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 120 checked references that resolve
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
resolves10.1016/0098-3004(77)90007-3Petrological and geochemical mass-balance equations: an algorithm for least-square fitting and general error analysis
resolves10.1007/BF00373683Fluorine geochemistry of basaltic rocks from continental and oceanic regions and petrogenetic application
resolves10.1016/j.lithos.2009.03.029Potassic and ultrapotassic magmatism in the circum-Tyrrhenian region: Significance of carbonated pelitic vs. pelitic sediment recycling at destructive plate margins
resolves10.1007/s00410-010-0497-zAuPdFe ternary solution model and applications to understanding the fO2 of hydrous, high-pressure experiments
resolves10.1016/j.epsl.2012.05.003Fluorine in nominally fluorine-free mantle minerals: Experimental partitioning of F between olivine, orthopyroxene and silicate melts with implications for magmatic processes
resolves10.1063/1.1709908Local Compositional Changes in Alkali Silicate Glasses during Electron Microprobe Analysis
resolves10.1016/0743-9547(94)00040-LThe igneous provinciality in Taiwan: Consequence of continental rifting superimposed by Luzon and Ryukyu subduction systems
resolves10.1007/s007100200004Source contamination and mantle heterogeneity in the genesis of Italian potassic and ultrapotassic volcanic rocks: Sr-Nd-Pb isotope data from Roman Province and Southern Tuscany
resolves10.1093/petrology/egm053Partial Melting Experiments of Peridotite + CO2 at 3 GPa and Genesis of Alkalic Ocean Island Basalts
resolves10.1007/s00410-013-0907-0The effects of K2O on the compositions of near-solidus melts of garnet peridotite at 3 GPa and the origin of basalts from enriched mantle
resolves10.1016/j.epsl.2011.06.008The composition of the incipient partial melt of garnet peridotite at 3 GPa and the origin of OIB
resolves10.2138/am-1995-3-413Comparison of microanalytical methods for estimating H
<sub>2</sub>
O contents of silicic volcanic glasses
resolves10.1180/minmag.1996.060.399.01Fluorine in igneous rocks and minerals with emphasis on ultrapotassic mafic and ultramafic magmas and their mantle source regions
resolves10.1007/BF01161817Anhydrous partial melting of MORB pyrolite and other peridotite compositions at 10 kbar: Implications for the origin of primitive MORB glasses
resolves10.1093/petrology/42.12.2363Peridotite Melting at 1 GPa: Reversal Experiments on Partial Melt Compositions Produced by Peridotite-Basalt Sandwich Experiments
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
resolves10.1007/BF00963584The effect of fluorine on phase relationships in the system KAlSiO4-Mg2SiO4-SiO2 at 28 kbar and the solution mechanism of fluorine in silicate melts
resolves10.1007/BF00592935The role of fluorine and oxygen fugacity in the genesis of the ultrapotassic rocks
resolves10.1007/s00410-009-0407-4Alkali in phlogopite and amphibole and their effects on phase relations in metasomatized peridotites: a high-pressure study
resolves10.1007/s00410-013-0881-6Melting phase relations of a mica–clinopyroxenite from the Milk River area, southern Alberta, Canada
resolves10.1039/b801807nQuantitative analysis of silicate certified reference materials by LA-ICPMS with and without an internal standard
resolves10.1016/0012-821X(90)90169-XPhlogopite-clinopyroxenite nodules from high-K magmas, Roccamonfina Volcano, Italy: evidence for a low-pressure metasomatic origin
resolves10.1007/s00410-013-0899-9Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite
resolves10.1093/petrology/egl007Post-collisional, Potassic and Ultrapotassic Magmatism of the Northern Tibetan Plateau: Constraints on Characteristics of the Mantle Source, Geodynamic Setting and Uplift Mechanisms
resolves10.1029/97GL02956Partial melt compositions of carbonated peridotite at 3 GPa and role of CO<sub>2</sub> in alkali‐basalt magma generation
resolves10.1016/0012-821X(93)90077-MPartial melting of dry peridotites at high pressures: Determination of compositions of melts segregated from peridotite using aggregates of diamond
resolves10.1007/s00410-007-0213-9A modified iterative sandwich method for determination of near-solidus partial melt compositions. I. Theoretical considerations
resolves10.1016/j.gca.2007.07.014Tungsten and hafnium distribution in calcium–aluminum inclusions (CAIs) from Allende and Efremovka
resolves10.1039/c001391aMajor element analysis of natural silicates by laser ablation ICP-MS
resolves10.1007/BF00348950The oxidation state of subcontinental mantle: oxygen thermobarometry of mantle xenoliths from central Asia
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/BF00287116Potassic primary melts of vulsini (Roman Province): evidence from mineralogy and melt inclusions
