The Large Salcito Landslide Triggered by the 2002 Molise, Italy, Earthquake

被引：13

作者：

Bozzano, Francesca ^{[1
]}

Martino, Salvatore ^{[1
]}

Naso, Giuseppe ^{[2
]}

Prestininzi, Alberto ^{[1
]}

Romeo, Roberto Walter ^{[3
]}

Mugnozza, Gabriele Scarascia ^{[1
]}

机构：

[1] Univ Roma La Sapienza, Dip Sci Terra, I-00185 Rome, Italy

[2] Natl Seism Survey, Civil Protect Dept, I-00189 Rome, Italy

[3] Univ Urbino, Ist Geol Applicata, I-61029 Urbino, Italy

来源：

EARTHQUAKE SPECTRA | 2004年 / 20卷

关键词：

D O I：

10.1193/1.1768539

中图分类号：

TU [建筑科学];

学科分类号：

0813 ;

摘要：

The 2002 Molise, Italy, earthquake triggered a deep planar earthslide about 38 km away from the epicenter, mainly involving scaly clay shales and related weathered material. Based on site investigations and borehole data, the inferred depth of the sliding surface is between 30 and 50 meters below ground level, indicating an involved volume of about 40.10(6) m(3). The complex geological setting, the generated excess pore water pressure, and possible local seismic response are thought to have been the primary contributing factors. [DOI: 10.1193/1.1768539]

引用

页码：S95 / S105

页数：11

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