2019
DOI: 10.1016/j.lithos.2018.12.018
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Geochemical and geochronological constraints on the tectonic setting of the Xinlin ophiolite, northern Great Xing’an Range, NE China

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Cited by 31 publications
(30 citation statements)
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“…Recently, according to the formation age of Xinlin gabbro (480 Ma; Wu et al, 2011). Feng et al (2019) believe that magmatic events are relatively few in NE China and may be in a quiet period from 440 to 380 Ma. Therefore, the inherited zircons may be the products of the expansion, subduction, and returning of the ocean crust.…”
Section: Zircon U-pb Agesmentioning
confidence: 99%
See 1 more Smart Citation
“…Recently, according to the formation age of Xinlin gabbro (480 Ma; Wu et al, 2011). Feng et al (2019) believe that magmatic events are relatively few in NE China and may be in a quiet period from 440 to 380 Ma. Therefore, the inherited zircons may be the products of the expansion, subduction, and returning of the ocean crust.…”
Section: Zircon U-pb Agesmentioning
confidence: 99%
“…F I G U R E 1 (a) Tectonic sketch map showing the main units of central and eastern Asia (Zhou, Wilde, Zhang, Ren, & Zheng, 2011). (b) Tectonic division of the central-northern Great Xing'an Range and distribution of reported U-Pb zircon ages (modified from Feng et al, 2016Feng et al, , 2019; data cited from Du, Han, & Bao, 2013; W. Sun et al, 2014;Feng et al, 2018Feng et al, , 2019. (c) Geological map of the ophiolite in Wunuer area investigated in this study time of collision and amalgamation between these blocks form key topics in understanding the tectonic and geodynamic history of the region.…”
mentioning
confidence: 99%
“…Many studies have suggested that the final closure of the Paleo-Asian Ocean occurred from west to east along the Solonker-Xar Moron-Changchun-Yanji suture zone in a scissor-like closure model [4,[8][9][10][11][12][13]. However, the precise timing of final closure is debated [15,16,18,28,30,31,33].…”
Section: The Final Scissor-like Closure Model Of the Paleo-asian Oceamentioning
confidence: 99%
“…Northeast (NE) China is located at the eastern segment of the CAOB between the Siberian Craton and the North China Craton (Figure 1) [4][5][6][7]. It was formed by long-lived subduction, continental margin accretion, and continent-arc-continent collision due to the closure of the Paleo-Asian Ocean and is a key element for understanding the evolution of the eastern CAOB [4,[8][9][10][11][12][13]. Previous studies have suggested that the closure of the Paleo-Asian Ocean is a scissor-like closure process [4,11]; however, the precise timing of the final closure of the Paleo-Asian Ocean is controversial, and includes proposals for Middle to Late Devonian, Late Devonian to Early Carboniferous, Late Permian, Late Permian to Early Triassic, or even Middle to Late Triassic timing [4,5,10,11,[14][15][16][17].…”
Section: Introductionmentioning
confidence: 99%
“…(a) Simplified tectonic map of the Central Asian Orogenic Belt (modified from Feng et al, 2019; Liu et al, 2017; Zhou, Wilde, Zhang, Ren, & Zheng, 2011). (b) Schematic tectonic map of NE China (modified from Ge, Wu, Zhou, & Zhang, 2007; Wu et al, 2011).…”
Section: Introductionmentioning
confidence: 99%