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- W2091214827 endingPage "400" @default.
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- W2091214827 abstract "A dense nationwide seismic network recently constructed in Japan has been yielding large volumes of high-quality data that have made it possible to investigate the seismic structure in the Japanese subduction zone with unprecedented resolution. In this article, recent studies on the subduction of the Philippine Sea and Pacific plates beneath the Japanese Islands and the mechanism of earthquake and magma generation associated with plate subduction are reviewed. Seismic tomographic studies have shown that the Philippine Sea plate subducting beneath southwest Japan is continuous throughout the entire region, from Kanto to Kyushu, without disruption or splitting even beneath the Izu Peninsula as suggested in the past. The contact of the Philippine Sea plate with the Pacific plate subducting below has been found to cause anomalously deep interplate and intraslab earthquake activity in Kanto. Detailed waveform inversion studies have revealed that the asperity model is applicable to interplate earthquakes. Analyses of dense seismic and GPS network data have confirmed the existence of episodic slow slip accompanied in many instances by low-frequency tremors/earthquakes on the plate interface, which are inferred to play an important role in stress loading at asperities. High-resolution studies of the spatial variation of intraslab seismicity and the seismic velocity structure of the slab crust strongly support the dehydration embrittlement hypothesis for the generation of intraslab earthquakes. Seismic tomography studies have shown that water released by dehydration of the slab and secondary convection in the mantle wedge, mechanically induced by slab subduction, are responsible for magma generation in the Japanese islands. Water of slab origin is also inferred to be responsible for large anelastic local deformation of the arc crust leading to inland crustal earthquakes that return the arc crust to a state of spatially uniform deformation." @default.
- W2091214827 created "2016-06-24" @default.
- W2091214827 creator A5013582768 @default.
- W2091214827 creator A5014249378 @default.
- W2091214827 creator A5023969183 @default.
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- W2091214827 creator A5036340333 @default.
- W2091214827 creator A5068501646 @default.
- W2091214827 creator A5088697244 @default.
- W2091214827 date "2009-12-01" @default.
- W2091214827 modified "2023-10-14" @default.
- W2091214827 title "Plate subduction, and generation of earthquakes and magmas in Japan as inferred from seismic observations: An overview" @default.
- W2091214827 cites W1544657794 @default.
- W2091214827 cites W1711146068 @default.
- W2091214827 cites W1821748331 @default.
- W2091214827 cites W1906688052 @default.
- W2091214827 cites W1913469372 @default.
- W2091214827 cites W1928348702 @default.
- W2091214827 cites W1963550432 @default.
- W2091214827 cites W1963593144 @default.
- W2091214827 cites W1963862763 @default.
- W2091214827 cites W1966613431 @default.
- W2091214827 cites W1967598671 @default.
- W2091214827 cites W1970273263 @default.
- W2091214827 cites W1970831581 @default.
- W2091214827 cites W1971686935 @default.
- W2091214827 cites W1973406015 @default.
- W2091214827 cites W1973542860 @default.
- W2091214827 cites W1974941284 @default.
- W2091214827 cites W1976229064 @default.
- W2091214827 cites W1976420647 @default.
- W2091214827 cites W1977921224 @default.
- W2091214827 cites W1978015797 @default.
- W2091214827 cites W1978290547 @default.
- W2091214827 cites W1978474781 @default.
- W2091214827 cites W1978534444 @default.
- W2091214827 cites W1978849688 @default.
- W2091214827 cites W1979581725 @default.
- W2091214827 cites W1980796709 @default.
- W2091214827 cites W1981648444 @default.
- W2091214827 cites W1982388448 @default.
- W2091214827 cites W1982720436 @default.
- W2091214827 cites W1983091118 @default.
- W2091214827 cites W1983419273 @default.
- W2091214827 cites W1984657613 @default.
- W2091214827 cites W1984670316 @default.
- W2091214827 cites W1984754860 @default.
- W2091214827 cites W1984763616 @default.
- W2091214827 cites W1985141954 @default.
- W2091214827 cites W1985298050 @default.
- W2091214827 cites W1985707168 @default.
- W2091214827 cites W1986022350 @default.
- W2091214827 cites W1986128094 @default.
- W2091214827 cites W1986637158 @default.
- W2091214827 cites W1986901548 @default.
- W2091214827 cites W1988814630 @default.
- W2091214827 cites W1989378417 @default.
- W2091214827 cites W1991251070 @default.
- W2091214827 cites W1992649887 @default.
- W2091214827 cites W1995378196 @default.
- W2091214827 cites W1995988653 @default.
- W2091214827 cites W1996237313 @default.
- W2091214827 cites W1996412456 @default.
- W2091214827 cites W1996918273 @default.
- W2091214827 cites W1997723797 @default.
- W2091214827 cites W1997932671 @default.
- W2091214827 cites W1998593363 @default.
- W2091214827 cites W2001899775 @default.
- W2091214827 cites W2002074664 @default.
- W2091214827 cites W2002191842 @default.
- W2091214827 cites W2003600307 @default.
- W2091214827 cites W2003725152 @default.
- W2091214827 cites W2005240602 @default.
- W2091214827 cites W2007850363 @default.
- W2091214827 cites W2008126095 @default.
- W2091214827 cites W2009149384 @default.
- W2091214827 cites W2009367373 @default.
- W2091214827 cites W2009454183 @default.
- W2091214827 cites W2010668132 @default.
- W2091214827 cites W2010813958 @default.
- W2091214827 cites W2011161735 @default.
- W2091214827 cites W2011928058 @default.
- W2091214827 cites W2012201259 @default.
- W2091214827 cites W2012806275 @default.
- W2091214827 cites W2017101384 @default.
- W2091214827 cites W2017649324 @default.
- W2091214827 cites W2017662684 @default.
- W2091214827 cites W2018363314 @default.
- W2091214827 cites W2018854158 @default.
- W2091214827 cites W2020952883 @default.
- W2091214827 cites W2021243560 @default.
- W2091214827 cites W2022774905 @default.
- W2091214827 cites W2025437017 @default.
- W2091214827 cites W2027277914 @default.
- W2091214827 cites W2028121951 @default.
- W2091214827 cites W2028404221 @default.
- W2091214827 cites W2028839654 @default.
- W2091214827 cites W2028983145 @default.