从断裂带构造认识断层滑移习性
Learning to read fault-slip behavior from fault-zone structure
摘要
对于地震物理学和断裂运动研究而言,探索断裂带构造和地震行为之间的联系是至关重要的。地震代表滑动行为的一个极端;摩擦熔融和假玄武玻璃为动力破裂过程中的局部滑动提供了野外证据[1-3]。无震滑动则代表滑动行为的另一极端,在无震滑动中,蠕变与断裂带内普遍存在的剪切作用有关。
出处
《国际地震动态》
2011年第10期15-18,共4页
Recent Developments in World Seismology
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