Heterogeneous mantle beneath the Neo-Tethys Ocean revealed by ultramafic rocks from the Xiugugabu Ophiolite in the Yarlung-Tsangpo Suture Zone, southwestern Tibet
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O. Müntener | Chuan-Zhou Liu | Wen-Bin Ji | Chang Zhang | Tong Liu | Zhen‐Yu Zhang | Wei‐Qi Zhang | A. Bénard | Fu-Yuan Wu
[1] W. Griffin,et al. Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere , 2022, Nature Communications.
[2] R. Arculus,et al. Spinel Harzburgite-Derived Silicate Melts Forming Sulfide-Bearing Orthopyroxenite in the Lithosphere. Part 1: Partition Coefficients and Volatile Evolution Accompanying Fluid- and Redox-Induced Sulfide Formation , 2022, Frontiers in Earth Science.
[3] Yan Liang,et al. Decoupled Trace Element and Isotope Compositions Recorded in Orthopyroxene and Clinopyroxene in Composite Pyroxenite Veins from the Xiugugabu Ophiolite (SW Tibet) , 2022, Journal of Petrology.
[4] Xiang Zhou,et al. Xigaze ophiolite (South Tibet) records complex melt-fluid-peridotite interaction in the crust-mantle transition zone beneath oceanic slow-ultraslow spreading centers , 2022, Lithos.
[5] Chuan-Zhou Liu,et al. An origin of ultraslow spreading ridges for the Yarlung-Tsangpo ophiolites , 2021, Fundamental Research.
[6] A. Sanfilippo,et al. Ancient refractory asthenosphere revealed by mantle re-melting at the Arctic Mid Atlantic Ridge , 2021, Earth and Planetary Science Letters.
[7] B. Su,et al. Supplemental Material: Subduction initiation-induced rapid emplacement of garnet-bearing peridotites at a nascent forearc: Petrological and Os-Li isotopic evidence from the Purang ophiolite, Tibet , 2021, GSA Bulletin.
[8] H. Dick,et al. Tectonic Controls on Block Rotation and Sheeted Sill Emplacement in the Xigaze Ophiolite (Tibet): The Construction Mode of Slow‐Spreading and Ultraslow‐Spreading Oceanic Crusts , 2021, Geochemistry, Geophysics, Geosystems.
[9] Tong Liu,et al. Heterogeneous sub-ridge mantle of the Neo-Tethys: Constraints from Re-Os isotope and HSE compositions of the Xigaze ophiolites , 2020 .
[10] H. Dick,et al. The Xigaze ophiolite: fossil ultraslow-spreading ocean lithosphere in the Tibetan Plateau , 2020, Journal of the Geological Society.
[11] Meijuan Zhao,et al. Geochemical evidence for forearc metasomatism of peridotite in the Xigaze ophiolite during subduction initiation in Neo-Tethyan Ocean, south to Tibet , 2020 .
[12] Wei Lin,et al. Melt extraction and reaction in the forearc mantle: Constraints from trace elements and isotope geochemistry of ultra-refractory peridotites of the New Caledonia Peridotite Nappe , 2020 .
[13] Tong Liu,et al. Evolution of mantle peridotites from the Luobusa ophiolite in the Tibetan Plateau: Sr-Nd-Hf-Os isotope constraints , 2020, Lithos.
[14] D. Pearson,et al. The complex life cycle of oceanic lithosphere: A study of Yarlung-Zangbo ophiolitic peridotites, Tibet , 2020 .
[15] W. Griffin,et al. Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective , 2020 .
[16] B. Su,et al. “Garnet” Lherzolites in the Purang Ophiolite, Tibet: Evidence for Exhumation of Deep Oceanic Lithospheric Mantle , 2020, Geophysical Research Letters.
[17] Nina Liu,et al. Origin of Mesozoic ophiolitic mélanges in the western Yarlung Zangbo suture zone, SW Tibet , 2019 .
[18] C. Tao,et al. Osmium isotope compositions and highly siderophile element abundances in abyssal peridotites from the Southwest Indian Ridge: Implications for evolution of the oceanic upper mantle , 2019, Lithos.
[19] Tong Liu,et al. Subduction re-initiation at dying ridge of Neo-Tethys: Insights from mafic and metamafic rocks in Lhaze ophiolitic mélange, Yarlung-Tsangbo Suture Zone , 2019, Earth and Planetary Science Letters.
