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- W1993844183 abstract "The Solonker suture zone is one of the most important tectonic boundaries in the southeastern part of the Central Asian Orogenic Belt (CAOB). An ~ 630 km-long reflection seismic profile across this suture was recently completed by the Chinese SinoProbe Project. The processed seismic data show clear crustal structures and provide new constraints on the tectonic and crustal evolution models. The Moho is delineated as a relatively flat boundary between a strongly reflective lower crust and a transparent mantle at a depth of ~ 40–45 km (~ 14.5 s two-way travel time), which is in agreement with the refraction data recorded along the same profile. In a broad view, the profile images an orogen that appears bivergent with, and approximately centered on, the Solonker suture zone. The southern portion of this profile is dominated by a crustal-scale, cratonward propagating fold-and-thrust system that formed during the late Permian and Triassic through collision and subsequent convergence in a post-collisional stage. The major thrust faults are truncated by Mesozoic granitoid plutons in the upper crust and by the Moho at the base of the crust. This geometry suggests that the Moho was formed after the thrusting event. The northern portion of the profile, although partially obliterated by post-collisional magmatic bodies, shows major south-dipping folding and thrusting. Bands of layered reflectors immediately overlying the Moho are interpreted as basaltic sills derived from the mantle. Episodic mafic underplating may have occurred in this region, giving rise to post-collisional magmatic events and renewal of the Moho. A few mantle reflectors are also visible. The overall geometry of these mantle reflectors supports the tectonic models that the southern orogen (Manchurides) experienced south-directed subduction and the northern orogen (Altaids) underwent north-directed subduction prior to collision along the Solonker suture zone." @default.
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- W1993844183 date "2014-02-01" @default.
- W1993844183 modified "2023-10-14" @default.
- W1993844183 title "Crustal structures revealed from a deep seismic reflection profile across the Solonker suture zone of the Central Asian Orogenic Belt, northern China: An integrated interpretation" @default.
- W1993844183 cites W120028556 @default.
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- W1993844183 cites W1952619490 @default.
- W1993844183 cites W1967198581 @default.
- W1993844183 cites W1974438203 @default.
- W1993844183 cites W1974796447 @default.
- W1993844183 cites W1975676133 @default.
- W1993844183 cites W1983072117 @default.
- W1993844183 cites W1984494567 @default.
- W1993844183 cites W1984637606 @default.
- W1993844183 cites W1986983284 @default.
- W1993844183 cites W1987732834 @default.
- W1993844183 cites W1988317790 @default.
- W1993844183 cites W1990701109 @default.
- W1993844183 cites W1992019984 @default.
- W1993844183 cites W1992516451 @default.
- W1993844183 cites W1992903525 @default.
- W1993844183 cites W1995897602 @default.
- W1993844183 cites W2002245641 @default.
- W1993844183 cites W2003323528 @default.
- W1993844183 cites W2006146493 @default.
- W1993844183 cites W2013067052 @default.
- W1993844183 cites W2013739893 @default.
- W1993844183 cites W2014364988 @default.
- W1993844183 cites W2016937874 @default.
- W1993844183 cites W2017587656 @default.
- W1993844183 cites W2019259962 @default.
- W1993844183 cites W2019695435 @default.
- W1993844183 cites W2020946896 @default.
- W1993844183 cites W2023621032 @default.
- W1993844183 cites W2026930689 @default.
- W1993844183 cites W2028345447 @default.
- W1993844183 cites W2029506771 @default.
- W1993844183 cites W2032353260 @default.
- W1993844183 cites W2034223887 @default.
- W1993844183 cites W2037091312 @default.
- W1993844183 cites W2038449935 @default.
- W1993844183 cites W2054620046 @default.
- W1993844183 cites W2060089581 @default.
- W1993844183 cites W2060482519 @default.
- W1993844183 cites W2062126220 @default.
- W1993844183 cites W2064440709 @default.
- W1993844183 cites W2068704074 @default.
- W1993844183 cites W2071432070 @default.
- W1993844183 cites W2077238634 @default.
- W1993844183 cites W2077976828 @default.
- W1993844183 cites W2078011306 @default.
- W1993844183 cites W2078816109 @default.
- W1993844183 cites W2079920926 @default.
- W1993844183 cites W2081020685 @default.
- W1993844183 cites W2082379982 @default.
- W1993844183 cites W2085717916 @default.
- W1993844183 cites W2086498883 @default.
- W1993844183 cites W2086841814 @default.
- W1993844183 cites W2089096123 @default.
- W1993844183 cites W2089426009 @default.
- W1993844183 cites W2090015082 @default.
- W1993844183 cites W2093898661 @default.
- W1993844183 cites W2099233919 @default.
- W1993844183 cites W2105181795 @default.
- W1993844183 cites W2117935716 @default.
- W1993844183 cites W2128712155 @default.
- W1993844183 cites W2130869872 @default.
- W1993844183 cites W2138013731 @default.
- W1993844183 cites W2168359944 @default.
- W1993844183 cites W2169036982 @default.
- W1993844183 cites W2170868101 @default.
- W1993844183 cites W2318240411 @default.
- W1993844183 cites W3146398826 @default.
- W1993844183 cites W3149707589 @default.
- W1993844183 doi "https://doi.org/10.1016/j.tecto.2013.11.035" @default.
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