Constraining the deep dynamic process beneath the Bangong-Nujiang suture zone: A case study from the early cretaceous trachytic rocks
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[1] Zhicai Zhu,et al. Ca. 110 Ma adakite-like magmatism along the Bangong–Nujiang suture zone: Implications for crustal thickening and early uplift in the central Tibetan Plateau , 2021, Palaeogeography, Palaeoclimatology, Palaeoecology.
[2] Wang Wei,et al. Cretaceous magmatic rocks in the Nyima area, North Tibet: Constraints for the tectonic evolution of the Bangong-Nujiang suture zone , 2021 .
[3] Haoruo Wu,et al. Simultaneous growth and reworking of the Lhasa basement: A case study from Early Cretaceous magmatism in the north-central Tibet , 2020 .
[4] Haoruo Wu,et al. Late Cretaceous adakitic rocks from the western Tibetan Plateau: implications for the subduction of the Neo-Tethys Ocean , 2020, International Geology Review.
[5] Qing-guo Zhai,et al. Transition from oceanic subduction to continental collision recorded in the Bangong-Nujiang suture zone: Insights from Early Cretaceous magmatic rocks in the north-central Tibet , 2020 .
[6] Xiao Wenjiao,et al. Tethyan geodynamics , 2020, Acta Petrologica Sinica.
[7] Peng Sun,et al. Late early Cretaceous peraluminous biotite granites along the Bangong–Nujiang suture zone, Central Tibet: Products derived by partial melting of metasedimentary rocks? , 2019, Lithos.
[8] Haoruo Wu,et al. Closure of the Bangong–Nujiang Tethyan Ocean in the central Tibet: Results from the provenance of the Duoni Formation , 2019, Journal of Sedimentary Research.
[9] Wei Li,et al. Early Cretaceous sedimentary evolution of the northern Lhasa terrane and the timing of initial Lhasa-Qiangtang collision , 2019, Gondwana Research.
[10] W. Xiao,et al. Cyclical one-way continental rupture-drift in the Tethyan evolution: Subduction-driven plate tectonics , 2019, Science China Earth Sciences.
[11] A. Matsuoka,et al. Late Anisian radiolarian assemblages from the Yarlung‐Tsangpo Suture Zone in the Jinlu area, Zedong, southern Tibet: Implications for the evolution of Neotethys , 2019, Island Arc.
[12] Xiumian Hu,et al. The disappearance of a Late Jurassic remnant sea in the southern Qiangtang Block (Shamuluo Formation, Najiangco area): Implications for the tectonic uplift of central Tibet , 2018, Palaeogeography, Palaeoclimatology, Palaeoecology.
[13] Jun Chen,et al. Temporal and spatial variations of Late Mesozoic granitoids in the SW Qiangtang, Tibet: Implications for crustal architecture, Meso-Tethyan evolution and regional mineralization , 2018, Earth-Science Reviews.
[14] Qiang-tai Huang,et al. Origin and tectonic implications of the Shiquanhe high-Mg andesite, western Bangong suture, Tibet , 2018, Gondwana Research.
[15] H. Sinclair,et al. Early Cretaceous palaeogeographic evolution of the Coqen Basin in the Lhasa Terrane, southern Tibetan Plateau , 2017 .
[16] Qing-guo Zhai,et al. Late Early Cretaceous magmatic rocks (118–113 Ma) in the middle segment of the Bangong–Nujiang suture zone, Tibetan Plateau: Evidence of lithospheric delamination , 2017 .
[17] Ming Wang,et al. Reconstructing in space and time the closure of the middle and western segments of the Bangong–Nujiang Tethyan Ocean in the Tibetan Plateau , 2017, International Journal of Earth Sciences.
[18] R. Shi,et al. A syn-collisional model for Early Cretaceous magmatism in the northern and central Lhasa subterranes , 2017 .
[19] N. Evans,et al. Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane, Tibet , 2016 .
[20] L. Ding,et al. Petrogenesis of Middle–Late Triassic volcanic rocks from the Gangdese belt, southern Lhasa terrane: Implications for early subduction of Neo-Tethyan oceanic lithosphere , 2016 .
[21] Peter A. Cawood,et al. Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction , 2016 .
[22] Wangchun Xu,et al. Adakite-like geochemical signature produced by amphibole-dominated fractionation of arc magmas: An example from the Late Cretaceous magmatism in Gangdese belt, south Tibet , 2015 .
[23] R. Shi,et al. Late Triassic island-arc--back-arc basin development along the Bangong-Nujiang suture zone (central Tibet): Geological, geochemical and chronological evidence from volcanic rocks , 2015 .
[24] Cai Li,et al. Early Cretaceous adakitic magmatism in the Dachagou area, northern Lhasa terrane, Tibet: Implications for slab roll-back and subsequent slab break-off of the lithosphere of the Bangong–Nujiang Ocean , 2015 .
