草岭山崩机制及后续地表作用估算(英文)  

Life cycle of Tsaoling landslide dam and its geomorphologic impacts

作　　者：张国桢[1] 陈柔妃 詹瑜璋 郭志禹[4] 

机构地区：[1]台北科技大学土木系,台北10608 [2]中央研究院地球科学研究所,台北11529 [3]中国文化大学地质系,台北11114 [4]中央研究院应用科学研究中心,台北11529

出　　处：《福建地质》2010年第A01期147-148,共2页Geology of Fujian

摘　　要：The Tsaoling rock-and-soil avalanche is the largest landslides triggered by the Chi-Chi earthquake(Taiwan,1999).In addition,because of the periodic reoccurrence of gigantic slides since 19 century,instruments installed and aerial photo scans regularly around the Tsaoling area.Besides of massive field observations,several periods of Digital Terrain Models(DTMs) generated by aerial photos sets have also been deployed to investigate and calculate the coseismic and post-seismic morphological changes.The Tsaoling rock-and-soil avalanche is the largest landslides triggered by the Chi-Chi earthquake （Taiwan, 1999） . In addition, because of the periodic reoccurrence of gigantic slides since 19 century, instruments installed and aerial photo scans regularly around the Tsaoling area. Besides of massive field observations, several periods of Digital Terrain Models （DTMs） generated by aerial photos sets have also been deployed to investigate and calculate the coseismic and post-seismic morphological changes.

关 键 词：草岭山崩) 河阶 侵蚀速率 

分 类 号：P642.21[天文地球—工程地质学]