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A possible high Nb/Ta reservoir in the continental lithospheric mantle and consequences on the global Nb budget – Evidence from continental basalts from Central Germany

https://doi.org/10.1016/j.gca.2011.11.017
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Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a publisher retraction, withdrawal, or removal notice.

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The 125 checked references that resolve
resolves10.1127/0935-1221/2003/0015-0831
The influence of pressure, mineral composition and water on trace element partitioning between clinopyroxene, amphibole and basanitic melts
resolves10.1007/s00410-006-0085-4
Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour
resolves10.1016/j.tecto.2005.11.022
Global 1°×1° thermal model TC1 for the continental lithosphere: Implications for lithosphere secular evolution
resolves10.1130/0091-7613(1998)026<0359:PAOICO>2.3.CO;2
Pb and Os isotopic constraints on the composition and rheology of the lower crust
resolves10.1038/ngeo226
Subcontinental lithospheric mantle origin of high niobium/tantalum ratios in eclogites
resolves10.1016/S0009-2541(99)00173-4
Tracking the budget of Nb and Ta in the continental crust
resolves10.1007/s004100100288
Multistage evolution of the European lithospheric mantle: new evidence from Sardinian peridotite xenoliths
resolves10.1016/S0012-821X(97)00167-2
Evolution of LILE-enriched small melt fractions in the lithospheric mantle: a case study from the East African Rift
resolves10.1007/s00410-003-0452-3
The brevity of carbonatite sources in the mantle: evidence from Hf isotopes
resolves10.1016/S0012-821X(97)00040-X
The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system
resolves10.1007/s004100050278
Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sector-multiple collector ICP-MS
resolves10.1016/0016-7037(89)90140-3
Sr, Nd, and Pb isotopic character of Tertiary basalts from southwest Poland
resolves10.1016/S0009-2541(02)00143-2
Osmium isotopic systematics of melilitites from the Tertiary Central European Volcanic Province in SW Germany
resolves10.1016/0016-7037(95)00431-9
Distribution of niobium, tantalum, and other highly incompatible trace elements in the lithospheric mantle: The spinel paradox
resolves10.1093/petrology/44.3.569
Petrogenesis of Basanitic to Tholeiitic Volcanic Rocks from the Miocene Vogelsberg, Central Germany
resolves10.1016/0012-821X(83)90071-7
Pyroxene-carbonate reactions in the upper mantle
resolves10.1016/j.epsl.2004.11.001
Noble gas isotopes suggest deep mantle plume source of late Cenozoic mafic alkaline volcanism in Europe
resolves10.1029/2000GC000128
Olivine‐poor sources for mantle‐derived magmas: Os and Hf isotopic evidence from potassic magmas of the Colorado Plateau
resolves10.1016/j.chemgeo.2006.06.008
High-field-strength elements in carbonatitic rocks: Geochemistry, crystal chemistry and significance for constraining the sources of carbonatites
resolves10.1016/S0009-2541(97)00029-6
Contrasting old and young volcanism in Rurutu Island, Austral chain
resolves10.1016/S0012-821X(97)00176-3
Crust–mantle interaction in large igneous provinces: Implications from the Re–Os isotope systematics of the Columbia River flood basalts
resolves10.1016/S0012-821X(97)00089-7
Plume-lithosphere interactions in the ocean basins: constraints from the source mineralogy
resolves10.1016/j.epsl.2009.04.031
Osmium isotopes in Grande Comore lavas: A new extreme among a spectrum of EM-type mantle endmembers
resolves10.1016/j.epsl.2004.08.004
Deep global cycling of carbon constrained by the solidus of anhydrous, carbonated eclogite under upper mantle conditions
resolves10.1093/petrology/egm053
Partial Melting Experiments of Peridotite + CO2 at 3 GPa and Genesis of Alkalic Ocean Island Basalts
resolves10.1016/j.chemgeo.2009.02.004
