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• W4220804998 endingPage "200" @default.
• W4220804998 startingPage "176" @default.
• W4220804998 abstract "The Archean Eastern Liaoning metamorphic basement block is located in the northeastern North China Craton (NCC), in which ∼2.9 to 3.8 Ga lithological assemblages are well developed. The region which exposed these ancient lithological assemblages is usually called as an ancient continental nucleus. Toward north from the northeastern margin of the ancient continental nucleus, ∼2.5 to 2.7 Ga lithological assemblages continuously developed, forming abundant ∼2.5 Ga tonalite- trondhjemite- granodiorite (TTG) and high-K granitoids. Some ∼2.7 Ga TTG gneisses and metamorphic calk-alkaline volcanic rocks have also been documented recently in the Eastern Liaoning to the Southern Jilin of northeastern NCC. Our geological investigations found that many big ∼2.7 Ga TTG gneiss enclaves are preserved in the ∼2.5 Ga granitoids in the northeastern NCC. The early Neoarchean (∼2.7 Ga) TTG gneisses are exposed in the Waitoushan-Baishan areas, together with many contemporaneous subduction-related metamorphic calk-alkaline volcanic rocks in the Helong area of Southern Jilin province, constituting a nearly E-W-trending ∼2.7 Ga island arc belt in the northeastern NCC. However, the ∼2.7 Ga geological record is absent within the Anshan-Benxi-Waitoushan ancient microblock (ABWN) domain, suggesting that the ∼2.7 Ga arc belt was formed far away from the ABWN domain. The petrogenesis of ∼2.52–2.59 Ga TTG and sanukitoid gneisses, integrating with contemporaneous top-to-the-NE thrusting structural features, indicate that the new oceanic crust in the Waitoushan-Weiziyu-Jiubing (WWJ) area subducted to the southwest from ∼2.53–2.60 Ga. At the Archean end, the northern Liaoning-eastern Hebei intraoceanic arc system subducted to the southeast, which led to the final amalgamation among the ABWN, WWJ and northern Liaoning areas. Subsequently (∼2.50–2.53 Ga), the subducted slab broke off and the collisions between the arc and ancient continental nucleus, as well as the arc and arc, resulted in the generation of extensive crust-derived high-K granitoids." @default.
• W4220804998 created "2022-04-03" @default.
• W4220804998 creator A5018029613 @default.
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• W4220804998 creator A5089426898 @default.
• W4220804998 date "2022-07-01" @default.
• W4220804998 modified "2023-10-13" @default.
• W4220804998 title "Neoarchean granitoids and tectonic regime of lateral growth in northeastern North China Craton" @default.
• W4220804998 cites W1467008107 @default.
• W4220804998 cites W1964047299 @default.
• W4220804998 cites W1965394610 @default.
• W4220804998 cites W1966700794 @default.
• W4220804998 cites W1967635228 @default.
• W4220804998 cites W1973876227 @default.
• W4220804998 cites W1979705656 @default.
• W4220804998 cites W1981122034 @default.
• W4220804998 cites W1981259355 @default.
• W4220804998 cites W1985885839 @default.
• W4220804998 cites W1988215475 @default.
• W4220804998 cites W1990593047 @default.
• W4220804998 cites W1994228585 @default.
• W4220804998 cites W2009171179 @default.
• W4220804998 cites W2009732140 @default.
• W4220804998 cites W2009895667 @default.
• W4220804998 cites W2010409639 @default.
• W4220804998 cites W2011607179 @default.
• W4220804998 cites W2013940511 @default.
• W4220804998 cites W2017141475 @default.
• W4220804998 cites W2017181284 @default.
• W4220804998 cites W2019035841 @default.
• W4220804998 cites W2019273078 @default.
• W4220804998 cites W2024248666 @default.
• W4220804998 cites W2027545949 @default.
• W4220804998 cites W2028536499 @default.
• W4220804998 cites W2028802548 @default.
• W4220804998 cites W2030328451 @default.
• W4220804998 cites W2035670944 @default.
• W4220804998 cites W2039669657 @default.
• W4220804998 cites W2042986233 @default.
• W4220804998 cites W2043003723 @default.
• W4220804998 cites W2044620880 @default.
• W4220804998 cites W2050926313 @default.
• W4220804998 cites W2051164400 @default.
• W4220804998 cites W2052028650 @default.
• W4220804998 cites W2053721096 @default.
• W4220804998 cites W2055172418 @default.
• W4220804998 cites W2056723788 @default.
• W4220804998 cites W2061359484 @default.
• W4220804998 cites W2063368192 @default.
• W4220804998 cites W2064241548 @default.
• W4220804998 cites W2068967748 @default.
• W4220804998 cites W2071782561 @default.
• W4220804998 cites W2071878446 @default.
• W4220804998 cites W2072620570 @default.
• W4220804998 cites W2075210745 @default.
• W4220804998 cites W2077085454 @default.
• W4220804998 cites W2080824639 @default.
• W4220804998 cites W2081923019 @default.
• W4220804998 cites W2088105278 @default.
• W4220804998 cites W2088824219 @default.
• W4220804998 cites W2089954248 @default.
• W4220804998 cites W2090206242 @default.
• W4220804998 cites W2090742495 @default.
• W4220804998 cites W2105636247 @default.
• W4220804998 cites W2111713504 @default.
• W4220804998 cites W2113397447 @default.
• W4220804998 cites W2123753516 @default.
• W4220804998 cites W2127994322 @default.
• W4220804998 cites W2131368249 @default.
• W4220804998 cites W2136857107 @default.
• W4220804998 cites W2138522501 @default.
• W4220804998 cites W2144596067 @default.
• W4220804998 cites W2147361256 @default.
• W4220804998 cites W2149787537 @default.
• W4220804998 cites W2153546088 @default.
• W4220804998 cites W2168001619 @default.
• W4220804998 cites W2175372297 @default.
• W4220804998 cites W2216056899 @default.
• W4220804998 cites W2253143849 @default.
• W4220804998 cites W2260953749 @default.
• W4220804998 cites W2275243530 @default.
• W4220804998 cites W2333248244 @default.
• W4220804998 cites W2333966633 @default.
• W4220804998 cites W2413679096 @default.
• W4220804998 cites W2419102025 @default.
• W4220804998 cites W2461480964 @default.
• W4220804998 cites W248673451 @default.
• W4220804998 cites W2508596546 @default.
• W4220804998 cites W2511984283 @default.
• W4220804998 cites W2521455060 @default.
• W4220804998 cites W2523098605 @default.
• W4220804998 cites W2524350816 @default.

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