Sub-arc mantle heterogeneity in oxygen isotopes: evidence from Permian mafic–ultramafic intrusions in the Central Asian Orogenic Belt
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K. Qin | Shengchao Xue | E. Ripley | Chusi Li | Z. Yao
[1] R. Klemd,et al. Final Assembly of the Southwestern Central Asian Orogenic Belt as Constrained by the Evolution of the South Tianshan Orogen: Links With Gondwana and Pangea , 2018, Journal of Geophysical Research: Solid Earth.
[2] K. Qin,et al. Geochronological, mineralogical and geochemical studies of sulfide mineralization in the Podong mafic-ultramafic intrusion in northern Xinjiang, western China , 2018, Ore Geology Reviews.
[3] Qingfei Wang,et al. Permian bimodal magmatism in the southern margin of the Central Asian Orogenic Belt, Beishan, Xinjiang, NW China: Petrogenesis and implication for post-subduction crustal growth , 2018, Lithos.
[4] B. Windley,et al. Late Paleozoic to early Triassic multiple roll-back and oroclinal bending of the Mongolia collage in Central Asia , 2017, Earth-Science Reviews.
[5] Guochun Zhao,et al. Final amalgamation of the Tianshan and Junggar orogenic collage in the southwestern Central Asian Orogenic Belt: Constraints on the closure of the Paleo-Asian Ocean , 2017, Earth-Science Reviews.
[6] Song-Yue Yu,et al. An integrated chemical and oxygen isotopic study of primitive olivine grains in picrites from the Emeishan Large Igneous Province, SW China: Evidence for oxygen isotope heterogeneity in mantle sources , 2017 .
[7] Jin-Hui Yang,et al. Zircon Hf-O isotope evidence for recycled oceanic and continental crust in the sources of alkaline rocks , 2017 .
[8] Jun Gao,et al. A subduction channel model for exhumation of oceanic-type high-pressure to ultrahigh-pressure eclogite-facies metamorphic rocks in SW Tianshan, China , 2016, Science China Earth Sciences.
[9] He Huang,et al. Petrogenesis of the Bashisuogong bimodal igneous complex in southwest Tianshan Mountains, China: Implications for the Tarim Large Igneous Province , 2016 .
[10] Ya-Jing Mao,et al. Crustal contamination and sulfide immiscibility history of the Permian Huangshannan magmatic Ni-Cu sulfide deposit, East Tianshan, NW China , 2016 .
[11] P. Holm,et al. Subduction zone mantle enrichment by fluids and Zr–Hf-depleted crustal melts as indicated by backarc basalts of the Southern Volcanic Zone, Argentina , 2016 .
[12] Ya-Jing Mao,et al. Geochronological, Petrological, and Geochemical Constraints on Ni-Cu Sulfide Mineralization in the Poyi Ultramafic-Troctolitic Intrusion in the Northeast Rim of the Tarim Craton, Western China , 2016 .
[13] K. Qin,et al. A non-plume model for the Permian protracted (266-286 Ma) basaltic magmatism in the Beishan-Tianshan region, Xinjiang, Western China , 2016 .
[14] Yanrong Liu,et al. The impact of early sulfur saturation and calc-crustal contamination on ore-forming process in the Posan mafic–ultramafic complex: Derived from the shallow depleted mantle, Beishan region, NW China , 2016 .
[15] O. Nebel,et al. The flaw in the crustal 'zircon archive': Mixed hf isotope signatures record progressive contamination of late-stage liquid in mafic-ultramafic layered intrusions , 2016 .
[16] Tao Wang,et al. Petrogenesis of the Early Permian volcanic rocks in the Chinese South Tianshan: Implications for crustal growth in the Central Asian Orogenic Belt , 2015 .
[17] Yang Zhang,et al. Recycling of sediment into the mantle source of K-rich mafic rocks: Sr–Nd–Hf–O isotopic evidence from the Fushui complex in the Qinling orogen , 2014, Contributions to Mineralogy and Petrology.
[18] Wei-Qiang Ji,et al. A ‘hidden’ 18O-enriched reservoir in the sub-arc mantle , 2014, Scientific Reports.
