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 retraction,
withdrawal, or removal notice.
The 71 checked references that resolve
resolves10.1007/s00410-006-0104-5Experimental evidence of decompression melting during exhumation of subducted continental crust
resolves10.1007/BF00379451Heat capacity of minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2: representation, estimation, and high temperature extrapolation
resolves10.1016/0016-7037(96)00056-7Constraints on the origin of the oxidation state of mantle overlying subduction zones: An example from Simcoe, Washington, USA
resolves10.1046/j.1525-1314.2000.00250.xA general model for the intrusion and evolution of ‘mantle’ garnet peridotites in high‐pressure and ultra‐high‐pressure metamorphic terranes
resolves10.2475/ajs.290.10.1093Oxygen thermobarometry of abyssal spinel peridotites; the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantle
resolves10.1007/BF01575622Oxidation state of mantle xenoliths from British Columbia, Canada
resolves10.1007/BF00306429The redox states of basic and silicic magmas: a reflection of their source regions?
resolves10.1127/0935-1221/2005/0017-0031On multi-phase mineral inclusions associated with microdiamond formation in mantle-derived peridotite lens at Bardane on Fjortoft, west Norway
resolves10.2475/ajs.290.6.666Multivariable phase diagrams; an algorithm based on generalized thermodynamics
resolves10.1016/0012-821X(73)90176-3Experimental melting studies on a model upper mantle composition at high pressure under water-saturated and water-undersaturated conditions
resolves10.2138/am.2007.2390The iron oxidation state of garnet by electron microprobe: Its determination with the flank method combined with major-element analysis
resolves10.1127/ejm/6/3/0407The determination of the oxidation state of iron by the electron microprobe
resolves10.2138/am-1996-11-1215Thermodynamics of order-disorder in minerals; II, Symmetric formalism applied to solid solutions
resolves10.1016/j.epsl.2005.06.018The water–basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400 °C
resolves10.1093/petrology/egi056Similar V/Sc Systematics in MORB and Arc Basalts: Implications for the Oxygen Fugacities of their Mantle Source Regions
resolves10.1016/j.epsl.2006.07.017Polyphase inclusions in garnet–orthopyroxenite (Dabie Shan, China) as monitors for metasomatism and fluid-related trace element transfer in subduction zone peridotite
resolves10.1007/s004100100244Oxidation during metasomatism in ultramafic xenoliths from the Wesselton kimberlite, South Africa: implications for the survival of diamond
resolves10.1016/S0264-3707(99)00029-0P–T evolution of ‘crustal’ garnet peridotites and included pyroxenites from Nonsberg area (upper Austroalpine), NE Italy: from the wedge to the slab
resolves10.1093/petrology/28.3.599Transformation of Spinel Lherzolite to Garnet Lherzolite in Ultramafic Lenses of the Austridic Crystalline Complex, Northern Italy
resolves10.1093/petrology/28.6.1169The Olivine--Orthopyroxene--Spinel Oxygen Geobarometer, the Nickel Precipitation Curve, and the Oxygen Fugacity of the Earth's Upper Mantle
resolves10.2138/am-1996-3-417Parameterization of energy and interactions in garnets; end-member properties
resolves10.1093/petrology/42.1.207Records of Crustal Metasomatism in the Garnet Peridotites of the Ulten Zone (Upper Austroalpine, Eastern Alps)
resolves10.1007/s00410-006-0064-9Melt- versus fluid-induced metasomatism in spinel to garnet wedge peridotites (Ulten Zone, Eastern Italian Alps): clues from trace element and Li abundances
resolves10.1130/G24056A.1Majoritic garnets monitor deep subduction fluid flow and mantle dynamics
resolves10.1016/S0016-7037(98)00105-7Redox state of Earth’s upper mantle peridotites under the ancient cratons and its connection with diamond genesis
resolves10.1130/0091-7613(2002)030<0959:MIAMGW>2.0.CO;2Microdiamonds in a megacrystic garnet websterite pod from Bardane on the island of Fjørtoft, western Norway: Evidence for diamond formation in mantle rocks during deep continental subduction
resolves10.1046/j.0263-4929.2000.00303.xCalculation of partial melting equilibria in the system Na<sub>2</sub>O–CaO–K<sub>2</sub>O–FeO–MgO–Al<sub>2</sub>O<sub>3</sub>–SiO<sub>2</sub>–H<sub>2</sub>O (NCKFMASH)
resolves10.1016/0016-7037(89)90062-8Upper mantle oxidation state: Ferric iron contents of Iherzolite spinels by 57Fe Mössbauer spectroscopy and resultant oxygen fugacities
resolves10.1029/1999JB900206Equations of state for Fe<sub>3</sub><sup>2+</sup>Fe<sub>2</sub><sup>3+</sup>Si<sub>3</sub>O<sub>12</sub>“skiagite” garnet and Fe<sub>2</sub>SiO<sub>4</sub>‐Fe<sub>3</sub>O<sub>4</sub>spinel solid solutions
resolves10.1127/ejm/7/1/0187Almandine-rich garnet from near Collobrières, southern France, and its petrological significance
resolves10.1016/S0024-4937(03)00106-3Titanian clinohumite–garnet–pyroxene rock from the Su-Lu UHP metamorphic terrane, China: chemical evolution and tectonic implications
resolves10.1111/j.1525-1314.2006.00688.xPetrogenesis of the garnet peridotite and garnet‐free peridotite of the Zhimafang ultramafic body in the Sulu ultrahigh‐pressure metamorphic belt, eastern China
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