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• W2139688051 endingPage "1194" @default.
• W2139688051 startingPage "1173" @default.
• W2139688051 abstract "The 14 November 2001 Kokoxili, Tibet, earthquake ( M w 7.8) ruptured ∼400 km of the western Kunlun fault in northern Tibet. We apply two inversion methods to P and SH waves recorded by the Global Seismographic Network to recover the spatial and temporal history of the rupture process. The observed surface rupture consists of two strike-slip segments, offset by an extensional step-over. Little surface rupture was observed in the graben system in this step-over, which is approximately 45 km long and over 10 km wide. Our results imply that the rupture did not jump this large gap, but that the rupture was continuous through the graben. The earthquake began with a small strike-slip subevent, presumably along the westernmost of the two segments. This was followed 5 sec later by a subevent of about the same magnitude but having an oblique mechanism with a large normal-faulting component. The likely location for this subevent is within the graben. This oblique-slip event probably enabled transfer of the rupture onto the main Kunlun fault. The main moment release began ∼18 sec after rupture initiation and propagated over 350 km eastward along the Kunlun fault. Slip on this segment was very heterogeneous, averaging ∼2 m for the first 200 km, followed by a sharp increase to a maximum of 7.5 m within the next 50 km, and then a rapid decline. The average rupture velocity along the main segment was high (∼3.6 km sec -1 ) and probably exceeded the local shear-wave velocity. The M w 7.8 Kokoxili earthquake had a longer surface rupture and faster average rupture velocity, radiated more energy, and probably had a lower average fracture energy than the November 2002, M w 7.9 Denali fault (Alaska) earthquake. Evidence suggests that the velocity of the rupture front dropped significantly after passing the point of maximum slip, implying a large difference in frictional strength between the two ends of the fault. Online material : Waveform fits to teleseismic body waves." @default.
• W2139688051 created "2016-06-24" @default.
• W2139688051 creator A5048557293 @default.
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• W2139688051 date "2004-08-01" @default.
• W2139688051 modified "2023-09-28" @default.
• W2139688051 title "The 14 November 2001 Kokoxili (Kunlunshan), Tibet, Earthquake: Rupture Transfer through a Large Extensional Step-Over" @default.
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• W2139688051 cites W1507384737 @default.
• W2139688051 cites W1775797309 @default.
• W2139688051 cites W1965098282 @default.
• W2139688051 cites W1968894582 @default.
• W2139688051 cites W1972833650 @default.
• W2139688051 cites W1973758910 @default.
• W2139688051 cites W1974155702 @default.
• W2139688051 cites W1974451966 @default.
• W2139688051 cites W1976542747 @default.
• W2139688051 cites W1976617725 @default.
• W2139688051 cites W1979526534 @default.
• W2139688051 cites W1980899146 @default.
• W2139688051 cites W1986047667 @default.
• W2139688051 cites W1988158662 @default.
• W2139688051 cites W1990582471 @default.
• W2139688051 cites W2002029124 @default.
• W2139688051 cites W2004428748 @default.
• W2139688051 cites W2012630864 @default.
• W2139688051 cites W2014390861 @default.
• W2139688051 cites W2041774199 @default.
• W2139688051 cites W2045641625 @default.
• W2139688051 cites W2053548789 @default.
• W2139688051 cites W2053639074 @default.
• W2139688051 cites W2054999338 @default.
• W2139688051 cites W2058413866 @default.
• W2139688051 cites W2058949675 @default.
• W2139688051 cites W2062221814 @default.
• W2139688051 cites W2071672567 @default.
• W2139688051 cites W2076547603 @default.
• W2139688051 cites W2077215931 @default.
• W2139688051 cites W2079335235 @default.
• W2139688051 cites W2081882231 @default.
• W2139688051 cites W2084493749 @default.
• W2139688051 cites W2085705453 @default.
• W2139688051 cites W2090939723 @default.
• W2139688051 cites W2093308116 @default.
• W2139688051 cites W2103113534 @default.
• W2139688051 cites W2106641143 @default.
• W2139688051 cites W2110448165 @default.
• W2139688051 cites W2110961704 @default.
• W2139688051 cites W2111180693 @default.
• W2139688051 cites W2113955130 @default.
• W2139688051 cites W2128251347 @default.
• W2139688051 cites W2129159015 @default.
• W2139688051 cites W2129742752 @default.
• W2139688051 cites W2130917613 @default.
• W2139688051 cites W2132888318 @default.
• W2139688051 cites W2136275493 @default.
• W2139688051 cites W2136338903 @default.
• W2139688051 cites W2140386203 @default.
• W2139688051 cites W2141396940 @default.
• W2139688051 cites W2150075840 @default.
• W2139688051 cites W2151088060 @default.
• W2139688051 cites W2151365379 @default.
• W2139688051 cites W2151924958 @default.
• W2139688051 cites W2152546160 @default.
• W2139688051 cites W2155307869 @default.
• W2139688051 cites W2163763308 @default.
• W2139688051 cites W2164468626 @default.
• W2139688051 cites W2167065192 @default.
• W2139688051 cites W2173409465 @default.
• W2139688051 cites W2270732534 @default.
• W2139688051 cites W2275750751 @default.
• W2139688051 cites W2322069610 @default.
• W2139688051 cites W2334849072 @default.
• W2139688051 cites W2565197769 @default.
• W2139688051 cites W3009463201 @default.
• W2139688051 cites W3010394131 @default.
• W2139688051 cites W3023538743 @default.
• W2139688051 cites W591303395 @default.
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• W2139688051 doi "https://doi.org/10.1785/012003180" @default.
• W2139688051 hasPublicationYear "2004" @default.
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