[20] Chuan-Zhou Liu,et al. Subduction-Induced Fractionated Highly Siderophile Element Patterns in Forearc Mantle , 2019, Minerals.
[21] A. Sanfilippo,et al. Role of ancient, ultra-depleted mantle in Mid-Ocean-Ridge magmatism , 2019, Earth and Planetary Science Letters.
[22] Fu-Yuan Wu,et al. Reconsideration of Neo-Tethys evolution constrained from the nature of the Dazhuqu ophiolitic mantle, southern Tibet , 2019, Contributions to Mineralogy and Petrology.
[23] Fu-Yuan Wu,et al. Limited Recycling of Crustal Osmium in Forearc Mantle During Slab Dehydration , 2018, Acta Geologica Sinica - English Edition.
[24] Y. Dilek,et al. Melt evolution of upper mantle peridotites and mafic dikes in the northern ophiolite belt of the western Yarlung Zangbo suture zone (southern Tibet) , 2018 .
[25] Tong Liu,et al. Ultra-refractory mantle domains in the Luqu ophiolite (Tibet): Petrology and tectonic setting , 2017 .
[26] B. Wood,et al. The roles of pyroxenite and peridotite in the mantle sources of oceanic basalts , 2017 .
[27] Y. Dilek,et al. Petrological and Re-Os isotopic constraints on the origin and tectonic setting of the Cuobuzha peridotite, Yarlung Zangbo suture zone, southwest Tibet, China , 2017 .
[28] Y. Dilek,et al. Petrological and Re-Os Isotopic Constraints on the Origin and Tectonic Setting of the Cuobuzha Peridotite, Yarlung Zangbo Suture Zone, SW Tibet, China , 2017 .
[29] W. Griffin,et al. Two‐layered oceanic lithospheric mantle in a Tibetan ophiolite produced by episodic subduction of Tethyan slabs , 2017 .
[30] R. Walker,et al. 186 Os– 187 Os and highly siderophile element abundance systematics of the mantle revealed by abyssal peridotites and Os-rich alloys , 2017 .
[31] L. Ding,et al. Processes of initial collision and suturing between India and Asia , 2017, Science China Earth Sciences.
[32] W. Griffin,et al. Recycling of ancient subduction-modified mantle domains in the Purang ophiolite (southwestern Tibet) , 2016 .
[33] E. Garzanti,et al. The timing of India-Asia collision onset – Facts, theories, controversies , 2016 .
[34] J. Warren. Global variations in abyssal peridotite compositions , 2016 .
[35] Peter A. Williams,et al. Mantle Recycling: Transition Zone Metamorphism of Tibetan Ophiolitic Peridotites and its Tectonic Implications , 2016 .
[36] S. Guo,et al. Tethyan suturing in Southeast Asia: Zircon U-Pb and Hf-O isotopic constraints from Myanmar ophiolites , 2016 .
[37] W. Griffin,et al. Southward trench migration at ~130-120 Ma caused accretion of the Neo-Tethyan forearc lithosphere in Tibetan ophiolites , 2016 .
[38] R. Walker,et al. Use of Hydrofluoric Acid Desilicification in the Determination of Highly Siderophile Element Abundances and Re‐Pt‐Os Isotope Systematics in Mafic‐Ultramafic Rocks , 2016 .
[39] T. Morishita,et al. Rhenium-osmium isotope fractionation at the oceanic crust-mantle boundary , 2016 .
[40] Y. Dilek,et al. Petrological and Os isotopic constraints on the origin of the Dongbo peridotite massif, Yarlung Zangbo Suture Zone, Western Tibet , 2015 .
[41] Yan Liang,et al. Temperatures and cooling rates recorded in REE in coexisting pyroxenes in ophiolitic and abyssal peridotites , 2015 .
[42] K. Hodges,et al. Forearc hyperextension dismembered the south Tibetan ophiolites , 2015 .
[43] Yongjun Lu,et al. A genetic linkage between subduction- and collision-related porphyry Cu deposits in continental collision zones , 2015 .
[44] A. McCarthy,et al. Ancient depletion and mantle heterogeneity: Revisiting the Permian-Jurassic paradox of Alpine peridotites , 2015 .
[45] J. Snow,et al. Constraints from Os-isotope variations on the origin of Lena Trough abyssal peridotites and implications for the composition and evolution of the depleted upper mantle , 2014 .
