第四纪松散沉积物中隐性活断层的显微构造特征  

CHARACTERISTICS OF MICROSTRUCTURES OF THE INVISIBLE FAULTS IN QUATERNARY UNCONSOLIDATED SEDIMENTS

作　　者：晁洪太[1] 邓起东[2] 李家灵[1] 王志才[1] 满洪敏[1] 

机构地区：[1]山东省地震局,济南250014 [2]中国地震局地质研究所,北京100029

出　　处：《地震地质》2000年第2期147-154,共8页Seismology and Geology

基　　金：地震科学联合基金课题! ( 950 0 0 59);山东省自然科学基金课题! ( 95E2 0 38)资助

摘　　要：第四纪松散沉积物中普遍存在断层的隐性现象 ,包括断层的隐形和尖灭 ,给古地震研究带来了复杂性和多解性。选择了一些典型古地震剖面 ,对涉及到断层隐形或尖灭的部位 ,进行了定向原状样品采集 ,通过室内样品固结 ,显微薄片制作和显微构造现象观察 ,从显微域里找到了鉴定隐形断层的许多标志 ,并对断层尖灭机制进行了研究。认为通过显微构造分析 ,排除或肯定隐形断层的存在 ,或者追踪断层尖灭的层位 ,结合宏观剖面研究和年代测定 。Invisible faults often developed in Quaternary unconsolidated sediments including concealed faults and die out faults, which lead to complexity and multi solution for paleoearthquake research. In this paper, original state directional samples related to invisible or die out faults are collected from some typical paleoearthquake profiles and solidified in laboratory. Microstructures have been observed after grinding slides in three dimension coordinate system. Some indicators of invisible faults have been found in micrscopic field. The mechanisms of die out faults have also been studied. It is suggested that according to microstructural observation, to confirm or negate the existence of concealed faults or to trace the terminated levels of die out faults, can help us determine the age and periods of paleoearthquake events more accurately combining with macroscopic observation and age dating.

关 键 词：隐形断层 显微构造 第四纪 松散沉积物 古地震 

分 类 号：P315.2[天文地球—地震学] P542.3[天文地球—固体地球物理学]