Trace element partitioning between garnet lherzolite and carbonatite at 6.6 and 8.6 GPa with applications to the geochemistry of the mantle and of mantle-derived melts
resolves10.1016/0012-821X(81)90153-9
Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization
resolves10.1016/j.gca.2010.09.024
Geochemical constraints on depth of origin of oceanic carbonatites: The Cape Verde case
resolves10.1093/petrology/42.1.233
Formation and Modification of the Shallow Sub-continental Lithospheric Mantle: a Review of Geochemical Evidence from Ultramafic Xenolith Suites and Tectonically Emplaced Ultramafic Massifs of Western and Central Europe
resolves10.1016/0016-7037(92)90198-R
Zr/hf fractionation in intraplate basaltic rocks: Carbonate metasomatism in the mantle source
resolves10.1016/0031-9201(81)90046-7
Preliminary reference Earth model
resolves10.1038/359718a0
Evidence from Re–Os isotopes for plume–lithosphere mixing in Karoo flood basalt genesis
resolves10.1016/S0016-7037(99)00355-5
Rutile/melt partition coefficients for trace elements and an assessment of the influence of rutile on the trace element characteristics of subduction zone magmas
resolves10.1016/j.lithos.2009.03.020
The composition of near-solidus melts of peridotite in the presence of CO2 and H2O between 40 and 60 kbar
resolves10.1016/S0024-4937(99)00031-6
Erosion of lithospheric mantle beneath the East African Rift system: geochemical evidence from the Kivu volcanic province
resolves10.1126/science.1164446
Carbonatite Melts and Electrical Conductivity in the Asthenosphere
resolves10.1126/science.286.5446.1928
A Lower Mantle Source for Central European Volcanism
resolves10.1016/j.epsl.2008.12.035
Extreme high field strength element (HFSE) depletion and near-chondritic Nb/Ta ratios in Central Andean adakite-like lavas (~ 28°S, ~ 68°W)
resolves10.1016/0016-7037(87)90006-8
An experimental study of Nb and Ta partitioning between Ti-rich minerals and silicate liquids at high pressure and temperature
resolves10.1016/S0024-4937(00)00023-2
SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C
resolves10.1046/j.1365-246x.2001.01553.x
The upper mantle under Central Europe: indications for the Eifel plume
resolves10.1093/petrology/egg115
Petrogenesis of Tertiary Continental Intra-plate Lavas from the Westerwald Region, Germany
resolves10.1016/S0012-821X(97)00075-7
Radiogenic Os in primitive basalts from the northwestern U.S.A.: Implications for petrogenesis
resolves10.1016/0016-7037(90)90196-R
Metasomatically altered peridotite xenoliths from the hessian depression (Northwest Germany)
resolves10.1038/365221a0
Evidence for hotspot-related carbonatite metasomatism in the oceanic upper mantle
resolves10.1007/s004100050131
Pb-Sr-Nd isotopic compositions and trace element geochemistry of megacrysts and melilitites from the Tertiary Urach volcanic field: source composition of small volume melts under SW Germany
resolves10.1038/374034a0
Seismic and geochemical evidence for large-scale mantle upwelling beneath the eastern Atlantic and western and central Europe
resolves10.1007/s004100100308
Geochemistry of oceanic carbonatites compared with continental carbonatites: mantle recycling of oceanic crustal carbonate
resolves10.1016/0012-821X(88)90132-X
Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust
resolves10.1016/0009-2541(94)90128-7
Experimentally determined partitioning of high field strength- and selected transition elements between spinel and basaltic melt
resolves10.1016/0012-821X(93)90139-Z
Carbonated peridotite xenoliths from Spitsbergen: implications for trace element signature of mantle carbonate metasomatism
resolves10.1093/petrology/43.12.2219
Mechanisms and Sources of Mantle Metasomatism: Major and Trace Element Compositions of Peridotite Xenoliths from Spitsbergen in the Context of Numerical Modelling
resolves10.1016/j.epsl.2004.09.009
Trace element fractionation during fluid-induced eclogitization in a subducting slab: trace element and Lu–Hf–Sm–Nd isotope systematics
resolves10.1016/S0009-2541(02)00198-5
