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 109 checked references that resolve
resolves10.1127/0935-1221/2003/0015-0831The influence of pressure, mineral composition and water on trace element partitioning between clinopyroxene, amphibole and basanitic melts
resolves10.1007/s00410-006-0085-4Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour
resolves10.1016/0009-2541(93)90060-VProton microprobe determined partitioning of Rb, Sr, Ba, Y, Zr, Nb and Ta between experimentally produced amphiboles and silicate melts with variable F content
resolves10.1007/s00410-006-0168-2Laser Ablation ICPMS study of trace element partitioning between plagioclase and basaltic melts: an experimental approach
resolves10.1016/0098-3004(77)90007-3Petrological and geochemical mass-balance equations: an algorithm for least-square fitting and general error analysis
resolves10.1016/0009-2541(94)90121-XSystematics and energetics of trace-element partitioning between olivine and silicate melts: Implications for the nature of mineral/melt partitioning
resolves10.1016/0016-7037(95)00416-5Thermodynamics of rare earth element partitioning between clinopyroxene and melt in the system CaO-MgO-Al2O3-SiO2
resolves10.1038/372452a0Prediction of crystal–melt partition coefficients from elastic moduli
resolves10.1007/s004100050580Distinct site preferences for heavy and light REE in amphibole and the prediction of Amph/L D REE
resolves10.1016/0012-821X(95)00139-4Experimental determination of trace-element partitioning between pargasite and a synthetic hydrous andesitic melt
resolves10.2138/rmg.2002.46.01Mica Crystal Chemistry and the Influence of Pressure, Temperature, and Solid Solution on Atomistic Models
resolves10.1016/0743-9547(94)00040-LThe igneous provinciality in Taiwan: Consequence of continental rifting superimposed by Luzon and Ryukyu subduction systems
resolves10.1007/s004100000181Experimental investigation of large-ion-lithophile-element-, high-field-strength-element- and rare-earth-element-partitioning between calcic amphibole and basaltic melt: the effects of pressure and oxygen fugacity
resolves10.1016/j.epsl.2011.06.008The composition of the incipient partial melt of garnet peridotite at 3 GPa and the origin of OIB
resolves10.1016/j.chemgeo.2008.08.013Micro-Raman determination of iron redox state in dry natural glasses: Application to peralkaline rhyolites and basalts
resolves10.1144/GSL.SP.1986.024.01.28Granulitic xenoliths from the French Massif Central—petrology, Sr and Nd isotope systematics and model age estimates
resolves10.1016/j.gca.2020.03.037Experimental determinations of trace element partitioning between plagioclase, pigeonite, olivine, and lunar basaltic melts and an fO2 dependent model for plagioclase-melt Eu partitioning
resolves10.1016/j.chemgeo.2020.119967Effect of fO2 on Eu partitioning between clinopyroxene, orthopyroxene and basaltic melt: Development of a Eu3+/Eu2+ oxybarometer
resolves10.1093/petroj/40.8.1301Pliocene Potassic Magmas from the Kings River Region, Sierra Nevada, California: Evidence for Melting of a Subduction-Modified Mantle
resolves10.1016/0024-4937(92)90006-KPetrological characterization of the source components of potassic magmas: geochemical and experimental constraints
resolves10.3390/min10010041Two-Stage Origin of K-Enrichment in Ultrapotassic Magmatism Simulated by Melting of Experimentally Metasomatized Mantle
resolves10.1007/s00410-008-0346-5Trace element partitioning between orthopyroxene and anhydrous silicate melt on the lherzolite solidus from 1.1 to 3.2 GPa and 1,230 to 1,535°C in the model system Na2O–CaO–MgO–Al2O3–SiO2
resolves10.1039/b801807nQuantitative analysis of silicate certified reference materials by LA-ICPMS with and without an internal standard
resolves10.1016/S0024-4937(00)00023-2SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C
resolves10.1016/0024-4937(90)90018-VExperimental study of barium partitioning between phlogopite and silicate liquid at upper-mantle pressure and temperature
resolves10.1007/s00410-013-0860-yPost-collisional, K-rich mafic magmatism in south Tibet: constraints on Indian slab-to-wedge transport processes and plateau uplift