resolves10.1029/96JB00988Melting of mantle peridotite at pressures approaching the spinel to garnet transition: Application to mid‐ocean ridge basalt petrogenesis
resolves10.1007/BF00307328The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states
resolves10.1029/GM095p0109Partial Melting of a Fertile Mantle Peridotite at High Pressures: An Experimental Study Using Aggregates of Diamond
resolves10.1016/0012-821X(67)90036-2Stability of phlogopite at high pressures and possible presence of phlogopite in the earth's upper mantle
resolves10.1016/j.epsl.2014.08.002Experimental derivation of nepheline syenite and phonolite liquids by partial melting of upper mantle peridotites
resolves10.1007/BF00374688Partial melting of a phlogopite-clinopyroxenite nodule from south-west Uganda: an experimental study bearing on the origin of highly potassic continental rift volcanics
resolves10.1029/2001GC000224An experimental investigation of the diffusive infiltration of alkalis into partially molten peridotite: Implications for mantle melting processes
resolves10.1007/BF00287113Mafic magma batches at Vesuvius: a glass inclusion approach to the modalities of feeding stratovolcanoes
resolves10.1093/petrology/egi083Melting of Amphibole-bearing Wehrlites: an Experimental Study on the Origin of Ultra-calcic Nepheline-normative Melts
resolves10.1007/s004100050017Phase relations and fractionation sequences in potassic magma series modelled in the system CaMgSi 2 O 6 -KAlSiO 4 -Mg 2 SiO 4 -SiO 2 -F 2 O −1 at 1 bar to 18 kbar
resolves10.1093/petrology/egl051Origin and Source Evolution of the Leucite Hills Lamproites: Evidence from Sr-Nd-Pb-O Isotopic Compositions
resolves10.2475/ajs.272.9.852The stability of phlogopite + enstatite at high pressures; a model for micas in the interior of the Earth
resolves10.2475/ajs.273.5.385Phase relationships of phlogopite in the system K 2 O-MgO-CaO-Al 2 O 3 -SiO 2 -H 2 O to 35 kilobars; a better model for micas in the interior of the Earth
resolves10.2138/am-2001-11-1209F-rich phlogopite stability in ultra-high-temperature metapelites from the Napier Complex, East Antarctica
resolves10.1016/0024-4937(92)90016-RIsotopic characteristics of potassic rocks: evidence for the involvement of subducted sediments in magma genesis
resolves10.1007/s004100050495Stability and chemical composition of pargasitic amphibole in MORB pyrolite under upper mantle conditions
resolves10.1016/j.jvolgeores.2010.06.014Heterogeneous mantle sources of potassium-rich magmas in central-southern Italy: Melt inclusion evidence from Roccamonfina and Ernici (Mid Latina Valley)
resolves10.1016/0012-8252(68)90147-5The bearing of phase equilibria studies in synthetic and natural systems on the origin and evolution of basic and ultrabasic rocks
resolves10.1007/s007100170012Geochemical similarities between the Vesuvius, Phlegraean Fields and Stromboli Volcanoes: petrogenetic, geodynamic and volcanological implications
resolves10.1093/petrology/egs008Ultrapotassic Mafic Rocks as Geochemical Proxies for Post-collisional Dynamics of Orogenic Lithospheric Mantle: the Case of Southwestern Anatolia, Turkey
resolves10.1007/s004100050145Thermobarometry of mafic igneous rocks based on clinopyroxene-liquid equilibria, 0-30 kbar
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(96)00246-4Phase relations of natural phlogopite with and without enstatite up to 8 GPa: implication for mantle metasomatism
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
resolves10.1016/j.epsl.2013.09.026Experimental melting of hydrous peridotite–pyroxenite mixed sources: Constraints on the genesis of silica-undersaturated magmas beneath volcanic arcs
resolves10.1029/GL017i001p00029Phlogopite and K‐amphibole in the upper mantle: Implication for magma genesis in subduction zones
resolves10.1180/002646198547774Stability of F-Ti-phlogopite in the system phlogopite–sillimanite–quartz: an experimental study of dehydration melting in H<sub>2</sub>O-saturated and undersaturated conditions
resolves10.1029/2011GC003942The effect of H<sub>2</sub>O on partial melting of garnet peridotite at 3.5 GPa
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
resolves10.1007/s007100200001Stability range and decomposition of potassic richterite and phlogopite end members at 5-15 GPa
resolves10.1093/petrology/egs074An Experimental Study on COH-bearing Peridotite up to 3·2 GPa and Implications for Crust–Mantle Recycling
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
resolves10.1007/s00410-010-0572-5Melt variability in percolated peridotite: an experimental study applied to reactive migration of tholeiitic basalt in the upper mantle
resolves10.1093/petrology/21.4.651Mineralogy, Petrology, and Geochemistry of an Ultrapotassic Basaltic Suite, Central Sierra Nevada, California, U.S.A.