[46] D. Ionov,et al. Melt– and Fluid–Rock Interaction in Supra-Subduction Lithospheric Mantle: Evidence from Andesite-hosted Veined Peridotite Xenoliths , 2013 .
[47] Chengshan Wang,et al. Rapid forearc spreading between 130 and 120 Ma: Evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibet , 2013 .
[48] P. Kelemen,et al. Along‐Strike Variation in the Aleutian Island Arc: Genesis of High Mg# Andesite and Implications for Continental Crust , 2013 .
[49] J. Warren,et al. Lead and osmium isotopic constraints on the oceanic mantle from single abyssal peridotite sulfides , 2012 .
[50] B. Romanowicz,et al. Cluster analysis of global lower mantle tomography: A new class of structure and implications for chemical heterogeneity , 2012 .
[51] A. Stracke. Earth's heterogeneous mantle: A product of convection-driven interaction between crust and mantle , 2012 .
[52] M. Thirlwall,et al. Garnet clinopyroxenite layers from the mantle sequences of the Northern Apennine ophiolites (Italy): Evidence for recycling of crustal material , 2012 .
[53] Chengshan Wang,et al. The Indus–Yarlung Zangbo ophiolites from Nanga Parbat to Namche Barwa syntaxes, southern Tibet: First synthesis of petrology, geochemistry, and geochronology with incidences on geodynamic reconstructions of Neo-Tethys , 2012 .
[54] Chengshan Wang,et al. Discovery of a dismembered metamorphic sole in the Saga ophiolitic mélange, South Tibet: Assessing an Early Cretaceous disruption of the Neo-Tethyan supra-subduction zone and consequences on basin closing , 2012 .
[55] Fu-Yuan Wu,et al. Preservation of ancient Os isotope signatures in the Yungbwa ophiolite (southwestern Tibet) after subduction modification , 2012 .
[56] D. Ionov,et al. A new petrogenetic model for low‐Ca boninites: Evidence from veined sub‐arc xenoliths on melt‐mantle interaction and melt fractionation , 2012 .
[57] S. Meffre,et al. The metamorphic sole of New Caledonia ophiolite: 40Ar/39Ar, U‐Pb, and geochemical evidence for subduction inception at a spreading ridge , 2012 .
[58] Chenguang Sun,et al. A REE-in-two-pyroxene thermometer for mafic and ultramafic rocks , 2012 .
[59] Chengshan Wang,et al. Petrology and geochemistry of peridotites in the Zhongba ophiolite, Yarlung Zangbo Suture Zone: Implications for the Early Cretaceous intra-oceanic subduction zone within the Neo-Tethys , 2011 .
[60] D. Günther,et al. Abyssal peridotite Hf isotopes identify extreme mantle depletion , 2011 .
[61] Chengshan Wang,et al. Petrology and geochemistry of the Xiugugabu ophiolitic massif, western Yarlung Zangbo suture zone, Tibet , 2011 .
[62] E. Nakamura,et al. An assessment of upper mantle heterogeneity based on abyssal peridotite isotopic compositions , 2009 .
[63] Yue-heng Yang,et al. Temporal Evolution of the Lithospheric Mantle beneath the Eastern North China Craton , 2009 .
[64] A. Hofmann,et al. Non-chondritic HSE budget in Earth's upper mantle evidenced by abyssal peridotites from Gakkel ridge (Arctic Ocean) , 2009 .
[65] B. Burchfiel,et al. The Geological Evolution of the Tibetan Plateau , 2008, Science.
[66] B. Xia,et al. Platinum-group elemental geochemistry of mafic and ultramafic rocks from the Xigaze ophiolite, southern Tibet , 2008 .
[67] Albrecht W. Hofmann,et al. Ancient, highly heterogeneous mantle beneath Gakkel ridge, Arctic Ocean , 2008, Nature.
[68] P. Szatmari,et al. Geophysical and geochemical evidence for cold upper mantle beneath the Equatorial Atlantic Ocean , 2008 .
[69] O. Alard,et al. The scale and origin of the osmium isotope variations in mid-ocean ridge basalts , 2007 .
[70] R. Walker,et al. Highly siderophile element composition of the Earth’s primitive upper mantle: Constraints from new data on peridotite massifs and xenoliths , 2006 .
