陕西五曲湾滑坡发育特征和~(14)C测龄
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
在陕西省凤翔县五曲湾滑坡的滑带土中发现一段树根,表面被炭化,并且发生了强烈的剪切变形,分析认为此乃滑坡滑动所致。经过14C测龄,年龄为462±45年B.P,这一年龄与地质分析获取的认识基本吻合,与1556年"华县大地震"发生的年份非常接近,从而为研究五曲湾滑坡的触发机制提供了重要依据。最后提出,如果在滑带土中发现可用于定年的样品,采用14C法测定滑坡年龄,是对滑坡进行定年的有效途径。
A piece of tree root was found in the slip soil of a landslide in Wuquwan,Fengxiang County, Shaanxi Province. Surface of the root was carbonized and intensely sheared,which was analyzed to be resulted from a landslide sliding. 14C dating suggests that the landslide age is 462 ± 45 years. This datum accords with the geology analysis result and is close to the year of 1556 when the Huaxian earthquake took place. This information contributes to the study on triggering mechanism of the Wuquwan landslide. Consequently,if we can find a sample from the sliding soil that can be used for dating,the method of 14C dating should be an effective approach for dating the age of a landslide.
引文
[1]Marten Geertsema,John J Clagu.1000-year record of landslide dams at Halden Creek,northeastern British Columbia[J].Landslides,2006,3(3):217-227.
    [2]Giovanni Bertolini,Nicola Casagli,Leonardo Ermini.Radiocar-bon data on lateglacial and holocene landslides in the northern ap-ennines[J].Natural Hazards,2004,31(3):645-662.
    [3]Tamer Y.Duman.The largest landslide dam in Turkey:Tortum landslide[J].Engineering Geology,2009,104(1/2):66-79.
    [4]邓清禄,柯于义,郭锋.长江三峡非正常含炭粘土沉积及其地质灾害意义[J].地球科学,2008,33(3):405-410.
    [5]王兰生,杨立铮,王小群,等.岷江叠溪古堰塞湖的发现[J].成都理工大学学报:自然科学版,2005,32(1):1-10.
    [6]国家地震局震害防御司.中国历史强震目录(公元前23世纪-公元1911年)[M].北京:地震出版社,1995.
    [7]张振中.黄土地震灾害[M].北京:地震出版社,1999.
    [8]陈永明,石玉成,刘红玫,等.黄土地区地震滑坡的分布特征及其影响因素分析[J].中国地震,2005,21(2):235-243.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心