体压力会产生一个孤立的摩擦区域,负责ETS.
- 一段半摩擦或粘性行为将地震和ETS区域分开.
结论:
- 拟议的模型协调了ETS和故障行为的不同观察.
- 它为研究主要断层的滑动行为和地震生成提供了一个概念框架.
- 该模型强调了热和流体条件在潜伏区力学中的支配作用.
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