[25] M. Santosh,et al. Slab breakoff triggered ca. 113 Ma magmatism around Xainza area of the Lhasa Terrane, Tibet☆ , 2014 .
[26] Kuo‐Lung Wang,et al. SHRIMP zircon U-Pb geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane, northern Tibet and geodynamic implications , 2013 .
[27] Hong-lin Yuan,et al. Compositional diversity of ca. 110 Ma magmatism in the northern Lhasa Terrane, Tibet: Implications for the magmatic origin and crustal growth in a continent–continent collision zone , 2013 .
[28] Z. Hou,et al. The origin and pre-Cenozoic evolution of the Tibetan Plateau , 2013 .
[29] G. Pan,et al. Tectonic evolution of the Qinghai-Tibet Plateau , 2012 .
[30] W. Griffin,et al. Melt/mantle mixing produces podiform chromite deposits in ophiolites : implications of Re-Os systematics in the Dongqiao Neo-tethyan ophiolite, northern Tibet , 2012 .
[31] C. Faccenna,et al. Mantle conveyor beneath the Tethyan collisional belt , 2011 .
[32] F. Huang,et al. Geochemical contrasts between early Cretaceous ore-bearing and ore-barren high-Mg adakites in central-eastern China: Implications for petrogenesis and Cu–Au mineralization , 2010 .
[33] Z. Hou,et al. The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth , 2010 .
[34] B. Dai,et al. Melting of enriched Archean subcontinental lithospheric mantle: Evidence from the ca 1760Ma volcanic rocks of the Xiong'er Group, southern margin of the North China Craton , 2010 .
[35] H. Martin,et al. THE ORIGIN OF FERROAN-POTASSIC A-TYPE GRANITOIDS: THE CASE OF THE HORNBLENDE-BIOTITE GRANITE SUITE OF THE MESOPROTEROZOIC MAZURY COMPLEX, NORTHEASTERN POLAND , 2010 .
[36] Wei-Qiang Ji,et al. Detrital zircon U–Pb and Hf isotopic data from the Xigaze fore-arc basin: Constraints on Transhimalayan magmatic evolution in southern Tibet , 2010 .
[37] Shan Gao,et al. Continental and Oceanic Crust Recycling-induced Melt^Peridotite Interactions in the Trans-North China Orogen: U^Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths , 2010 .
[38] Fu-Yuan Wu,et al. Geochemical investigation of Early Cretaceous igneous rocks along an east–west traverse throughout the central Lhasa Terrane, Tibet , 2009 .
[39] Wei-Qiang Ji,et al. Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith, southern Tibet , 2009 .
[40] G. Dong,et al. Early cretaceous subduction-related adakite-like rocks of the Gangdese Belt, southern Tibet: Products of slab melting and subsequent melt-peridotite interaction? , 2009 .
[41] J. Miller,et al. Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICPMS , 2008 .
[42] Wei Yang,et al. Geochronology and geochemistry of the Mesozoic volcanic rocks in Western Liaoning: Implications for lithospheric thinning of the North China Craton , 2008 .
[43] Mei-Fu Zhou,et al. Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China : Their relationship to the Emeishan mantle plume , 2007 .
[44] V. Garduño-Monroy,et al. Geology and geochemistry characteristics of the Chiapanecan Volcanic Arc (Central Area), Chiapas Mexico , 2007 .
[45] D. Champion,et al. An overview of adakite, tonalite–trondhjemite–granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution , 2005 .
[46] U. Schaltegger,et al. The Composition of Zircon and Igneous and Metamorphic Petrogenesis , 2003 .
[47] R. Kilian,et al. Constraints on the interaction between slab melts and the mantle wedge from adakitic glass in peridotite xenoliths , 2002 .
[48] An Yin,et al. Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .
[49] N. Petford,et al. Na-rich Partial Melts from Newly Underplated Basaltic Crust: the Cordillera Blanca Batholith, Peru , 1996 .
[50] A. Hofmann,et al. Hydrous, silica-rich melts in the sub-arc mantle and their relationship with erupted arc lavas , 1995, Nature.
[51] I. Metcalfe. Gondwanaland origin, dispersion, and accretion of East and Southeast Asian continental terranes , 1994 .
[52] M. Drummond,et al. Derivation of some modern arc magmas by melting of young subducted lithosphere , 1990, Nature.
[53] J. Pearce,et al. The ophiolites of the Tibetan Geotraverses, Lhasa to Golmud (1985) and Lhasa to Kathmandu (1986) , 1988, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[54] R. W. Le Maitre,et al. A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram , 1986 .
[55] J. Gill. Orogenic Andesites and Plate Tectonics , 1981 .
[56] A. Şengör,et al. Mid-Mesozoic closure of Permo–Triassic Tethys and its implications , 1979, Nature.
[57] E. Middlemost. The basalt clan , 1975 .