摘要
利用C14测年方法对陕西翠华山不同时期的山崩进行了绝对年龄的初步研究。C14测年数据与宏观野外地质地貌调查的结论吻合,证实了翠华山山崩景观形成为多期性的结论,同时与地震事件有一定的关系,为研究山崩成因提供了科学论据。
In this paper, the absolute age for collapses of Shaanxi Cuihua Mountain in different periods of time were studied preliminarily using the C^14 dating method. The coincidence of C^14 dating data with the results of the macrofield geological features investigation confirmed the conclusions that collapses landscape of Cuihua Mountain was formed with the multi-phase nature and has certain relationship with the seismic events, providing a scientific argument for the study of the form causes of the collapses.
出处
《山地学报》
CSCD
北大核心
2009年第3期349-352,共4页
Mountain Research
关键词
翠华山
山崩遗迹
C14测年
Cuihua Mountain
collapses remains
C^14 measurement of age