[71] N. Rogers,et al. Ancient melt extraction from the oceanic upper mantle revealed by Re–Os isotopes in abyssal peridotites from the Mid-Atlantic ridge , 2006 .
[72] M. Storey,et al. New insights into the origin and distribution of the DUPAL isotope anomaly in the Indian Ocean mantle from MORB of the Southwest Indian Ridge , 2005 .
[73] W. Griffin,et al. In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle , 2005, Nature.
[74] C. Herzberg. Geodynamic Information in Peridotite Petrology , 2004 .
[75] B. Dupré,et al. Osmium isotopic constraints on the nature of the DUPAL anomaly from Indian mid-ocean-ridge basalts , 2004, Nature.
[76] T. Meisel,et al. Reference materials for geochemical PGE analysis : new analytical data for Ru, Rh, Pd, Os, Ir, Pt and Re by isotope dilution ICP-MS in 11 geological reference materials , 2004 .
[77] E. Bonatti,et al. Oceanic crust generated by elusive parents: Sr and Nd isotopes in basalt-peridotite pairs from the Mid-Atlantic Ridge , 2004 .
[78] T. Barry,et al. A combined basalt and peridotite perspective on 14 million years of melt generation at the Atlantis Bank segment of the Southwest Indian Ridge: Evidence for temporal changes in mantle dynamics? , 2004 .
[79] V. Salters,et al. Composition of the depleted mantle , 2003 .
[80] J. Lorand,et al. Sulfide petrology and highly siderophile element geochemistry of abyssal peridotites: a coupled study of samples from the Kane Fracture Zone (45°W 23°20N, MARK area, Atlantic Ocean) , 2003 .
[81] P. Hoppe,et al. Garnet-field melting and late-stage refertilization in "Residual" abyssal peridotites from the Central Indian Ridge , 2002 .
[82] H. Dick,et al. Mineralogy of the mid-ocean-ridge basalt source from neodymium isotopic composition of abyssal peridotites , 2002, Nature.
[83] Peter E. van Keken,et al. MANTLE MIXING: The Generation, Preservation, and Destruction of Chemical Heterogeneity , 2002 .
[84] G. Stampfli,et al. A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons , 2002 .
[85] J. Blusztajn,et al. Abyssal peridotite osmium isotopic compositions from cr‐spinel , 2002 .
[86] W. Wegscheider,et al. Recognizing heterogeneous distribution of platinum group elements (PGE) in geological materials by means of the Re–Os isotope system , 2001, Analytical and Bioanalytical Chemistry.
[87] R. Walker,et al. Osmium isotopic compositions of mantle xenoliths: A global perspective , 2001 .
[88] A. Hofmann,et al. Coupled major and trace elements as indicators of the extent of melting in mid-ocean-ridge peridotites , 2001, Nature.
[89] An Yin,et al. Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .
[90] J. Morgan,et al. 190Pt–186Os and 187Re–187Os systematics of abyssal peridotites , 2000 .
[91] H. Becker. Re–Os fractionation in eclogites and blueschists and the implications for recycling of oceanic crust into the mantle , 2000 .
[92] E. Bonatti,et al. Trace and REE content of clinopyroxenes from supra-subduction zone peridotites. Implications for melting and enrichment processes in island arcs , 2000 .
[93] Hai. B. O. Zou. Modeling of trace element fractionation during non-modal dynamic melting with linear variations in mineral/melt distribution coefficients , 2000 .
[94] J. Fitton,et al. Non-chondritic platinum-group element ratios in oceanic mantle lithosphere: petrogenetic signature of melt percolation? , 1999 .
[95] Allègre,et al. Direct measurement of femtomoles of osmium and the 187Os/186Os ratio in seawater , 1998, Science.
[96] R. Walker,et al. THE Re-Os ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY , 1998 .
[97] C. Langmuir,et al. The origin of abyssal peridotites: a new perspective , 1997 .
[98] R. Vannucci,et al. Chemistry and origin of trapped melts in ophioiitic peridotites , 1997 .
[99] J. Birck,et al. Re‐Os Isotopic Measurements at the Femtomole Level in Natural Samples , 1997 .
[100] P. Kelemen,et al. A review of melt migration processes in the adiabatically upwelling mantle beneath oceanic spreading ridges , 1997, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.
[101] R. Kinzler. Melting of mantle peridotite at pressures approaching the spinel to garnet transition: Application to mid‐ocean ridge basalt petrogenesis , 1997 .
