Depth Extent and Geometry of Active Continental Normal Faulting

该项目是一项世界范围的研究破裂的特点， 大陆正断层大地震及其 余震 开发用于分析整个地震的程序 波形 检查破裂深度，断层变化 倾角作为深度的函数， 余震区的底部（如果有同震滑动 在这些表面上的事件），以及破裂的变化 模式作为区域的功能。 目前集中的领域是 爱琴海地区。

Project is a world wide study of the rupture characteristics of large continental normal faulting earthquakes and their aftershocks. Develops procedures for analyzing whole seismic waveforms. Examines the depth of rupturing, variation of fault dip as a function of depth, evidence of detachment surfaces at the base of the aftershock zones (and if there is coseismic slip on these surfaces during an event), and variations in the rupture modes as a function of region. Current area of concentration is the Aegean region.