On far field occurrence of seismically induced landslides

Engineering Geology

Volumn 123, Issue 3, 2011, Pages 204-213

  Delgado, J ^a   Garrido, J ^b   Lopez Casado C ^b   Martino, S ^c   Pelaez J A ^d  

^a UNIVERSITY OF ALICANTE   (Spain)

^b UNIVERSITY OF GRANADA   (Spain)

^c SAPIENZA UNIVERSITY OF ROME   (Italy)

^d UNIVERSITY OF JAÉN   (Spain)

Author keywords

Earthquake; Landslide; Macroseismic intensity; Magnitude; Maximum distance

Indexed keywords

COHESIVE SOILS; EARTHQUAKE EPICENTER; EPICENTRAL AREA; EPICENTRAL DISTANCES; EXPECTED DISTANCE; FAR FIELD; JOINTED ROCK; LONG DISTANCES; MACROSEISMIC INTENSITY; MAGNITUDE; MAXIMUM DISTANCE; RESIDUAL SOIL SLOPE; SEISMICALLY INDUCED LANDSLIDE; SITE EFFECTS; UPPER BOUND; VOLCANIC SOILS;

ANOXIC SEDIMENTS; EARTHQUAKES; SOILS;

LANDSLIDES;

COHESIVE SOIL; COLLUVIAL DEPOSIT; DATABASE; EARTHQUAKE EPICENTER; EARTHQUAKE INTENSITY; EARTHQUAKE MAGNITUDE; LANDSLIDE; RESIDUAL SOIL; VOLCANIC SOIL;

EID: 80054681721     PISSN: 00137952     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.enggeo.2011.08.002     Document Type: Article

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