Temporal variation and carbonatite contamination in primitive ocean island volcanics from São Vicente, Cape Verde Islands
resolves10.1016/S0377-0273(98)00087-0
Major- and trace-element systematics and isotope geochemistry of Cenozoic mafic volcanic rocks from the Vogelsberg (central Germany)
resolves10.1016/S0377-0273(00)00156-6
The major- and trace-element and isotope (Sr, Nd, O) geochemistry of Cenozoic alkaline rift-type volcanic rocks from the Rhön area (central Germany): petrology, mantle source characteristics and implications for asthenosphere–lithosphere interactions
resolves10.1007/s00410-005-0029-4
Sources of primitive alkaline volcanic rocks from the Central European Volcanic Province (Rhön, Germany) inferred from Hf, Os and Pb isotopes
resolves10.1093/petrology/egl023
Petrogenesis of Tertiary Mafic Alkaline Magmas in the Hocheifel, Germany
resolves10.1016/j.gca.2011.02.017
Crustal contamination and mantle source characteristics in continental intra-plate volcanic rocks: Pb, Hf and Os isotopes from central European volcanic province basalts
resolves10.1016/S0009-2541(99)00218-1
Role of ‘hidden’ deeply subducted slabs in mantle depletion
resolves10.1016/0377-0273(81)90048-2
Carbonatitic volcanism in the Kaiserstuhl alkaline complex: Evidence for highly fluid carbonatitic melts at the earth's surface
resolves10.1016/S0012-821X(02)00861-0
3D shear-wave velocity structure of the Eifel plume, Germany
resolves10.1016/j.gca.2004.11.015
Partitioning of trace elements between rutile and silicate melts: Implications for subduction zones
resolves10.1016/j.epsl.2010.11.007
Deep melting of old subducted oceanic crust recorded by superchondritic Nb/Ta in modern island arc lavas
resolves10.1016/j.epsl.2008.07.002
Mobility of tungsten in subduction zones
resolves10.1093/petroj/40.4.629
The Stability of Hydrous Potassic Phases in Lherzolitic Mantle--an Experimental Study to 9.5 GPa in Simplified and Natural Bulk Compositions
resolves10.1016/0012-821X(90)90120-M
Excess argon and dating of Quaternary Eifel volcanism, IV. Common argon with high and lower-than-atmospheric 40Ar/36Ar ratios in phonolitic rocks, East Eifel, F.R.G.
resolves10.1016/j.gca.2008.02.018
Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton
resolves10.1007/BF00375175
Carbonatite in the tuffs of the West Eifel, Germany
resolves10.1016/j.gca.2009.08.006
Evidence for high-pressure core-mantle differentiation from the metal–silicate partitioning of lithophile and weakly-siderophile elements
resolves10.1093/petrology/42.6.1197
Osmium Isotopic Evidence for Crust–Mantle Interaction in the Genesis of Continental Intraplate Basalts from the Newer Volcanics Province, Southeastern Australia
resolves10.1016/S0031-9201(03)00149-3
Trace element partitioning on the Tinaquillo Lherzolite solidus at 1.5GPa
resolves10.1098/rsta.1991.0055
Partial melting of subducted oceanic crust and isolation of its residual eclogitic lithology
resolves10.1016/0009-2541(94)00140-4
The composition of the Earth
resolves10.1016/0012-821X(89)90167-2
Some remarks on the movement of small melt fractions in the mantle
resolves10.1016/j.lithos.2003.12.019
Carbonatite melt in oceanic upper mantle beneath the Kerguelen Archipelago
resolves10.1029/2001GC000183
Separation of high field strength elements (Nb, Ta, Zr, Hf) and Lu from rock samples for MC‐ICPMS measurements
resolves10.1126/science.1084662
Evolution of Planetary Cores and the Earth-Moon System from Nb/Ta Systematics
resolves10.1016/j.epsl.2004.05.030
Behaviour of high field strength elements in subduction zones: constraints from Kamchatka–Aleutian arc lavas
resolves10.1016/j.gca.2010.04.061
Deep mantle storage of the Earth’s missing niobium in late-stage residual melts from a magma ocean
resolves10.1016/0012-821X(83)90212-1
Phase relations of amphibole, amphibole-carbonate, and phlogopite-carbonate peridotite: petrologic constraints on the asthenosphere
resolves10.1016/0012-821X(95)00125-V
