
求翻译。用软件的话也整理下。谢谢!
Comparisonwith2003earthquake:LandslidestriggeredbytheJuly2009Fiordlandearthquakeweres...
Comparison with 2003 earthquake: Landslides triggered by the July 2009 Fiordland earthquake
were similar in type and size to those caused by other recent earthquakes in Fiordland, such
as the Mw 6.8 earthquake in 1993 (Van Dissen et al. 1994, Hancox et al. 2002), and the Mw
7.2 earthquake in August 2003 (Hancox et al. 2003, Reyners et al. 2003). However, the 2009
earthquake was unusual because the number of landslides was much less than those that
occurred during the 2003 earthquake. Landslides triggered by the 2009 earthquake affected
an area of ~5600 km2, compared to ~10,000 km2 affected by landslides in 2003 (Figure 5).
The 2009 landslides were also generally slightly smaller in size, and none had volumes
greater than ~100,000 m3 compared to at least 15 landslides of ~50,000–700,000 m3 in 2003
(Hancox et al. 2003). Many of the 2009 landslides were clearly reactivations (generally upslope
enlargements) of those that occurred in 2003 or earlier, as shown in Figure 4. 展开
were similar in type and size to those caused by other recent earthquakes in Fiordland, such
as the Mw 6.8 earthquake in 1993 (Van Dissen et al. 1994, Hancox et al. 2002), and the Mw
7.2 earthquake in August 2003 (Hancox et al. 2003, Reyners et al. 2003). However, the 2009
earthquake was unusual because the number of landslides was much less than those that
occurred during the 2003 earthquake. Landslides triggered by the 2009 earthquake affected
an area of ~5600 km2, compared to ~10,000 km2 affected by landslides in 2003 (Figure 5).
The 2009 landslides were also generally slightly smaller in size, and none had volumes
greater than ~100,000 m3 compared to at least 15 landslides of ~50,000–700,000 m3 in 2003
(Hancox et al. 2003). Many of the 2009 landslides were clearly reactivations (generally upslope
enlargements) of those that occurred in 2003 or earlier, as shown in Figure 4. 展开
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与2003年地震:比较堰塞湖在2009年7月Fiordland地震
相似类型和大小由于其它地震在Fiordland,是不是这样
当马克-韦伯6.8地震,在1993年(范Dissen孙俐。1994年,•汉考克斯等人。2002),亿瓦
2003年8月720地震(•汉考克斯等人。2003年,Reyners孙俐。2003)。然而,2009年
不寻常的,因为地震塌方的数量比少多了
发生在2003年地震。2009年堰塞湖在地震的影响
面积~ 5600人平方公里,约10,000平方公里的影响相比,在2003年由山体滑坡(图5)。
2009年的山体滑坡也一般的小一点的大小,也没有卷
比~ 10万立方米比至少15滑坡造成的~ 50,000-700,000 m3在2003年
(•汉考克斯等人。2003)。许多2009年的滑坡(一般地而记忆
这放大这发生在2003年或更早的,如图4。
相似类型和大小由于其它地震在Fiordland,是不是这样
当马克-韦伯6.8地震,在1993年(范Dissen孙俐。1994年,•汉考克斯等人。2002),亿瓦
2003年8月720地震(•汉考克斯等人。2003年,Reyners孙俐。2003)。然而,2009年
不寻常的,因为地震塌方的数量比少多了
发生在2003年地震。2009年堰塞湖在地震的影响
面积~ 5600人平方公里,约10,000平方公里的影响相比,在2003年由山体滑坡(图5)。
2009年的山体滑坡也一般的小一点的大小,也没有卷
比~ 10万立方米比至少15滑坡造成的~ 50,000-700,000 m3在2003年
(•汉考克斯等人。2003)。许多2009年的滑坡(一般地而记忆
这放大这发生在2003年或更早的,如图4。
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