| 1 |
13:40 ~ 13:50 |
長官致詞及介紹來賓
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| 2 |
13:50 ~ 14:10 |
古應力分析方法、可能性和限制及結果示例
Paleostress analysis methods, their possibilities and limits, and examples of their results
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馬薩里克大學 Melichar Rostislav
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| 3 |
14:10 ~ 14:40 |
從逆衝斷層到平移斷層：
西喀爾巴阡山脈側緣增積岩體的新階段
From oblique thrust to strike-slip: Latest stage of the Western-Carpathian accretionary wedge lateral margin
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馬薩里克大學 Šuťjak Martin
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| 4 |
14:40 ~ 15:00 |
從3D活動斷層微動力運動學中學習了什麼？
在歐洲東阿爾卑斯山區的經驗
What can we learn from active fault 3D microkinematic behaviour? Experience gained in the Eastern Alps in Europe
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捷克科學院 Baroň Ivo
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| 5 |
15:00 ~ 15:20 |
休息時間
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| 6 |
15:20 ~ 15:40 |
捷克復理層地區降雨觸發型深層崩塌—辨別與危害評估
Deep-seated rainfall-triggered landslides in the Czech flysch regions – identification and hazard assessment
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捷克科學院 Klimeš Jan
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| 7 |
15:40 ~ 16:00 |
磁化率不均向性應用於活斷層和崩塌岩體
Application of magnetic susceptibility anisotropy to active faults and landslide masses
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馬薩里克大學 Bárta František
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| 8 |
16:00 ~ 16:20 |
應用數位影像相關方法
研究潛在大規模崩塌斷面幾何形狀
Applying digital image correlation method to study the activity and failure surface geometry of potential large-scale landslide
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國立成功大學 郭賢立
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| 9 |
16:20 ~ 16:40 |
以密集式微地動訊號快速評估大規模崩塌地之滑動特徵
Rapid assessment of sliding characteristics of large-scale landslide using dense microtremor records
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國立成功大學 吳澄峰
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