Stabilisation of Archaean lithospheric mantle: A ReOs isotope study of peridotite xenoliths from the Kaapvaal craton
resolves10.1016/j.epsl.2006.11.027
Nb/Ta and Zr/Hf in ocean island basalts — Implications for crust–mantle differentiation and the fate of Niobium
resolves10.1126/science.1156563
Metasomatized Lithosphere and the Origin of Alkaline Lavas
resolves10.1016/j.lithos.2010.07.007
Hf isotope compositions of Mediterranean lamproites: Mixing of melts from asthenosphere and crustally contaminated mantle lithosphere
resolves10.1016/S0012-821X(02)00836-1
Compaction in a mantle with a very small melt concentration: Implications for the generation of carbonatitic and carbonate-bearing high alkaline mafic melt impregnations
resolves10.1016/0012-821X(93)90236-3
Os isotope systematics in ocean island basalts
resolves10.1016/S0012-821X(01)00226-6
A mantle plume below the Eifel volcanic fields, Germany
resolves10.1016/j.epsl.2009.04.036
Petrogenesis of strongly alkaline primitive volcanic rocks at the propagating tip of the western branch of the East African Rift
resolves10.1016/0012-821X(93)90076-L
Carbonatite metasomatism in the northern Tanzanian mantle: Petrographic and geochemical characteristics
resolves10.1126/science.287.5451.278
Rutile-Bearing Refractory Eclogites: Missing Link Between Continents and Depleted Mantle
resolves10.1016/0012-821X(96)00070-2
The generation of mid-ocean ridge basalts from the Hf and Nd isotope perspective
resolves10.1029/2003GC000597
Composition of the depleted mantle
resolves10.1126/science.1061372
Calibration of the Lutetium-Hafnium Clock
resolves10.1016/0012-821X(94)90265-8
Cogenetic silica-rich and carbonate-rich melts trapped in mantle minerals in Kerguelen ultramafic xenoliths: Implications for metasomatism in the oceanic upper mantle
resolves10.1007/s00410-002-0372-7
Os isotopes in mantle xenoliths from the Eifel volcanic field and the Vogelsberg (Germany): age constraints on the lithospheric mantle
resolves10.1016/j.epsl.2004.08.010
The dependence of Nb and Ta rutile–melt partitioning on melt composition and Nb/Ta fractionation during subduction processes
resolves10.1016/j.gca.2008.10.028
HFSE systematics of rutile-bearing eclogites: New insights into subduction zone processes and implications for the earth’s HFSE budget
resolves10.1016/0016-7037(70)90009-8
Trace element fractionation during anatexis
resolves10.1146/annurev.earth.26.1.423
THE R<scp>e</scp>-O<scp>s</scp>ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY
resolves10.1093/petrology/42.5.999
Energy-Constrained Open-System Magmatic Processes I: General Model and Energy-Constrained Assimilation and Fractional Crystallization (EC-AFC) Formulation
resolves10.1016/0016-7037(80)90044-7
Geochemistry and mineralogy of two spinel peridotite suites from Dreiser Weiher, West Germany
resolves10.1016/0012-821X(86)90111-1
Trace element and Sr and Nd isotope geochemistry of peridotite xenoliths from the Eifel (West Germany) and their bearing on the evolution of the subcontinental lithosphere
resolves10.1029/2004GC000824
FOZO, HIMU, and the rest of the mantle zoo
resolves10.1016/j.epsl.2007.01.036
Craton reactivation on the Labrador Sea margins: 40Ar/39Ar age and Sr–Nd–Hf–Pb isotope constraints from alkaline and carbonatite intrusives
resolves10.1016/j.gca.2008.03.008
Between carbonatite and lamproite—Diamondiferous Torngat ultramafic lamprophyres formed by carbonate-fluxed melting of cratonic MARID-type metasomes
resolves10.1016/S0012-821X(00)00004-2
Nb and Ta incorporation and fractionation in titanian pargasite and kaersutite: crystal–chemical constraints and implications for natural systems
resolves10.1016/j.lithos.2004.04.007
Melt inclusions from the deep Slave lithosphere: implications for the origin and evolution of mantle-derived carbonatite and kimberlite
resolves10.2138/am-1999-5-617
Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt
resolves10.1038/35051064
The Earth's ‘missing’ niobium may be in the core
resolves10.1016/0016-7037(89)90240-8