[102] A. Cohen,et al. Separation of osmium from geological materials by solvent extraction for analysis by thermal ionisation mass spectrometry , 1996 .
[103] L. Reisberg,et al. Os isotopic systematics of the MORB mantle: results from altered abyssal peridotites , 1995 .
[104] P. Kelemen,et al. Extraction of mid-ocean-ridge basalt from the upwelling mantle by focused flow of melt in dunite channels , 1995, Nature.
[105] P. Kelemen,et al. Focused melt flow and localized deformation in the upper mantle: Juxtaposition of replacive dunite and ductile shear zones in the Josephine peridotite, SW Oregon , 1995 .
[106] M. Roy‐Barman,et al. 187Os186Os ratios of mid-ocean ridge basalts and abyssal peridotites , 1994 .
[107] S. Arai. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation , 1994 .
[108] Candace E Martin. Osmium isotopic characteristics of mantle-derived rocks , 1991 .
[109] G. Witt-Eickschen,et al. Solubility of Ca and Al in orthopyroxene from spinel peridotite: an improved version of an empirical geothermometer , 1991 .
[110] T. Köhler,et al. Geothermobarometry in Four-phase Lherzolites II. New Thermobarometers, and Practical Assessment of Existing Thermobarometers , 1990 .
[111] H. Dick,et al. Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites , 1990 .
[112] J. Girardeau,et al. Petrology and texture of the ultramafic rocks of the Xigaze ophiolite (Tibet): constraints for mantle structure beneath slow-spreading ridges , 1988 .
[113] H. O’Neill,et al. The Olivine—Orthopyroxene—Spinel Oxygen Geobarometer, the Nickel Precipitation Curve, and the Oxygen Fugacity of the Earth's Upper Mantle , 1987 .
[114] Donald L. Turcotte,et al. Implications of a two-component marble-cake mantle , 1986, Nature.
[115] H. Dick,et al. Chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas , 1984 .
[116] B. Dupré,et al. The Xigaze ophiolite (Tibet): a peculiar oceanic lithosphere , 1981, Nature.
[117] R. Arculus,et al. Silica-rich spinel harzburgite residues formed by fractional hybridization-melting of the intra-oceanic supra-subduction zone mantle: New evidence from TUBAF seamount peridotites , 2021 .
[118] Wu Fu. Yarlung Zangbo ophiolite: A critical updated view , 2014 .
[119] G. Ceuleneer,et al. The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both? , 2013 .
[120] P. Kelemen,et al. Composition and Genesis of Depleted Mantle Peridotites from the Wadi Tayin Massif, Oman Ophiolite; Major and Trace Element Geochemistry, and Os Isotope and PGE Systematics , 2010 .
[121] Li Yi-jun. Sm-Nd ages and Nd-Sr-Pb isotope signatures of the Xiugugabu ophiolite, southwestern Tibet , 2008 .
[122] P. Sylvester. Laser Ablation-ICP-MS in the Earth Sciences CURRENT PRACTICES AND OUTSTANDING ISSUES , 2008 .
[123] Wei Zhen-quan. SHRIMP ZIRCON DATING OF DIABASE IN THE XIUGUGABU OPHIOLITE IN TIBET AND ITS GEOLOGICAL IMPLICATIONS , 2006 .
[124] C. J. Stephens. HETEROGENEITY OF OCEANIC PERIDOTITE FROM THE WESTERN CANYON WALL AT MARK : RESULTS FROM SITE 920 1 , 2006 .
[125] M. Reid,et al. Quantitative modeling of trace element fractionation during incongruent dynamic melting , 2001 .
[126] M. Walter. Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere , 1998 .
[127] E. Bonatti,et al. Regional-scale melt-rock interaction in lherzolitic mantle in the Romanche Fracture Zone (Atlantic Ocean) , 1997 .
[128] John F. Casey. Comparison of major- and trace-element geochemistry of abyssal peridotites and mafic plutonic rocks with basalts from the MARK region of the Mid-Atlantic Ridge , 1997 .
[129] R. Berry,et al. High-pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle , 1994 .
[130] R. Berry,et al. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle , 1991 .
[131] M. Menzies,et al. Continental to Oceanic Mantle Transition—REE and Sr-Nd Isotopic Geochemistry of the Lanzo Lherzolite Massif , 1991 .
[132] W. McDonough,et al. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.