草岭山崩机制及后续地表作用估算(英文)

• 作 者: 张国桢 陈柔妃 詹瑜璋 郭志禹
• 机 构: 台北科技大学土木系,中央研究院地球科学研究所,中国文化大学地质系,中央研究院应用科学研究中心,
• 出 处: 福建地质
• 发表日期: 2010年S1期
• 关键词: 侵蚀速率 河阶 草岭山崩 triggered regularly rock slides instruments aerial installed

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). 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.