Matches in SemOpenAlex for { <https://semopenalex.org/work/W2050871585> ?p ?o ?g. }
- W2050871585 endingPage "n/a" @default.
- W2050871585 startingPage "n/a" @default.
- W2050871585 abstract "[1] Subduction zone plate boundary megathrust faults accommodate relative plate motions with spatially varying sliding behavior. The 2004 Sumatra-Andaman (Mw 9.2), 2010 Chile (Mw 8.8), and 2011 Tohoku (Mw9.0) great earthquakes had similar depth variations in seismic wave radiation across their wide rupture zones – coherent teleseismic short-period radiation preferentially emanated from the deeper portion of the megathrusts whereas the largest fault displacements occurred at shallower depths but produced relatively little coherent short-period radiation. We represent these and other depth-varying seismic characteristics with four distinct failure domains extending along the megathrust from the trench to the downdip edge of the seismogenic zone. We designate the portion of the megathrust less than 15 km below the ocean surface as domain A, the region of tsunami earthquakes. From 15 to ∼35 km deep, large earthquake displacements occur over large-scale regions with only modest coherent short-period radiation, in what we designate as domain B. Rupture of smaller isolated megathrust patches dominate in domain C, which extends from ∼35 to 55 km deep. These isolated patches produce bursts of coherent short-period energy both in great ruptures and in smaller, sometimes repeating, moderate-size events. For the 2011 Tohoku earthquake, the sites of coherent teleseismic short-period radiation are close to areas where local strong ground motions originated. Domain D, found at depths of 30–45 km in subduction zones where relatively young oceanic lithosphere is being underthrust with shallow plate dip, is represented by the occurrence of low-frequency earthquakes, seismic tremor, and slow slip events in a transition zone to stable sliding or ductile flow below the seismogenic zone." @default.
- W2050871585 created "2016-06-24" @default.
- W2050871585 creator A5001452413 @default.
- W2050871585 creator A5015709391 @default.
- W2050871585 creator A5019138159 @default.
- W2050871585 creator A5032613807 @default.
- W2050871585 creator A5052197567 @default.
- W2050871585 creator A5055979975 @default.
- W2050871585 creator A5074301415 @default.
- W2050871585 creator A5082647864 @default.
- W2050871585 date "2012-04-01" @default.
- W2050871585 modified "2023-10-16" @default.
- W2050871585 title "Depth-varying rupture properties of subduction zone megathrust faults" @default.
- W2050871585 cites W1487409102 @default.
- W2050871585 cites W1510841103 @default.
- W2050871585 cites W1513444457 @default.
- W2050871585 cites W1522296717 @default.
- W2050871585 cites W1549786948 @default.
- W2050871585 cites W1560076455 @default.
- W2050871585 cites W1563219554 @default.
- W2050871585 cites W1588203029 @default.
- W2050871585 cites W1612272730 @default.
- W2050871585 cites W1627794111 @default.
- W2050871585 cites W1653322462 @default.
- W2050871585 cites W1659874525 @default.
- W2050871585 cites W1665176202 @default.
- W2050871585 cites W1668424321 @default.
- W2050871585 cites W1783205279 @default.
- W2050871585 cites W1828504277 @default.
- W2050871585 cites W1840778637 @default.
- W2050871585 cites W1842026185 @default.
- W2050871585 cites W1967150943 @default.
- W2050871585 cites W1968688970 @default.
- W2050871585 cites W1970078712 @default.
- W2050871585 cites W1970302283 @default.
- W2050871585 cites W1970651719 @default.
- W2050871585 cites W1971431926 @default.
- W2050871585 cites W1972074236 @default.
- W2050871585 cites W1975501867 @default.
- W2050871585 cites W1978294558 @default.
- W2050871585 cites W1978947945 @default.
- W2050871585 cites W1979920203 @default.
- W2050871585 cites W1982307620 @default.
- W2050871585 cites W1989188749 @default.
- W2050871585 cites W1989509352 @default.
- W2050871585 cites W1994994476 @default.
- W2050871585 cites W2001874346 @default.
- W2050871585 cites W2004366374 @default.
- W2050871585 cites W2008660245 @default.
- W2050871585 cites W2011000549 @default.
- W2050871585 cites W2012347529 @default.
- W2050871585 cites W2012972590 @default.
- W2050871585 cites W2014782452 @default.
- W2050871585 cites W2017274089 @default.
- W2050871585 cites W2017325167 @default.
- W2050871585 cites W2017481021 @default.
- W2050871585 cites W2017611649 @default.
- W2050871585 cites W2019317415 @default.
- W2050871585 cites W2019611228 @default.
- W2050871585 cites W2021063270 @default.
- W2050871585 cites W2021574151 @default.
- W2050871585 cites W2022774905 @default.
- W2050871585 cites W2026024577 @default.
- W2050871585 cites W2026338384 @default.
- W2050871585 cites W2028121951 @default.
- W2050871585 cites W2030654837 @default.
- W2050871585 cites W2033253901 @default.
- W2050871585 cites W2033331760 @default.
- W2050871585 cites W2033577285 @default.
- W2050871585 cites W2036168488 @default.
- W2050871585 cites W2037168657 @default.
- W2050871585 cites W2038644291 @default.
- W2050871585 cites W2039015562 @default.
- W2050871585 cites W2039724866 @default.
- W2050871585 cites W2040197273 @default.
- W2050871585 cites W2042521829 @default.
- W2050871585 cites W2043704065 @default.
- W2050871585 cites W2044709616 @default.
- W2050871585 cites W2046735996 @default.
- W2050871585 cites W2048816495 @default.
- W2050871585 cites W2052201950 @default.
- W2050871585 cites W2054591717 @default.
- W2050871585 cites W2059477612 @default.
- W2050871585 cites W2061824192 @default.
- W2050871585 cites W2062221814 @default.
- W2050871585 cites W2063346332 @default.
- W2050871585 cites W2065914103 @default.
- W2050871585 cites W2068133258 @default.
- W2050871585 cites W2072322762 @default.
- W2050871585 cites W2073324480 @default.
- W2050871585 cites W2076966703 @default.
- W2050871585 cites W2077076159 @default.
- W2050871585 cites W2077291550 @default.
- W2050871585 cites W2079921730 @default.
- W2050871585 cites W2081082344 @default.
- W2050871585 cites W2084928725 @default.
- W2050871585 cites W2085127199 @default.
- W2050871585 cites W2086215816 @default.