resolves10.1093/petroj/40.2.297Calculation of Peridotite Partial Melting from Thermodynamic Models of Minerals and Melts. II. Isobaric Variations in Melts near the Solidus and owing to Variable Source Composition
resolves10.1016/0012-821X(88)90132-XChemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust
resolves10.2138/am.2006.1909Effect of melt structure on trace-element partitioning between clinopyroxene and silicic, alkaline, aluminous melts
resolves10.1039/c001391aMajor element analysis of natural silicates by laser ablation ICP-MS
resolves10.1016/j.gca.2007.07.014Tungsten and hafnium distribution in calcium–aluminum inclusions (CAIs) from Allende and Efremovka
resolves10.2138/am-1995-11-1213An experimental study of element partitioning among biotite, muscovite, and coexisting peraluminous silicic melt at 200 MPa (H
<sub>2</sub>
O)
resolves10.1093/petrology/egl013Interpretation of Whole-rock Geochemical Data in Igneous Geochemistry: Introducing Geochemical Data Toolkit (GCDkit)
resolves10.1007/s00531-020-01872-2Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Třebíč Pluton, the largest durbachitic body in the Bohemian Massif
resolves10.2138/am.2005.1663Piston-cylinder experiments on H2O undersaturated Fe-bearing systems: An experimental setup approaching fO2 conditions of natural calc-alkaline magmas
resolves10.1007/s00410-009-0435-0Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melt: substitution mechanisms and the effect of iron
resolves10.1016/j.chemgeo.2011.02.007Experimental study of trace element partitioning between lunar orthopyroxene and anhydrous silicate melt: Effects of lithium and iron
resolves10.1016/S0009-2541(97)00019-3Partitioning of high field-strength and rare-earth elements between amphibole and quartz-dioritic to tonalitic melts: an experimental study
resolves10.1007/BF00307328The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states
resolves10.1007/s00410-003-0509-3A new experimental technique for extracting liquids from peridotite at very low degrees of melting: application to partial melting of depleted peridotite
resolves10.1007/s00531-016-1434-9Protracted, coeval crust and mantle melting during Variscan late-orogenic evolution: U–Pb dating in the eastern French Massif Central
resolves10.1016/j.gca.2014.03.031Postcollisional potassic and ultrapotassic rocks in southern Tibet: Mantle and crustal origins in response to India–Asia collision and convergence
resolves10.1007/s00410-015-1139-2Partial melting of fertile peridotite fluxed by hydrous rhyolitic melt at 2–3 GPa: implications for mantle wedge hybridization by sediment melt and generation of ultrapotassic magmas in convergent margins
resolves10.1093/petrology/egi083Melting of Amphibole-bearing Wehrlites: an Experimental Study on the Origin of Ultra-calcic Nepheline-normative Melts
resolves10.1016/j.gca.2008.09.030Influence of glass polymerisation and oxidation on micro-Raman water analysis in alumino-silicate glasses
resolves10.1016/0024-4937(92)90016-RIsotopic characteristics of potassic rocks: evidence for the involvement of subducted sediments in magma genesis
resolves10.1093/petrology/egs008Ultrapotassic Mafic Rocks as Geochemical Proxies for Post-collisional Dynamics of Orogenic Lithospheric Mantle: the Case of Southwestern Anatolia, Turkey
resolves10.1038/35065583Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust
resolves10.1007/BF00378265The geochemistry of potassic lavas from Vulsini, central Italy and implications for mantle enrichment processes beneath the Roman region
resolves10.1016/S0012-821X(04)00048-2The relationship between potassic, calc-alkaline and Na-alkaline magmatism in South Italy volcanoes: A melt inclusion approach
resolves10.1007/BF01132066Phase relationships in the system KAlSiO4-Mg2SiO4-SiO2-H2O as a model for hybridization between hydrous siliceous melts and peridotite
resolves10.2138/am-2017-6110Parameterized lattice strain models for REE partitioning between amphibole and silicate melt
resolves10.1007/s00410-009-0411-8Basanite–nephelinite suite from early Kilauea: carbonated melts of phlogopite–garnet peridotite at Hawaii’s leading magmatic edge
resolves10.1016/j.epsl.2013.09.026Experimental melting of hydrous peridotite–pyroxenite mixed sources: Constraints on the genesis of silica-undersaturated magmas beneath volcanic arcs
