Spatial–temporal relationships of Mesozoic volcanic rocks in NE China: Constraints on tectonic overprinting and transformations between multiple tectonic regimes

Xu, Wen‐Liang; Pei, Fu‐Ping; Wang, Feng; Meng, En; Ji, Wei‐Qiang; Yang, Debin; Wang, Wei

doi:10.1016/j.jseaes.2013.04.003

Cited by 720 publications

(582 citation statements)

References 74 publications

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“…The mafic intrusions were previously considered to have formed in late Paleozoic, but the precise emplacement ages are lacking. The Mesozoic geological evolution of the area was characterized by eruption of voluminous lavas, granitoid emplacement and deposition of terrestrial sediments, probably as a result of subduction of the paleo-Pacific Ocean (Zhang et al, 2004;Li et al, 2007;Xu et al, 2013b;Guo et al, 2015).…”

Section: Geological Backgroundsmentioning

confidence: 99%

Variable sediment flux in generation of Permian subduction-related mafic intrusions from the Yanbian region, NE China

Guo

et al. 2016

Lithos

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Section: Geological Backgroundsmentioning

confidence: 99%

Variable sediment flux in generation of Permian subduction-related mafic intrusions from the Yanbian region, NE China

Guo

et al. 2016

Lithos

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“…Others argue that the Russian Far East and NE China were geologically active continental margin related to the subduction of the paleo-Pacific plate during 130-100 Ma (Faure and Natal'in, 1992;Kiminami and Imaoka, 2013;Sun et al, 2013;Wu et al, 2011;Xu et al, 2013). The exact position of the plate boundary, whether subduction or transform, is unknown.…”

Section: Accepted M Manuscriptmentioning

confidence: 99%

“…It is generally considered that the Mesozoic granitoid magmatism in the eastern continental Asia was associated with the paleo-Pacific plate subduction and the spatial-temporal distribution of the granitoids has thus been used to discuss the tectonic evolution of the paleo-Pacific plate (Niu et al, 2015;Wu et al, 2011;Xu et al, 2013). It is thus necessary to reconstruct the late Mesozoic-early Cenozoic tectonics of the eastern Asian continental margin.…”

Section: Asian Continental Marginmentioning

confidence: 99%

“…They are enriched in LREEs and LILEs, and depleted in HFSEs, consistent with being of subduction origin. The Late Cretaceous (97-88 Ma) granitoids, dacites and andesites in Tongjiang and Yanji areas of NE China with similar geochemical characteristics were interpreted to have formed in an active continental margin (Ji et al, 2007, Xu et al, 2013Yu et al, 2013). It is generally accepted that the eastern Asian margin has experienced successive seafloor subduction with occasional oceanic ridge subduction since the Paleozoic (Isozaki, 1996;Isozaki et al, 2010;Maruyama et al, 1997).…”

Section: Asian Continental Marginmentioning

confidence: 99%

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Geochronology and geochemistry of Late Cretaceous–Paleocene granitoids in the Sikhote-Alin Orogenic Belt: Petrogenesis and implications for the oblique subduction of the paleo-Pacific plate

Tang

Niu

et al. 2016

Lithos

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) 'Geochronology and geochemistry of Late CretaceousPaleocene granitoids in the Sikhote-Alin Orogenic Belt : petrogenesis and implications for the oblique subduction of the paleo-Pacic plate. ', Lithos.,[266][267] Further information on publisher's website: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. A C C E P T E D M A N U S C R I P T ACCEPTED MANUSCRIPT

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“…The composite eastern NCC block amalgamated with the western NCC block to form the NCC via a~1.85 Ga continent-continent collision (Zhao et al, 2005). Long after stabilization, the NCC experienced massive circum-craton Phanerozoic subduction and collisional orogenies, manifested in several orogenic belts: the Early Paleozoic Qilianshan Orogen to the west, the Late Paleozoic Xing-Meng Orogenic Belt to the north, and the Late Permian to Triassic Qinling-Dabie-Sulu ultra-high pressure metamorphic orogenic belt to the south and east, as well as the Jurassic onset of the Paleo-Pacific Ocean plate subduction beneath eastern China (Xu et al, 2013a). The sinistral Tan-Lu strike-slip fault system likely formed following the collision of the Yangtze Craton and NCC during the Triassic, which led to the creation of the Qinling-DabieSulu Belt (Yin and Nie, 1993).…”

Section: Geological Settings and Samplesmentioning

confidence: 99%

Big insights from tiny peridotites: Evidence for persistence of Precambrian lithosphere beneath the eastern North China Craton

et al. 2015

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Previous studies have shown that the eastern North China Craton (NCC) lost its ancient lithospheric mantle root during the Phanerozoic. The temporal sequence, spatial extent, and cause of the lithospheric thinning, however, continue to be debated. Here we report olivine compositions, whole-rock Re-Os isotopic systematics, and platinum-group element abundances of small (b 2 cm in maximum dimension) mantle peridotite xenoliths from two basalt localities from the eastern NCC, Wudi (Cenozoic) and Fuxin (Cretaceous). These locations lie far (~150-200 km) from the Tan-Lu fault, which has been linked to lithospheric replacement in the eastern NCC. Peridotites at both locations have fertile to moderately refractory compositions (Fo b 91.5), while highly refractory (Fo N 92) lithospheric mantle is largely absent. Osmium isotopic data suggest the Wudi peridotites experienced melt depletion primarily during the Paleoproterozoic (~1.8 Ga), although an Archean Os model age for one xenolith indicates incorporation of a minor component of Archean lithospheric mantle. These data suggest that a previously unrecognized Paleoproterozoic orogenic event removed and replaced the original Archean lithospheric mantle beneath the sedimentary basin at the southern edge of the Bohai Sea. By contrast, the Fuxin peridotites, entrained in Cretaceous basalts that crop out along the northern edge of the eastern NCC, document the coexistence of both ancient (≥2.3 Ga) and modern lithospheric mantle components. Here, the original Late Archean-Early Paleoproterozoic lithospheric mantle was, at least partially, removed and replaced prior to 100 Ma. Combined with literature data, our results show that removal of the original Archean lithosphere occurred within Proterozoic collisional orogens, and that replacement of Precambrian lithosphere during the Mesozoic may have been spatially associated with the collisional boundaries and the strike-slip Tan-Lu fault, as well as the onset of Paleo-Pacific plate subduction.

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Spatial–temporal relationships of Mesozoic volcanic rocks in NE China: Constraints on tectonic overprinting and transformations between multiple tectonic regimes

Cited by 720 publications

References 74 publications

Variable sediment flux in generation of Permian subduction-related mafic intrusions from the Yanbian region, NE China

Variable sediment flux in generation of Permian subduction-related mafic intrusions from the Yanbian region, NE China

Geochronology and geochemistry of Late Cretaceous–Paleocene granitoids in the Sikhote-Alin Orogenic Belt: Petrogenesis and implications for the oblique subduction of the paleo-Pacific plate

Big insights from tiny peridotites: Evidence for persistence of Precambrian lithosphere beneath the eastern North China Craton

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