FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385422297> ?p ?o ?g. }

• W4385422297 abstract "Abstract This paper summarizes the results of 10 years of research on models of the megathrust earthquake cycles and crustal deformation associated with the 2011 Tohoku-oki earthquake. Several earthquake cycle models have been proposed for the northeast Japan subduction zone to elucidate why megathrust earthquakes occur at intervals of approximately 600 years and why large slips occurred in the shallow subduction zone. A model that considers a strong asperity in the shallow plate interface, and a hierarchical asperity model that considers the scale dependence of the critical displacement of the rate- and state-dependent friction law have been proposed. Modeling with dynamic weakening of faults has also been proposed. In the model using the shallow friction characteristics obtained by the Japan Trench Fast Drilling Project, rupture from depth can propagate to the trench, resulting in shallow large slips. Submarine crustal deformation has been observed for the first time in addition to dense observations of the inland crustal deformation. The observation of the seafloor deformation near the trench showed that viscoelastic relaxation played an important role in short-term postseismic deformation near the trench. The effects of the low-viscosity region at the oceanic lithosphere and asthenosphere boundary, and the cold forearc mantle wedge (cold nose) have been discussed. Simulations using the nonlinear flow law of rock in the mantle, where a power–law relationship holds between stress and strain rate, and the fault friction law at the plate boundary, show that the Tohoku-oki earthquake caused large stress fluctuations, resulting in a sudden viscosity decrease and rapid flow in the asthenosphere below the oceanic lithosphere. The simulations of the crustal deformation associated with the Tohoku-oki earthquake cycle also indicate that in the later stage of the earthquake cycle, the Pacific coastal region begins to subside due to the increasing slip deficit rate on the deeper parts of the plate interface. These results explain the subsidence of the Pacific coast of northeast Japan observed for about 100 years prior to the Tohoku-oki earthquake. In the future, a model that explains the long-term crust and mantle deformation during the entire Tohoku-oki earthquake cycle must be constructed." @default.
• W4385422297 created "2023-08-01" @default.
• W4385422297 creator A5026063332 @default.
• W4385422297 date "2023-07-31" @default.
• W4385422297 modified "2023-10-16" @default.
• W4385422297 title "Progress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processes" @default.
• W4385422297 cites W1481622287 @default.
• W4385422297 cites W1498453939 @default.
• W4385422297 cites W1507384737 @default.
• W4385422297 cites W1521779082 @default.
• W4385422297 cites W1530195759 @default.
• W4385422297 cites W1532952932 @default.
• W4385422297 cites W1562817020 @default.
• W4385422297 cites W1585803840 @default.
• W4385422297 cites W1768335013 @default.
• W4385422297 cites W1807213132 @default.
• W4385422297 cites W1837144984 @default.
• W4385422297 cites W1864465221 @default.
• W4385422297 cites W1876878401 @default.
• W4385422297 cites W1905940307 @default.
• W4385422297 cites W1938062868 @default.
• W4385422297 cites W1938111796 @default.
• W4385422297 cites W1967072856 @default.
• W4385422297 cites W1976815700 @default.
• W4385422297 cites W1981523453 @default.
• W4385422297 cites W1982669256 @default.
• W4385422297 cites W1983505775 @default.
• W4385422297 cites W1992363677 @default.
• W4385422297 cites W1993648481 @default.
• W4385422297 cites W1995307791 @default.
• W4385422297 cites W1998819856 @default.
• W4385422297 cites W2003017747 @default.
• W4385422297 cites W2005489768 @default.
• W4385422297 cites W2007782885 @default.
• W4385422297 cites W2015906752 @default.
• W4385422297 cites W2015931951 @default.
• W4385422297 cites W2017274089 @default.
• W4385422297 cites W2017611649 @default.
• W4385422297 cites W2019087482 @default.
• W4385422297 cites W2022774905 @default.
• W4385422297 cites W2029441462 @default.
• W4385422297 cites W2031532693 @default.
• W4385422297 cites W2033998922 @default.
• W4385422297 cites W2035612331 @default.
• W4385422297 cites W2039285506 @default.
• W4385422297 cites W2041125878 @default.
• W4385422297 cites W2049546117 @default.
• W4385422297 cites W2049723847 @default.
• W4385422297 cites W2052242710 @default.
• W4385422297 cites W2052619697 @default.
• W4385422297 cites W2052967122 @default.
• W4385422297 cites W2055821052 @default.
• W4385422297 cites W2057288458 @default.
• W4385422297 cites W2061328577 @default.
• W4385422297 cites W2063503947 @default.
• W4385422297 cites W2069711545 @default.
• W4385422297 cites W2070566444 @default.
• W4385422297 cites W2070932919 @default.
• W4385422297 cites W2076670652 @default.
• W4385422297 cites W2079749210 @default.
• W4385422297 cites W2083949913 @default.
• W4385422297 cites W2084227550 @default.
• W4385422297 cites W2088025384 @default.
• W4385422297 cites W2092208635 @default.
• W4385422297 cites W2093498753 @default.
• W4385422297 cites W2094392092 @default.
• W4385422297 cites W2095587387 @default.
• W4385422297 cites W2108523563 @default.
• W4385422297 cites W2110574886 @default.
• W4385422297 cites W2113695464 @default.
• W4385422297 cites W2115116587 @default.
• W4385422297 cites W2119963804 @default.
• W4385422297 cites W2123892884 @default.
• W4385422297 cites W2137433526 @default.
• W4385422297 cites W2140795339 @default.
• W4385422297 cites W2151763383 @default.
• W4385422297 cites W2156721705 @default.
• W4385422297 cites W2265909173 @default.
• W4385422297 cites W2278318545 @default.
• W4385422297 cites W2282702692 @default.
• W4385422297 cites W2305851736 @default.
• W4385422297 cites W2345829845 @default.
• W4385422297 cites W2384819789 @default.
• W4385422297 cites W2466082175 @default.
• W4385422297 cites W2552075882 @default.
• W4385422297 cites W2560717077 @default.
• W4385422297 cites W2585112520 @default.
• W4385422297 cites W2585120618 @default.
• W4385422297 cites W2601944289 @default.
• W4385422297 cites W2737436751 @default.
• W4385422297 cites W2748639534 @default.
• W4385422297 cites W2753917120 @default.
• W4385422297 cites W2764274660 @default.
• W4385422297 cites W2768967845 @default.
• W4385422297 cites W2792596103 @default.
• W4385422297 cites W2796379802 @default.
• W4385422297 cites W2914778901 @default.
• W4385422297 cites W2923627075 @default.
• W4385422297 cites W2935337177 @default.
• W4385422297 cites W2946122277 @default.

• next