岩层或岩体破裂错开,沿两盘发生相对移动的面,称断层面。断层面有的较规则平整,有的破碎曲折。
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断层面解随时间没有明显的变化。
虽然如此,如果智利的断层面接近崩溃,那些微波可能会促使它更快崩溃。
Nevertheless, if the Chilean fault surface were close to failure, those small waves could push it even closer.
若一断层的断层面是直立的,我们怎么去确定它的上盘和下盘呢?
If a fault has a vertical fault plane. How do we determine its hanging wall and footwall?
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