摘要
本文通过对大青山山前活动断裂带上的变形产物进行定向采集、原态固结并进行系统微观观测，结合宏观和实验岩石学资料分析，归纳出能反映该断裂运动特性的微观粘滑与蠕滑标志，并对有关问题进行了讨论。
Based on directive Sampling and undisturbed induration on the deformation products on the Dagingshan Piedmont active fault, to take systematic and microscopic observation in combination with results of rock-breaking test and macroscopic analysis, marks of stick slip and creep slippage were obtained and this reflected the kinetic characteristics of the fault. In this paper, Some other related studies were also discussed.
出处
《中国地震》
CSCD
北大核心
1995年第3期231-238,共8页
Earthquake Research in China
基金
地震科学联合基金
关键词
岩组分析
古地震
粘滑标志
蠕滑标志
活动断裂
Petrofabrics analysis, Microstructure, Palaeoearthquake, Nei Monggal, Stick slipmark, Creep slip mark
