地球および惑星深部における分別結晶化と部分融解

在我担任研究员的第二年，我继续了解核心和核心边界区域的结构。地球核心是地球核心的固体部分，由于地球中心温度的下降，随着液体部分的冻结，核心正在增长。固体内核内部的流动还没有完全被理解。对内核的地震观测发现了几个尺度上的复杂结构。在我攻读博士期间，我开发了内核变形的地球动力学模型。在这一年里，我开发了一个软件来比较地震观测和地球动力学模型。这段代码在地球动力学模型中传播地震射线，并允许进行简单的比较。

During the second year of my fellowship, I have continued the work to understand the structure of the inner core and the inner core boundary region. The Earth’s inner core is the solid part of the Earth’s core, and is growing as the liquid part is freezing, because of the decrease of temperature in the center of the Earth. The flow inside the solid inner core is not yet fully understood. Seismic observations of the inner core have detected complex structures on several scales. During my Ph.D., I developed geodynamical models for deformation in the inner core. During this year, I developed a software to compare seismic observations and geodynamical models. This code propagates seismic rays in the geodynamical models, and allow easy comparisons.