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• W2572028188 endingPage "74" @default.
• W2572028188 startingPage "54" @default.
• W2572028188 abstract "The Trans-North China Orogen (TNCO) is a major collisional belt along which the Western and Eastern Blocks of the North China Craton were amalgamated through subduction–accretion–collision tectonics during Paleoproterozoic. The Lüliang Complex along the western margin of the TNCO is thought to be the trace of an ancient suture zone. Here we employ magnetotelluric array to build a lithosphere-scale high-resolution 3-D resistivity model for this region. Between 36°N and 38°N, E-W trending slices of the resistivity model show relatively high-conductivity (∼10–100 Ωm) lithospheric mantle of the Western Block that extends eastward beneath the relatively high-resistivity lithosphere of the TNCO at depths from 80 to 180 km. We interpret this east-dipping upper mantle conductivity contrast as the lithosphere-scale suture between the Western Block and TNCO that formed through eastward subduction. The enhanced conductivity of the fossil oceanic subduction zone might be a reflection of the reduction in grain size of olivine grains in mantle peridotite by the localized shearing stress associated with the subduction, combined with the interconnecting high-conductivity minerals along grain boundaries formed through metasomatism by slab-derived fluids. Similar subduction-related boundaries are absent in the resistivity models beneath the northern Lüliang Complex near 39°N, where prominent high-conductivity anomalies indicating asthenosphere upwelling and lower crustal underplating are seen. Such mantle architecture could result from the subduction of an oceanic ridge or slab window, as also proposed for the origin of the subduction-related Luyashan charnockite suite in this region. Our data also suggest that the Phanerozoic tectonic and magmatic events in this region only locally modified the Precambrian lithospheric tectonic framework without total destruction. We propose a 3-D model to illustrate the contrasting Paleoproterozoic tectonic evolution between the northern and southern domains of the Lüliang Complex and the TNCO during the transition stage between the termination of oceanic subduction and the subsequent continental collision." @default.
• W2572028188 created "2017-01-26" @default.
• W2572028188 creator A5027263336 @default.
• W2572028188 creator A5057195398 @default.
• W2572028188 creator A5060053337 @default.
• W2572028188 creator A5088181315 @default.
• W2572028188 date "2017-12-01" @default.
• W2572028188 modified "2023-10-16" @default.
• W2572028188 title "Fossil oceanic subduction zone beneath the western margin of the Trans-North China Orogen: Magnetotelluric evidence from the Lüliang Complex" @default.
• W2572028188 cites W1504722926 @default.
• W2572028188 cites W1563836150 @default.
• W2572028188 cites W1567268310 @default.
• W2572028188 cites W1569043652 @default.
• W2572028188 cites W1577273182 @default.
• W2572028188 cites W1716208990 @default.
• W2572028188 cites W1963766798 @default.
• W2572028188 cites W1964174114 @default.
• W2572028188 cites W1967874909 @default.
• W2572028188 cites W1972295324 @default.
• W2572028188 cites W1973224471 @default.
• W2572028188 cites W1977351304 @default.
• W2572028188 cites W1978338132 @default.
• W2572028188 cites W1980985326 @default.
• W2572028188 cites W1981883491 @default.
• W2572028188 cites W1982274555 @default.
• W2572028188 cites W1984191236 @default.
• W2572028188 cites W1986909225 @default.
• W2572028188 cites W1988871240 @default.
• W2572028188 cites W1989445090 @default.
• W2572028188 cites W1989945922 @default.
• W2572028188 cites W1991243694 @default.
• W2572028188 cites W1991259689 @default.
• W2572028188 cites W1991732676 @default.
• W2572028188 cites W1996545688 @default.
• W2572028188 cites W1996778004 @default.
• W2572028188 cites W1997859575 @default.
• W2572028188 cites W1999186212 @default.
• W2572028188 cites W2000321393 @default.
• W2572028188 cites W2001291680 @default.
• W2572028188 cites W2003181451 @default.
• W2572028188 cites W2003259286 @default.
• W2572028188 cites W2005305925 @default.
• W2572028188 cites W2005520120 @default.
• W2572028188 cites W2005569462 @default.
• W2572028188 cites W2006713945 @default.
• W2572028188 cites W2007546423 @default.
• W2572028188 cites W2007855554 @default.
• W2572028188 cites W2008632580 @default.
• W2572028188 cites W2009148447 @default.
• W2572028188 cites W2011143928 @default.
• W2572028188 cites W2013267275 @default.
• W2572028188 cites W2013708350 @default.
• W2572028188 cites W2014603089 @default.
• W2572028188 cites W2015959750 @default.
• W2572028188 cites W2016861708 @default.
• W2572028188 cites W2017577740 @default.
• W2572028188 cites W2018209057 @default.
• W2572028188 cites W2019621021 @default.
• W2572028188 cites W2024111545 @default.
• W2572028188 cites W2026638428 @default.
• W2572028188 cites W2027170597 @default.
• W2572028188 cites W2027368616 @default.
• W2572028188 cites W2030540205 @default.
• W2572028188 cites W2030612659 @default.
• W2572028188 cites W2033117518 @default.
• W2572028188 cites W2033354344 @default.
• W2572028188 cites W2034208590 @default.
• W2572028188 cites W2039072788 @default.
• W2572028188 cites W2039145047 @default.
• W2572028188 cites W2040076862 @default.
• W2572028188 cites W2041802530 @default.
• W2572028188 cites W2042345416 @default.
• W2572028188 cites W2042360103 @default.
• W2572028188 cites W2042396050 @default.
• W2572028188 cites W2042477030 @default.
• W2572028188 cites W2043003723 @default.
• W2572028188 cites W2047770336 @default.
• W2572028188 cites W2049120158 @default.
• W2572028188 cites W2050596379 @default.
• W2572028188 cites W2055343428 @default.
• W2572028188 cites W2055715194 @default.
• W2572028188 cites W2057235710 @default.
• W2572028188 cites W2059517119 @default.
• W2572028188 cites W2061359484 @default.
• W2572028188 cites W2061983288 @default.
• W2572028188 cites W2062637542 @default.
• W2572028188 cites W2064411977 @default.
• W2572028188 cites W2065463075 @default.
• W2572028188 cites W2066398024 @default.
• W2572028188 cites W2069333276 @default.
• W2572028188 cites W2070724362 @default.
• W2572028188 cites W2072681703 @default.
• W2572028188 cites W2074248188 @default.
• W2572028188 cites W2074463249 @default.
• W2572028188 cites W2074503780 @default.
• W2572028188 cites W2077474983 @default.
• W2572028188 cites W2077479198 @default.
• W2572028188 cites W2077746951 @default.

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