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

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Seismicity Trends and Potential for Large Earthquakes in the Alaska-Aleutian Region,e “D” zones). The largest Alaska-Aleutian earthquakes—in 1957, 1964, and 1965—originated in zones that exhibit type D behavior. Type A zones currently showing accelerating release are the Shumagin, Alaska Peninsula, Delarof, and Kommandorski segments. Time-to-failure analysis suggests that the large

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,Global Variability in Subduction Thrust Zone—Forearc Systems,han oceanic or young arcs. The inferred absence of forearc deformation at continental arcs from this study is counter to inferences drawn from compiled geologic information on forearc faults. Correlations of the apparent forearc rheology with backarc spreading, convergence rate, slab dip, arc curvat

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Large Thrust Earthquakes and Volcanic Eruptions,litude of the strain field beneath the volcano is uniform up to a depth of 20 km and decreases downward. The sudden extension of the region is thought to be the main factor in facilitating the eruption of the volcano. It is postulated that strain beneath the volcano triggered the eruption of the Puy

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Shallow Subduction Zones: Seismicity, Mechanics and Seismic PotentialPart II

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Pageoph Topical Volumeshttp://image.papertrans.cn/s/image/866324.jpg

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https://doi.org/10.1007/978-3-0348-7333-8Geophysik; Seismologie; earthquake; geophysics; seismic; seismology; volcanic eruption

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Introduction,This is a companion volume to PAGEOPH’s vol. 140, N. 2, 1993, and, as its predecessor, it reports recent research on seismicity, mechanics and seismic potential in shallow subduction zones around the world.