[19] Yue-heng Yang,et al. Qinghu zircon: A working reference for microbeam analysis of U-Pb age and Hf and O isotopes , 2013 .
[20] W. Xiao,et al. Provenance of metasedimentary rocks from the Beishan orogenic collage, southern Altaids: Constraints from detrital zircon U–Pb and Hf isotopic data , 2013 .
[21] Liang Zhao,et al. Formation of mafic magmas through lower crustal AFC processes - An example from the Jinan gabbroic intrusion in the North China Block , 2013 .
[22] F. Guo,et al. Crustal recycling processes in generating the early Cretaceous Fangcheng basalts, North China Craton: New constraints from mineral chemistry, oxygen isotopes of olivine and whole-rock geochemistry , 2013 .
[23] Yong‐Fei Zheng,et al. The nature of orogenic lithospheric mantle: Geochemical constraints from postcollisional mafic–ultramafic rocks in the Dabie orogen , 2012 .
[24] H. Marschall,et al. Arc magmas sourced from melange diapirs in subduction zones , 2012 .
[25] M. Santosh,et al. Late Paleozoic post-collisional magmatism in the Eastern Tianshan Belt, Northwest China: New insights from geochemistry, geochronology and petrology of bimodal volcanic rocks , 2011 .
[26] Zhaojie Guo,et al. Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South Tian Shan Orogen, Central Asia, and implications for the Northern Xinjiang, western China , 2011 .
[27] A. Crawford,et al. Slab break-off and the formation of Permian mafic-ultramafic intrusions in southern margin of Central Asian Orogenic Belt, Xinjiang, NW China , 2011 .
[28] T. Plank,et al. The Hf–Nd isotopic composition of marine sediments , 2011 .
[29] R. Klemd,et al. Changes in dip of subducted slabs at depth: Petrological and geochronological evidence from HP-UHP rocks (Tianshan, NW-China) , 2011 .
[30] Ping Liu,et al. U-Pb ages and Hf-O isotopes of zircons from Late Paleozoic mafic-ultramafic units in the southern Central Asian Orogenic Belt: Tectonic implications and evidence for an Early-Permian mantle plume , 2011 .
[31] Yue-heng Yang,et al. Zircon Hf–O isotope evidence for crust–mantle interaction during continental deep subduction , 2011 .
[32] I. Bindeman,et al. Oxygen isotope heterogeneity of the mantle beneath the Canary Islands: insights from olivine phenocrysts , 2011 .
[33] J. Beckett,et al. Fe–Mg Partitioning between Olivine and High-magnesian Melts and the Nature of Hawaiian Parental Liquids , 2011 .
[34] Ping Liu,et al. SIMS zircon U-Pb geochronology and Sr-Nd isotopes of Ni-Cu-Bearing Mafic-Ultramafic Intrusions in Eastern Tianshan and Beishan in correlation with flood basalts in Tarim Basin (NW China): Constraints on a ca. 280 Ma mantle plume , 2011, American Journal of Science.
[35] H. Furnes,et al. Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere , 2011 .
[36] J. Charvet,et al. Palaeozoic tectonic evolution of the Tianshan belt, NW China , 2011 .
[37] M. Willbold,et al. Formation of enriched mantle components by recycling of upper and lower continental crust , 2010 .
[38] Yue-heng Yang,et al. Penglai Zircon Megacrysts: A Potential New Working Reference Material for Microbeam Determination of Hf–O Isotopes and U–Pb Age , 2010 .
[39] Yue-heng Yang,et al. Petrogenesis and tectonic significance of the ~850 Ma Gangbian alkaline complex in South China: Evidence from in situ zircon U-Pb dating, Hf-O isotopes and whole-rock geochemistry , 2010 .
[40] Peter A. Cawood,et al. Accretionary orogens through Earth history , 2009 .
[41] S. Hauck,,et al. Re–Os and O isotopic variations in magnetite from the contact zone of the Duluth Complex and the Biwabik Iron Formation, northeastern Minnesota , 2008 .
[42] N. Arndt,et al. Role of recycled oceanic basalt and sediment in generating the Hf–Nd mantle array , 2008 .
[43] I. Bindeman. Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis , 2008 .
