Geodynamics and earthquakes of subduction zones

这项拟议的研究旨在了解俯冲带的力学过程。这一发现将对理解板块俯冲的地球动力学，特别是其地震过程具有重要的意义。这项提案寻求有限的资金，以在未来五年内的任何一年为两名研究生提供部分支持，以进行三个学科的计算机建模。第一个主题是大俯冲地震的形变周期，例如1700年加拿大西海岸发生的9级地震。基于不同俯冲带的大地测量和地震学观测，我们将开发模型来研究地壳和地幔在地震期间和地震后如何变形，以及应变能如何重新积累以导致下一次地震。第二个主题是幕式地震和滑动(ETS)，这是最近在一些俯冲断裂的孕震带下倾发现的现象，例如在西海岸的卡斯卡迪亚俯冲带。这将有助于我们理解俯冲断层的复杂行为，即为什么和如何不仅在地震中滑动，而且在两次地震之间的非地震滑动瞬变中滑动。第三个主题是对大俯冲地震的几何和构造控制。地震破裂是不稳定摩擦的表现，但俯冲断层不是离散的摩擦接触，而是三维结构复杂的地带。我们将致力于一个新的概念框架，它将使我们能够解决许多尚未回答的一阶问题，例如为什么卡斯卡迪亚俯冲带倾向于产生罕见的但巨大的(M~9)地震，而许多其他俯冲带倾向于产生更频繁但较小的事件。

The proposed research is designed to understand mechanical processes of subduction zones. The findings will have important implications for understanding the geodynamics of plate subduction, especially its earthquake processes. This proposal seeks limited funding to provide partial support for two graduate students at any given year over the next five years to conduct computer modeling on three subjects. The first subject is the deformation cycles of great subduction earthquakes such as the M 9 earthquake in 1700 off Canada's west coast. Based on geodetic and seismological observations from different subduction zones, we will develop models to address how the Earth's crust and mantle deform during and after an earthquake and how strain energy is re-accumulated leading to the next event. The second subject is the Episodic Tremor and Slip (ETS), a phenomenon newly found downdip of the seismogenic zone of some subduction faults, such as at the Cascadia subduction zone off the west coast. This will help us understand the complex behavior of subduction faults, that is, why and how they slip not only in earthquakes but also in aseismic slip transients during the time between earthquakes. The third subject is geometrical and structural controls on great subduction earthquakes. Earthquake rupture is a manifestation of unstable friction, but subduction faults are not discrete frictional contacts but zones of three-dimensional structural complexity. We will work on a new conceptual framework that will allow us to address many unanswered first-order questions such as why the Cascadia subduction zone tends to produce infrequent but giant (M ~ 9) earthquakes while many other subduction zones tend to produce more frequent but smaller events.