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 62 checked references that resolve
resolves10.1007/BF00371074Quartz diorites derived by partial melting of eclogite or amphibolite at mantle depths
resolves10.1016/S0301-9268(01)00216-9Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions
resolves10.1016/j.gca.2009.12.011Trace-element mobilization during Ca-metasomatism along a major fluid conduit: Eclogitization of blueschist as a consequence of fluid–rock interaction
resolves10.1016/j.epsl.2007.11.033The role of TiO2 phases during melting of subduction-modified crust: Implications for deep mantle melting
resolves10.2475/ajs.290.6.666Multivariable phase diagrams; an algorithm based on generalized thermodynamics
resolves10.1093/petrology/egp034Trace Element Partitioning in HP–LT Metamorphic Assemblages during Subduction-related Metamorphism, Ile de Groix, France: a Detailed LA-ICPMS Study
resolves10.1038/nature00799Growth of early continental crust controlled by melting of amphibolite in subduction zones
resolves10.1016/j.epsl.2008.06.002A model for rutile saturation in silicate melts with applications to eclogite partial melting in subduction zones and mantle plumes
resolves10.1007/s004100100275Primary fluids entrapped at blueschist to eclogite transition: evidence from the Tianshan meta-subduction complex in northwestern China
resolves10.1016/S0024-4937(02)00153-6Formation of HP–LT rocks and their tectonic implications in the western Tianshan Orogen, NW China: geochemical and age constraints
resolves10.1046/j.1525-1314.1999.00219.x<i>P–T</i> path of high‐pressure/low‐temperature rocks and tectonic implications in the western Tianshan Mountains, NW China
resolves10.1016/0009-2541(86)90131-2Rare-earth element partitioning between sphene and coexisting silicate liquid at high pressure and temperature
resolves10.1016/0012-821X(88)90132-XChemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust
resolves10.1016/j.lithos.2007.09.005Trace-element mobilization in slabs due to non steady-state fluid–rock interaction: Constraints from an eclogite-facies transport vein in blueschist (Tianshan, China)
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
resolves10.1046/j.1525-1314.2002.00347.x<i>P–T</i> evolution of glaucophane–omphacite bearing HP–LT rocks in the western Tianshan Orogen, NW China:new evidence for ‘Alpine‐type’ tectonics
resolves10.1016/j.gca.2004.11.015Partitioning of trace elements between rutile and silicate melts: Implications for subduction zones
resolves10.1093/petrology/egn001Trace Element Partitioning and Accessory Phase Saturation during H2O-Saturated Melting of Basalt with Implications for Subduction Zone Chemical Fluxes
resolves10.2138/am.2008.2800Coesite inclusions in garnet from eclogitic rocks in western Tianshan, northwest China: Convincing proof of UHP metamorphism
resolves10.1111/j.1525-1314.2009.00845.xPetrology of coesite‐bearing eclogite from Habutengsu Valley, western Tianshan, NW China and its tectonometamorphic implication
resolves10.1007/BF00687196The Reaction Titanite+Kyanite=Anorthite+Rutile and Titanite-Rutile Barometry in Eclogites
resolves10.1126/science.286.5441.937Seismic Consequences of Warm Versus Cool Subduction Metamorphism: Examples from Southwest and Northeast Japan
resolves10.1093/petrology/egg074Anhydrous Partial Melting Experiments on MORB-like Eclogite: Phase Relations, Phase Compositions and Mineral-Melt Partitioning of Major Elements at 2-3 GPa
resolves10.1029/2003GC000638Experimental determination of trace element partitioning between garnet and silica‐rich liquid during anhydrous partial melting of MORB‐like eclogite
resolves10.1016/j.epsl.2006.11.027Nb/Ta and Zr/Hf in ocean island basalts — Implications for crust–mantle differentiation and the fate of Niobium
resolves10.1016/j.gca.2004.06.037Effect of melt composition on the partitioning of trace elements between titanite and silicate melt
resolves10.1016/j.epsl.2004.08.010The dependence of Nb and Ta rutile–melt partitioning on melt composition and Nb/Ta fractionation during subduction processes
resolves10.1016/j.gca.2008.10.028HFSE systematics of rutile-bearing eclogites: New insights into subduction zone processes and implications for the earth’s HFSE budget
resolves10.1007/BF00307273Dehydration melting of a basaltic composition amphibolite at 1.5 and 2.0 GPa: implications for the origin of adakites
resolves10.1093/petrology/egi017Using In Situ Trace-Element Determinations to Monitor Partial-Melting Processes in Metabasites
resolves10.1127/0935-1221/2010/0022-2040UPb zircon geochronology of Tianshan eclogites in NW China: implication for the collision between the Yili and Tarim blocks of the southwestern Altaids
resolves10.1016/S0009-2541(02)00151-1Trace-element incorporation in titanite: constraints from experimentally determined solid/liquid partition coefficients
resolves10.1007/s004100100309Thermodynamic properties and stability of AlF-bearing titanite CaTiOSiO4–CaAlFSiO4
resolves10.1016/j.chemgeo.2008.03.010The current status of titanite–rutile thermobarometry in ultrahigh-pressure metamorphic rocks: The influence of titanite activity models on phase equilibrium calculations
resolves10.1093/petrology/43.10.1787The Substitution of Al and F in Titanite at High Pressure and Temperature: Experimental Constraints on Phase Relations and Solid Solution Properties
resolves10.1016/j.chemgeo.2008.06.037Blueschist-facies rehydration of eclogites (Tian Shan, NW-China): Implications for fluid–rock interaction in the subduction channel
resolves10.1016/j.chemgeo.2006.08.013Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area, northern Tianshan Range (western China): Implications for Phanerozoic crustal growth in the Central Asia orogenic belt
resolves10.1046/j.1525-1314.2003.00435.xEclogites from the south Tianshan, NW China: petrological characteristic and calculated mineral equilibria in the Na<sub>2</sub>O–CaO–FeO–MgO–Al<sub>2</sub>O<sub>3</sub>–SiO<sub>2</sub>–H<sub>2</sub>O system
resolves10.1130/G22711A.1Trace element evidence for growth of early continental crust by melting of rutile-bearing hydrous eclogite
resolves10.1016/j.chemgeo.2005.01.014Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis
resolves10.2138/am.2009.3158Experimental constraints on rutile saturation during partial melting of metabasalt at the amphibolite to eclogite transition, with applications to TTG genesis
The 5 references without a DOI — listed, not checked
no DOI — not checkedBernau R, Franz G (1987) Crystal chemistry and genesis of Nb-, V-, and Al-rich metamorphic titanite from Egypt and Greece. Can Mineral 25:695–705
no DOI — not checkedConnolly JAD, Podladchikov YY (2007) Decompaction weakening and channeling instability in ductile porous media: Implications for asthenospheric melt segregation. J Geophys Res 112:1–15
no DOI — not checkedHoffmann JE et al (2009) The origin of TTGs inferred from high-precision HFSE measurements. Geochim Cosmochim Acta 73:A540
no DOI — not checkedKing RL, Bebout GE, Kobayashi K, Nakamura E, van der Klauw SNGC (2004) Ultrahigh-pressure metabasaltic garnets as probes into deep subduction zone chemical cycling. Geochem Geophys Geosyst 5:Q12J14. doi: 10.1029/2004GC000746
no DOI — not checkedPaul BJ, Cerny P, Chapman R (1981) Niobian titanite from the Huron Claim Pegmatite, southeastern Manitoba. Can Mineral 19:549–552
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