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• W2061678478 abstract "The 2008 M w 7.9 Wenchuan earthquake ruptured an imbricate thrust system in the Longmen Shan range, which forms the eastern boundary of the Tibetan Plateau. We use seismic reflection data and surface geology to construct geologic cross sections and a three-dimensional (3D) fault model in the range front. The rupture was complex, with slip on both the steeply dipping Beichuan fault and the more shallowly dipping Pengguan fault, which appear to merge at depth. In contrast, only the Beichuan fault ruptured in the north, with the transition near a lateral fault offset. Thus, the earthquake involved multiple thrust splays and breached a significant segment boundary. To investigate the tectonic setting of the earthquake, we extend our previous measurements of crustal shortening (Hubbard and Shaw, 2009) into the interior of the range and show that shortening correlates with topography. This suggests that upper-crustal shortening can produce the high topography of the Longmen Shan without calling on other uplift mechanisms. Based on this understanding, we model the thrust belt as a critical taper wedge, to assess what rock and fault strengths are required to explain the topographic slopes within the range front and basin. The low taper within the basin is consistent with a weak detachment ( δ f ≈0.1), while a slightly stronger ( δ f ≈0.3–0.4) detachment is necessary to explain the higher taper of the range front. This difference may relate to the localization of the detachment within a Triassic evaporite sequence within the basin, while the faults beneath the range front are rooted in Precambrian metasedimentary or igneous rocks. Critical taper theory implies that shortening in the range front where the 2008 Wenchuan earthquake occurred is many times greater than in the basin, consistent with our shortening measurements. We examine the implications of these findings for seismic hazard assessment in the region and in other active mountain belts around the world." @default.
• W2061678478 created "2016-06-24" @default.
• W2061678478 creator A5008816346 @default.
• W2061678478 creator A5018130887 @default.
• W2061678478 creator A5058298574 @default.
• W2061678478 date "2010-10-19" @default.
• W2061678478 modified "2023-10-05" @default.
• W2061678478 title "Structural Setting of the 2008 Mw 7.9 Wenchuan, China, Earthquake" @default.
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• W2061678478 cites W1963721836 @default.
• W2061678478 cites W1965337507 @default.
• W2061678478 cites W1973341400 @default.
• W2061678478 cites W1973936656 @default.
• W2061678478 cites W1977156689 @default.
• W2061678478 cites W1979867347 @default.
• W2061678478 cites W1982508701 @default.
• W2061678478 cites W1984774984 @default.
• W2061678478 cites W1997667374 @default.
• W2061678478 cites W2011656167 @default.
• W2061678478 cites W2012594522 @default.
• W2061678478 cites W2013856174 @default.
• W2061678478 cites W2014201444 @default.
• W2061678478 cites W2023091835 @default.
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• W2061678478 cites W2083330317 @default.
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• W2061678478 doi "https://doi.org/10.1785/0120090341" @default.
• W2061678478 hasPublicationYear "2010" @default.
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