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| 草岭山崩机制及后续地表作用估算(英文) | |
| 引用本文： | 张国桢,陈柔妃,詹瑜璋,郭志禹.草岭山崩机制及后续地表作用估算(英文)[J].福建地质,2010,29(Z1). |
| 作者姓名： | 张国桢 陈柔妃 詹瑜璋 郭志禹 |
| 作者单位： | 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;中国文化大学地质系,台北,11114 3. 中央研究院地球科学研究所,台北,11529 4. 中央研究院应用科学研究中心,台北,11529 |
| 摘 要： | <正>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 |
Life cycle of Tsaoling landslide dam and its geomorphologic impacts |
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| Abstract: | |
| Keywords: | Tsaoling landslide river terrace erosin rate |
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