resolves10.1007/BF00307759Phase relations in the phlogopite-apatite system at 20 kbar; implications for the role of fluorine in mantle melting
resolves10.1038/335343a0An experimental determination of primary carbonatite magma composition
resolves10.1093/petroj/39.1.29Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere
resolves10.1093/petrology/egh001Geochemical Constraints for the Genesis of Post-collisional Magmatism and the Geodynamic Evolution of the Northern Taiwan Region
resolves10.2475/ajs.280.5.385The origins of potassic magmas; 1, Melting relations in the systems KAlSiO 4 -Mg 2 SiO 4 -SiO 2 and KAlSiO 4 MgO-SiO 2 -CO 2 to 30 kilobars
resolves10.2475/ajs.280.5.421The origins of potassic magmas; 2, Stability of phlogopite in natural spinel lherzolite and in the system KAlSiO 4 -MgO-SiO 2 -H 2 O-CO 2 at high pressures and high temperatures
resolves10.1007/BF01132067The formation of mantle phlogopite in subduction zone hybridization
The 12 references without a DOI — listed, not checked
no DOI — not checkedEdgar AD, Arima M (1985) Fluorine and chlorine contents of phlogopites crystallized from ultrapotassic rock compositions in high pressure experiments; implication for halogen reservoirs in source regions. Am Mineral 70(5–6):529–536
no DOI — not checkedElkins-Tanton LT, Grove TL (2003) Evidence for deep melting of hydrous metasomatized mantle: pliocene high-potassium magmas from the Sierra Nevadas. J Geophys Res Solid Earth 108(B7):2350
no DOI — not checkedFlanagan FJ (1984) Three USGS mafic rock reference samples. W-2, DNC-1, and BIR-1. US Government Printing Office
no DOI — not checkedHall L (1999) The effect of water on mantle melting. PhD Thesis, University of Bristol, Bristol. 159
no DOI — not checkedMM (2000) Mantle solidus: Experimental constraints and the effects of peridotite composition. Geochemistry Geophysics Geosystems 1(10)
no DOI — not checkedO’Neill HSC (1987) Quartz-fayalite-iron and quartz-fayalite-magnetite equilibria and the free energy of formation of fayalite (Fe2SiO4) and magnetite (Fe3O4). Am Mineral 72(1–2):67–75
no DOI — not checkedPeterson JW, Chacko T, Kuehner SM (1991) The effects of fluorine on the vapor-absent melting of phlogopite + quartz: implications for deep-crustal processes. Am Mineral 76:470–476
no DOI — not checkedRieder M, Cavazzini G, D’Yakonov YS (1998) Nomenclature of the micas. Can Mineral 36:41–48
no DOI — not checkedThibault Y, Edgar AD, Lloyd FE (1992) Experimental investigation of melts from a carbonated phlogopite lherzolite: implications for metasomatism in the continental lithospheric mantle. Am Mineral 77:784–794
no DOI — not checkedVielzeuf D, Clemens JD (1992) The fluid-absent melting of phlogopite + quartz: experiments and models. Am Mineral 77:1206–1222
no DOI — not checkedWilson SA (1997) Basalt, Columbia River, BCR-2. United States Geological Survey Certificate of Analysis
no DOI — not checkedYoder HS, Kushiro I (1969) Melting of hydrous phase: phlogopite. Am J Sci 267:558–582
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