[44] I. Bindeman,et al. Boron and oxygen isotope evidence for recycling of subducted components over the past 2.5 Gyr , 2007, Nature.
[45] Yue-heng Yang,et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U–Pb geochronology , 2006 .
[46] W. Griffin,et al. Trace element and isotopic composition of GJ-red zircon standard by laser ablation , 2006 .
[47] Han Bao,et al. Late Paleozoic vertical growth of continental crust around the Junggar Basin,Xinjiang,China(PartI):Timing of post-collisionai plutonism , 2006 .
[48] T. Pettke,et al. Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth , 2005, Nature.
[49] Yong‐Fei Zheng,et al. Zircon U-Pb age, element and C-O isotope geochemistry of post-collisional mafic-ultramafic rocks from the Dabie orogen in east-central China , 2005 .
[50] S. Eggins,et al. Zircon Hf-isotope analysis with an excimer laser, depth profiling, ablation of complex geometries, and concomitant age estimation , 2004 .
[51] Kuo‐Lung Wang. Geochemical Constraints for the Genesis of Post-collisional Magmatism and the Geodynamic Evolution of the Northern Taiwan Region , 2004 .
[52] J. Valley,et al. Volcanic arc of Kamchatka: a province with high-δ18O magma sources and large-scale 18O/16O depletion of the upper crust , 2004 .
[53] R. Carlson,et al. Unusual coexistence of subduction-related and intraplate-type magmatism: Sr, Nd and Pb isotope and trace element data from the magmatism of the San Pedro–Ceboruco graben (Nayarit, Mexico) , 2003 .
[54] K. Righter,et al. Source contamination versus assimilation: an example from the Trans-Mexican Volcanic Arc , 2002 .
[55] J. Eiler. Oxygen Isotope Variations of Basaltic Lavas and Upper Mantle Rocks , 2001 .
[56] C. Lo,et al. Crust–mantle interaction induced by deep subduction of the continental crust: geochemical and Sr–Nd isotopic evidence from post-collisional mafic–ultramafic intrusions of the northern Dabie complex, central China , 1999 .
[57] M. Searle,et al. Tectonic setting, origin, and obduction of the Oman ophiolite , 1999 .
[58] J. Valley,et al. Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts , 1998 .
[59] J. Eiler,et al. Oxygen isotope evidence for slab-derived fluids in the sub-arc mantle , 1998, Nature.
[60] Charles H. Langmuir,et al. The chemical composition of subducting sediment and its consequences for the crust and mantle , 1998 .
[61] H. Craig,et al. Oxygen isotope variations in ocean island basalt phenocrysts , 1997 .
[62] H. Craig,et al. Oxygen isotope evidence against bulk recycled sediment in the mantle sources of Pitcairn Island lavas , 1995, Nature.
[63] R. Harmon,et al. Oxygen isotope heterogeneity of the mantle deduced from global 18O systematics of basalts from different geotectonic settings , 1995 .
[64] Mark S. Ghiorso,et al. Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures , 1995 .
[65] D. Lowry,et al. Oxygen isotope composition of mantle peridotite , 1994 .
[66] T. Lay. The Fate of Descending Slabs , 1994 .
[67] H. Chiba. Oxygen isotope fractionations involving diopside, forsterite, magnetite, and calcite: Application to geothermometry : , , and (1989) Goechim. Cosmochim. Acta 53 , 2985-2995 , 1991 .
[68] K. Muehlenbachs. Chapter 12. ALTERATION of the OCEANIC CRUST and the 18O HISTORY of SEAWATER , 1986 .
[69] K. Muehlenbachs. Alteration of the oceanic crust and the 18 O history of seawater , 1986 .
[70] Albrecht W. Hofmann,et al. Mantle plumes from ancient oceanic crust , 1982 .
[71] Shen-su Sun,et al. Chemical heterogeneity of the Archaean mantle, composition of the earth and mantle evolution , 1977 .
[72] J. Hoefs. Stable Isotope Geochemistry , 1973 .
[73] R. Clayton,et al. The use of bromine pentafluoride in the extraction of oxygen from oxides and silicates for isotopic analysis , 1963 .