resolves10.1016/j.chemgeo.2014.02.014An assessment of subsolidus re-equilibration on REE distribution among mantle minerals olivine, orthopyroxene, clinopyroxene, and garnet in peridotites
resolves10.1016/j.gca.2013.05.036Distribution of REE and HFSE between low-Ca pyroxene and lunar picritic melts around multiple saturation points
resolves10.1007/s00410-011-0700-xDistribution of REE between clinopyroxene and basaltic melt along a mantle adiabat: effects of major element composition, water, and temperature
resolves10.1016/j.chemgeo.2013.08.045The importance of crystal chemistry on REE partitioning between mantle minerals (garnet, clinopyroxene, orthopyroxene, and olivine) and basaltic melts
resolves10.1016/0016-7037(95)00270-ASelected trace and minor element partitioning between peridotite minerals and carbonatite melts at 18–46 kb pressure
resolves10.1029/2011GC003942The effect of H<sub>2</sub>O on partial melting of garnet peridotite at 3.5 GPa
resolves10.1029/2000GC000064Partitioning of rare earth elements, Y, Th, U, and Pb between pargasite, kaersutite, and basanite to trachyte melts: Implications for percolated and veined mantle
resolves10.1007/s00410-004-0629-4The thermodynamics of iron and magnesium partitioning between olivine and liquid: criteria for assessing and predicting equilibrium in natural and experimental systems
resolves10.1093/petrology/37.1.45Post-collision, Shoshonitic Volcanism on the Tibetan Plateau: Implications for Convective Thinning of the Lithosphere and the Source of Ocean Island Basalts
resolves10.1093/petrology/21.4.651Mineralogy, Petrology, and Geochemistry of an Ultrapotassic Basaltic Suite, Central Sierra Nevada, California, U.S.A.
resolves10.1016/S0016-7037(00)00336-7Atomistic simulation of trace element incorporation into garnets—comparison with experimental garnet-melt partitioning data
resolves10.1016/S0024-4937(00)00024-4Effect of Fe2+ on garnet–melt trace element partitioning: experiments in FCMAS and quantification of crystal-chemical controls in natural systems
resolves10.1093/petrology/egg094Nature of the Source Regions for Post-collisional, Potassic Magmatism in Southern and Northern Tibet from Geochemical Variations and Inverse Trace Element Modelling
resolves10.1007/s004100050330A predictive model for rare earth element partitioning between clinopyroxene and anhydrous silicate melt
resolves10.1007/s00410-012-0737-5A parameterized model for REE distribution between low-Ca pyroxene and basaltic melts with applications to REE partitioning in low-Ca pyroxene along a mantle adiabat and during pyroxenite-derived melt and peridotite interaction
resolves10.1007/s004100050472The Finero phlogopite-peridotite massif: an example of subduction-related metasomatism
resolves10.2138/am-1999-5-617Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt
The 11 references without a DOI — listed, not checked
no DOI — not checked10.1016/j.gca.2022.04.011_b0145
no DOI — not checkedUltrapotassic plutonic rocks of the durbachite series in the Bohemian Massif: Petrology, geochemistry and petrogenetic interpretation
no DOI — not checkedProgressive melting of a metasedimentary sequence: The Saint-Malo Migmatitic Complex, France
no DOI — not checkedComposition of low-degree hydrous melts of fertile spinel-or garnet-bearing lherzolite
no DOI — not checkedQuartz-fayalite-iron and quartz-fayalite-magnetite equilibria and the free energy of formation of fayalite (Fe2SiO4) and magnetite (Fe3O4)
no DOI — not checkedRaman and fluorescence
no DOI — not checkedTrace element characteristics of lavas from destructive plate boundaries
no DOI — not checkedVolcanic rocks of the 1985 tibet geotraverse: Lhasa to Golmud
no DOI — not checkedSabatier H. (1991) Vaugnerites: special lamprophyre derived mafic enclaves in some Hercynian granites from Western and Central Europe. In Enclaves and Granite Petrology. pp. 63–81.
no DOI — not checkedWilson S. A. (1997) Basalt, Columbia River, BCR-2. United States Geological Survey Certificate of Analysis.
no DOI — not checkedProton microprobe determined trace element partition coefficients between pargasite, augite and silicate or carbonatitic melts
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