Os, Sr, Nd, and Pb isotope systematics of southern African peridotite xenoliths: Implications for the chemical evolution of subcontinental mantle
resolves10.1007/s004100050534
Central European Cenozoic plume volcanism with OIB characteristics and indications of a lower mantle source
resolves10.1007/BF00310766
Cenozoic alkali basaltic magmas of western Germany and their products of differentiation
resolves10.1016/S0009-2541(02)00129-8
Determination of ultra-low Nb, Ta, Zr and Hf concentrations and the chondritic Zr/Hf and Nb/Ta ratios by isotope dilution analyses with multiple collector ICP-MS
resolves10.1016/S0012-821X(02)01059-2
Nb/Ta, Zr/Hf and REE in the depleted mantle: implications for the differentiation history of the crust–mantle system
resolves10.1093/petroj/40.2.279
Os Isotope Systematics in the Canary Islands and Madeira: Lithospheric Contamination and Mantle Plume Signatures
resolves10.1029/2005GC001005
Trace element composition of mantle end‐members: Implications for recycling of oceanic and upper and lower continental crust
resolves10.1016/j.epsl.2008.12.029
Continental geochemical signatures in dacites from Iceland and implications for models of early Archaean crust formation
resolves10.1016/0040-1951(92)90343-5
Mafic alkaline magmatism associated with the European Cenozoic rift system
resolves10.1007/BF00307280
Melilitites: partial melts of the thermal boundary layer?
resolves10.1016/0012-821X(86)90044-0
Sr, Nd, and Pb isotope geochemistry of Tertiary and Quaternary alkaline volcanics from West Germany
resolves10.1016/j.chemgeo.2005.01.014
Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis
resolves10.1016/0012-821X(91)90078-V
Evidence for carbonatite metasomatism in spinel peridotite xenoliths from western Victoria, Australia
resolves10.1093/petroj/39.11-12.1917
Carbonatite Metasomatism in the Southeastern Australian Lithosphere
resolves10.1007/s004100050114
Metasomatism in mantle xenoliths from Gees, West Eifel, Germany: evidence for the genesis of calc-alkaline glasses and metasomatic Ca-enrichment
The 16 references without a DOI — listed, not checked
no DOI — not checked10.1016/j.gca.2011.11.017_b0015
no DOI — not checkedHigh-precision Nb/Ta and Zr/Hf ratios in global MORB
no DOI — not checkedGeodynamic setting of the Hocheifel volcanism, western Germany
no DOI — not checkedNachweis eines Mantelplumes unter Frankreichs Zentralmassiv durch seismische Sondierung
no DOI — not checkedNiobium in planetary cores: consequences for the interpretation of terrestrial Nb systematics
no DOI — not checkedGeochemistry and petrogenesis of rift-related Tertiary alkaline rocks from the Rhön area (central Germany)
no DOI — not checkedHFSE residence and Nb/Ta ratios in metasomatised, rutile bearing mantle peridotites
no DOI — not checkedAlong-strike variation in the Aleutian Island Arc: genesis of high Mg# andesite and implications for continental crust
no DOI — not checkedK/Ar determinations and the correlation of Tertiary volcanic activity in Central Europe
no DOI — not checkedThe circum-mediterranean anorogenic Cenozoic igneous province
no DOI — not checkedStability of amphibole and phlogopite in metasomatized peridotite under water-saturated and water-undersaturated conditions
no DOI — not checkedRe–Os, Sm–Nd and Rb–Sr isotope evidence for thick Archaean lithospheric mantle beneath the Siberian craton modified by multi-stage metasomatism
no DOI — not checkedComposition of the continental crust
no DOI — not checkedChemical and isotopic systematics of oceanic basalts: implications for mantle compositions and processes
no DOI — not checkedIntra-plate magmatism related to hot fingers in the upper mantle: evidence from the tertiary–quaternary volcanic province of western and central Europe
no DOI — not checkedThermal and geochemical evolution of the shallow subcontinental lithospheric mantle beneath the Eifel: constraints from mantle xenoliths, a review
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