Reference health
Fractionation of Nb and Ta by biotite and phengite: Implications for the “missing Nb paradox”
32/32 checkable references clean · checked 2026-07-14
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.
The 32 checked references that resolve
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Mechanisms of Crustal Anatexis: a Geochemical Study of Partially Melted Metapelitic Enclaves and Host Dacite, SE Spain
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
resolves10.1038/ngeo226
Subcontinental lithospheric mantle origin of high niobium/tantalum ratios in eclogites
resolves10.1016/S0016-7037(98)00292-0
Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy
resolves10.1016/0016-7037(94)90501-0
Mineral/matrix partition coefficients for orthopyroxene, plagioclase, and olivine in basaltic to andesitic systems: A combined analytical and experimental study
resolves10.1016/S0012-821X(97)00195-7
The composition of peridotites and their minerals: a laser-ablation ICP–MS study
resolves10.1016/0009-2541(94)90131-7
Application of proton-microprobe data to trace-element partitioning in volcanic rocks
resolves10.1016/j.gca.2010.02.020
High-precision high field strength element partitioning between garnet, amphibole and alkaline melt from Kakanui, New Zealand
resolves10.1016/j.chemgeo.2009.05.018
Accessory phase control on the trace element signature of sediment melts in subduction zones
resolves10.1016/j.gca.2011.04.027
Mechanisms of Archean crust formation inferred from high-precision HFSE systematics in TTGs
resolves10.1111/j.1945-5100.2000.tb01771.x
Niobium and tantalum in carbonaceous chondrites: Constraints on the solar system and primitive mantle niobium/tantalum, zirconium/niobium, and niobium/uranium ratio
resolves10.1111/j.1751-908X.2011.00120.x
Determination of Reference Values for NIST SRM 610–617 Glasses Following ISO Guidelines
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.chemgeo.2008.07.023
Nb and Zr behavior in rutile during high-grade metamorphism and retrogression: An example from the Ivrea–Verbano Zone
resolves10.1126/science.1084662
Evolution of Planetary Cores and the Earth-Moon System from Nb/Ta Systematics
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/S0009-2541(97)00150-2
The chemical composition of subducting sediment and its consequences for the crust and mantle
resolves10.1016/j.gca.2004.06.037
Effect of melt composition on the partitioning of trace elements between titanite and silicate melt
resolves10.1029/95RG01302
Nature and composition of the continental crust: A lower crustal perspective
resolves10.1126/science.287.5451.278
Rutile-Bearing Refractory Eclogites: Missing Link Between Continents and Depleted 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/S0016-7037(98)00101-X
Mineral-aqueous fluid partitioning of trace elements at 900–1200°C and 3.0–5.7 GPa: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism
resolves10.1016/j.chemgeo.2012.01.007
Experimental study of monazite/melt partitioning with implications for the REE, Th and U geochemistry of crustal rocks
resolves10.1130/0091-7613(1996)024<0587:FAMREI>2.3.CO;2
Fluid- and melt-related enrichment in the subarc mantle: Evidence from Nb/Ta variations in island-arc basalts
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.gca.2010.06.039
Partitioning of Nb and Ta between rutile and felsic melt and the fractionation of Nb/Ta during partial melting of hydrous metabasalt
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