Early Paleozoic to Devonian multiple-accretionary model for the Qilian Shan, NW China

Xiao, Wenjiao; Windley, Brian F.; Yong, Yong; Yan, Zhen; Yuan, Chao; Liu, Chuan-Zhou; Li, Jiliang

doi:10.1016/j.jseaes.2008.10.001

Cited by 369 publications

(266 citation statements)

References 88 publications

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“…The North Qilian Accretionary Belt records globally one of the earliest "cold" oceanic subduction zones, in response to the closure of the ancient Qilian Ocean between the Alashan and Qilian-Qaidam blocks during the Early Paleozoic (Wu et al, 1993;Song et al, 2006Song et al, , 2007Song et al, , 2009Song et al, , 2013Zhang et al, 2007;Yin et al, 2007;Xiao et al, 2009). It consists of Precambrian basement, Early Paleozoic subduction-related rock associations (ophiolite complexes, high-pressure/ low-temperature metamorphic rocks, arc-related volcanic and intrusive rocks),…”

Section: Accepted M Manuscriptmentioning

confidence: 99%

Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?

Zhang

Song

Yang

et al. 2017

Lithos

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'Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen : accretion of a Cambrian Oceanic Plateau? ', Lithos.,[278][279][280][281] 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-pro t 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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Section: Accepted M Manuscriptmentioning

confidence: 99%

Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?

Zhang

Song

Yang

et al. 2017

Lithos

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“…The Mohe gneiss within the NQ-UHPM is the oldest sampled crystalline basement in the QOB, dated at ~ 2.5 Ga , and the inherited zircons with ages >2.6 Ga confirm the existence of an Archean basement in the region (Huang et al, 2015;. Different models have been proposed to explain the tectonic evolution in the whole QOB (Xu et al, 1994;Yin and Harrison, 2000;Yang et al, 2002;Gehrels et al, 2003Gehrels et al, , 2011Song et al, 2006Song et al, , 2013Song et al, , 2014Wu et al, 2006Wu et al, , 2010Xu Z. Q, 2006;Xiao et al, 2009;Huang et al, 2015). The…”

Section: Geological Backgroundmentioning

confidence: 99%

Garnet effect on Nd-Hf isotope decoupling: Evidence from the Jinfosi batholith, Northern Tibetan Plateau

Huang

Niu

2017

Lithos

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Additional information: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-pro t 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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“…(2) The Central Qilian Block (CQB), considered as an arc-accretionary system, is dominated by Precambrian basement overlain by the Paleozoic sedimentary lithologies (Tung et al 2012;Xiao et al 2009;Xu et al 2010a, b), as well as the synchronous granitoids, granitic gneisses, amphibolites and minor granulites (Huang et al 2015;Song et al 2013Song et al , 2014. Recent studies suggest that the Central Qilian Block and Qaidam Block have close affinities with the Yangtze Craton (Darby and Gehrels 2006;Gehrels et al 2003b;Tung et al 2012;Xu et al 2015), but this is debatable (Huang et al 2015).…”

Section: Geological Setting and Petrographymentioning

confidence: 99%

“…Furthermore, the subdivision of the South Qilian Orogenic Belt (dotted line in Fig. 1b) composed of volcanic rocks and limestones (Xiao et al 2009) on the basis of limited study, is also questionable; (3) The North Qaidam UHPM Belt is dominated by granitic and pelitic gneisses with eclogite lenses. Previous studies indicate that the North Qaidam UHPM Belt has experienced the processes from continental deep subduction to subsequent exhumation (Liu et al 2012;Song et al 2009bSong et al , 2014Zhang et al 2010); (4) The Qaidam Block (QDB), has a Precambrian meta-crystalline basement overlain by the Paleozoic-Mesozoic sedimentary strata (Song et al 2013(Song et al , 2014).…”

Section: Geological Setting and Petrographymentioning

confidence: 99%

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Petrogenesis of granitoids in the eastern section of the Central Qilian Block: Evidence from geochemistry and zircon U-Pb geochronology

Niu

Chen

et al. 2016

Miner Petrol

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(2017) 'Petrogenesis of granitoids in the eastern section of the Central Qilian Block : evidence from geochemistry and zircon U-Pb geochronology.', Mineralogy and petrology., 111 (1). pp. 23-41. Further information on publisher's website:https://doi.org/10.1007/s00710-016-0461-3Publisher's copyright statement:The nal publication is available at Springer via https://doi.org/10.1007/s00710-016-0461-3Additional information: 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-pro t 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.

show abstract

Early Paleozoic to Devonian multiple-accretionary model for the Qilian Shan, NW China

Cited by 369 publications

References 88 publications

Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?

Basalts and picrites from a plume-type ophiolite in the South Qilian Accretionary Belt, Qilian Orogen: Accretion of a Cambrian Oceanic Plateau?

Garnet effect on Nd-Hf isotope decoupling: Evidence from the Jinfosi batholith, Northern Tibetan Plateau

Petrogenesis of granitoids in the eastern section of the Central Qilian Block: Evidence from geochemistry and zircon U-Pb geochronology

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