Titlebook: Seismogenic and Tsunamigenic Processes in Shallow Subduction Zones; Jeanne Sauber,Renata Dmowska Book 1999 Springer Basel AG 1999 Geophysi

Harass

闪光东本

Local Tsunamis and Distributed Slip at the Source,tion zone earthquakes. Assumptions inherent in calculating the coseismic vertical displacement field that defines the initial condition for tsunami propagation are examined. By comparing the seafloor displacement from uniform slip to that from an ideal static crack, we demonstrate that dip-directed

GULF

Geologie Setting, Field Survey and Modeling of the Chimbote, Northern Peru, Tsunami of 21 February quiet. On 21 February 1996 at 21:51 GMT (07:51 local time) a large, tsunamigenic earthquake (Harvard estimate .. =7.5) struck at 9.6°S, 79.6°W, approximately 130 km off the northern coast of Peru, north of the intersection of the Mendana fracture zone with the Peru-Chile trench. The likely mechanism

Stress-Fracture

abnegate

TAIN

Relation between the Subducting Plate and Seismicity Associated with the Great 1964 Alaska Earthquasmological observations in the Prince William and Kodiak areas that ruptured during this earthquake with the corresponding morphology and structure of the subducting plate. The upper plate geology (Prince William Terrane) and velocity structure are the same in both areas. In the Prince William area

注意到

inflame

阻碍

Rupture Process of the 1995 Antofagasta Subduction Earthquake (,, = 8.1),ves that span periods from 20 to 290 s. A long-period (150–290 s) surface-wave spectral inversion technique is applied to estimate the average finite-fault source properties. Deconvolutions of broadband body waves using theoretical Green’s functions, and deconvolutions of broadband fundamental mode

集合

GPS-derived Deformation of the Central Andes Including the 1995 Antofagasta ,, = 8.0 Earthquake,ng Chile and the western part of Argentina was selected, monumented and observed in 1993 and 1994. A dense part of the network in northern Chile and northwest Argentina, comprising some 70 sites, was re-observed after two years in October/November, 1995. The .. = 8.0 Antofagasta (North Chile) earthq