000 | 01668nam a22002537a 4500 | ||
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003 | ZW-GwMSU | ||
005 | 20230502113013.0 | ||
008 | 230502b |||||||| |||| 00| 0 eng d | ||
040 |
_aMSU _cMSU _erda |
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100 | _aNONOMURA, Atsuko | ||
245 | _aRegional extraction of flexural-toppled slopes in epicentral regions of subduction earthquakes along the Nankai Trough using DEMs | ||
264 |
_aVerlag _bSpringer _c2013 |
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336 |
_2rdacontent _atext _btxt |
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337 |
_2rdamedia _aunmediated _bn |
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338 |
_2rdacarrier _avolume _bnc |
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440 |
_aEnvironmental earth services _vVolume , number , |
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520 | _aIn the epicentral region of subduction earthquakes, large-scale landslides are triggered by strong shaking of slopes weakened by flexural toppling. The distribution of flexural-toppled slopes is the primary information for predicting and mitigating landslide damage beforehand. This study proposes and tests a simple algorithm for extracting flexural-toppled slopes on a regional basis from a 10-m resolution digital elevation model by windows of two sizes. Local relief is extracted with a large window (200 × 200 pixels), and microtopography is extracted with a small window (3 × 3 pixels). The algorithm was derived from the region of the Kanagi-kuzure landslide in Shikoku, and tested at Aka-kuzure landslide in Honshu in Japan. Both areas are underlain by strongly tilted sedimentary rocks in epicentral regions of subduction earthquakes along the Nankai Trough. | ||
650 | _aDEM | ||
650 | _aMicrotopography | ||
650 | _atoppling | ||
700 | _aHASEGAWA, Shuichi | ||
856 | _uhttps://doi.org/10.1007/s12665-012-1722-z | ||
942 |
_2lcc _cJA |
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999 |
_c161926 _d161926 |