Titlebook: Shallow Subduction Zones: Seismicity, Mechanics and Seismic Potential; Part II Renata Dmowska,Göran Ekström Book 1994 Birkhäuser Verlag, Ba

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Coseismic Slip in the 1964 Prince William Sound Earthquake: A New Geodetic Inversion,al Alaska. In this study geodetic and geologic measurements of this surface deformation were inverted for the slip distribution on the 1964 rupture surface. Previous seismologic, geologic, and geodetic studies of this region were used to constrain the geometry of the fault surface. In the Kodiak Isl

间谍活动

Seismicity Trends and Potential for Large Earthquakes in the Alaska-Aleutian Region,sis of historic earthquake recurrence data and time-to-failure analysis applied to recent decades of instrumental data. Recent (May 1993) earthquake activity in the Shumagin Islands gap is consistent with previous projections of increases in seismic release, indicating that this segment, along with

Benign

Rupture Process of Large Earthquakes in the Northern Mexico Subduction Zone,ones, has ruptured in a sequence of five large earthquakes from 1973 to 1985: the Jan. 30, 1973 Colima event (.. 7.5) at the northern end of the segment near Rivera fracture zone; the Mar. 14, 1979 Petatlan event (.. 7.6) at the southern end of the segment on the Orozco fracture zone; the Oct. 25, 1

Microaneurysm

,Global Variability in Subduction Thrust Zone—Forearc Systems,ematic information about the deformation of forearcs and indirect evidence on the dynamics of the plate boundary. A global survey of slip vectors at major trenches of the world reveals a large variability in the kinematic response of forearcs to shear produced by oblique convergence. The variability

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debunk

The 1957 Great Aleutian Earthquake,a is smaller than the aftershock zone and is about 850 km long. This does not include the Unalaska Island area in the eastern end of the aftershock zone, making this area a possible seismic gap and a possible site of a future large or great earthquake. We also inverted the tsunami waveforms for the

FLEET

The Rupture Process and Tectonic Implications of the Great 1964 Prince William Sound Earthquake,are able to locate the spatial distribution of moment along the length of the fault. The first moment pulse most likely initiated near the epicenter at the northeastern down-dip edge of the aftershock area and then spread over the fault surface in a semi-circular fashion until the full width of the

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