Both kinds of plate boundary are associated with fault systems, earthquakes and volcanism, but the kinds of geologic activity observed at the two boundaries are quite different.
两种板块边界均与地层系统、地震以及火山活动有关,但在两种边界处观察到的诸般地质活动却迥然不同。
Fault dislocation due to large earthquake is known very well by people, and geologic disasters induced by fault creep get more attentions gradually.
大地震引发的断层错动已为人们所熟知,而断层蠕滑造成的地质灾害也逐渐受到更多的关注。
And some relevant geologic data regression equations for fault scarp formed in the past 2700 years have been obtained.
获得了相应地区断层陡坎的一些资料和距今2700年左右形成的断层陡坎回归方程。
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