In this paper, we study the mechani

In this paper, we study the mechanical process of
the Jiufengershan landslide, which is one of the major
slides triggered by Chi-Chi earthquake. This landslide
is located about 12 km to the north of the epicenter
(120.848E, 23.968N). The slide affected weathered,
jointed rock and soil materials, which slid along the
bedding plane, generating a rock-and-soil avalanche
during the earthquake. The volume of the sliding
debris is roughly 50
106 m3 and consists of ~50–
60 m of thick-bedded muddy sandstones with thin
shale beds, covered by weathered rock and soil.
These materials were transported downslope for
about 1 km. The avalanche created a debris deposit
with maximum thickness of 110 m, which dammed
two small rivers and created three small lakes located
upstream.

結果 (中文) 1:

在本文中，我们研究的力学过程Jiufengershan 滑坡，是一个主要由集集大地震触发的幻灯片。该滑坡是位于震中的北面约 12 公里（120.848E，23.968N）。受影响的幻灯片风化，接合的岩石和土壤的材料，沿滑床上用品平面，生成的岩石和土壤雪崩在地震。滑动的卷碎片大约是 50 106 m3 和包含 ~ 50 — —厚层状泥质砂岩与薄的 60 米页岩风化的岩石和土壤所涵盖。这些材料是为运输的下坡约 1 公里。创建碎屑沉积的雪崩最大厚度为 110 米，堰塞两个小河和创建三个小湖，位于上游。

結果 (中文) 3:

在本文中，我们研究
的集集地震的力学过程，它是一个主要的
幻灯片集集大地震触发。该滑坡的
位于约12公里的震中
北（120.848e，23.968n）。滑动的影响
风化，节理岩土材料的滑动，沿
层面，在地震产生的岩石和土壤的雪崩
。的滑动
碎片的体积大约是50
106 m3，由~ 50–
60 m厚层状泥质砂岩与页岩层薄
，被风化的岩石和土壤。
这些材料被运下坡
约1公里。雪崩创造了一个最大厚度为110米的碎片存款
，其中堰塞湖
两个小河流和湖泊的上游，创造了三个小
。