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 59 checked references that resolve
resolves10.1038/310575a0Empirical approach to estimating the composition of the continental crust
resolves10.1016/j.epsl.2016.01.032Role of arc magmatism and lower crustal foundering in controlling elevation history of the Nevadaplano and Colorado Plateau: A case study of pyroxenitic lower crust from central Arizona, USA
resolves10.1016/j.epsl.2017.04.025Effects of crustal thickness on magmatic differentiation in subduction zone volcanism: A global study
resolves10.1144/GSL.SP.1986.024.01.17Geochemical constraints on the origin of Archaean tonalitic-trondhjemitic rocks and implications for lower crustal composition
resolves10.1007/s00410-008-0351-8Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids
resolves10.1007/BF00373770Crystallization of calc-alkaline andesite under controlled high-pressure hydrous conditions
resolves10.1126/sciadv.aar4444The redox “filter” beneath magmatic orogens and the formation of continental crust
resolves10.1038/srep08115Crustal thickness control on Sr/Y signatures of recent arc magmas: an Earth scale perspective
resolves10.1016/j.gca.2010.02.020High-precision high field strength element partitioning between garnet, amphibole and alkaline melt from Kakanui, New Zealand
resolves10.1007/s00410-005-0056-1The development and refinement of continental arcs by primary basaltic magmatism, garnet pyroxenite accumulation, basaltic recharge and delamination: insights from the Sierra Nevada, California
resolves10.1038/nature12758Foundering of lower island-arc crust as an explanation for the origin of the continental Moho
resolves10.1016/0016-7037(87)90006-8An experimental study of Nb and Ta partitioning between Ti-rich minerals and silicate liquids at high pressure and temperature
resolves10.1016/0016-7037(93)90611-YDetermination of partition coefficients for trace elements in high pressure-temperature experimental run products by laser ablation microprobe-inductively coupled plasma-mass spectrometry (LAM-ICP-MS)
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.chemgeo.2005.01.014Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis
resolves10.1016/j.epsl.2007.11.033The role of TiO2 phases during melting of subduction-modified crust: Implications for deep mantle melting
resolves10.1016/j.gca.2010.06.039Partitioning of Nb and Ta between rutile and felsic melt and the fractionation of Nb/Ta during partial melting of hydrous metabasalt
resolves10.1016/j.epsl.2007.04.020Rutile saturation in hydrous siliceous melts and its bearing on Ti-thermometry of quartz and zircon
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
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
resolves10.1029/2001JB000643Constraints on the bulk composition and root foundering rates of continental arcs: A California arc perspective
resolves10.1016/S0012-821X(98)00021-1Crustal recycling beneath continental arcs: silica-rich glass inclusions in ultramafic xenoliths from the Sierra Nevada, California
resolves10.1029/2002TC001374Production and loss of high‐density batholithic root, southern Sierra Nevada, California
resolves10.1093/petrology/15.1.1Geochemical and High Pressure Experimental Studies of Garnet Pyroxenite and Pyroxene Granulite Xenoliths from the Delegate Basaltic Pipes, Australia
resolves10.1007/s004100050184A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB
resolves10.1016/j.epsl.2009.11.027Major element chemistry of ocean island basalts — Conditions of mantle melting and heterogeneity of mantle source
resolves10.1016/j.epsl.2004.10.035Flow and melting of a heterogeneous mantle: 1. Method and importance to the geochemistry of ocean island and mid-ocean ridge basalts
resolves10.1029/2001GC000217The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa
resolves10.1016/j.gca.2011.11.017A possible high Nb/Ta reservoir in the continental lithospheric mantle and consequences on the global Nb budget – Evidence from continental basalts from Central Germany
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
resolves10.1038/srep05314Missing Lead and High 3He/4He in Ancient Sulfides Associated with Continental Crust Formation
resolves10.1111/j.1945-5100.2000.tb01771.xNiobium and tantalum in carbonaceous chondrites: Constraints on the solar system and primitive mantle niobium/tantalum, zirconium/niobium, and niobium/uranium ratio
resolves10.1016/j.epsl.2017.11.016On the development of the calc-alkaline and tholeiitic magma series: A deep crustal cumulate perspective
resolves10.1126/science.aad5513Archean upper crust transition from mafic to felsic marks the onset of plate tectonics
resolves10.1130/G37475.1Nb-Ta fractionation in peraluminous granites: A marker of the magmatic-hydrothermal transition
resolves10.1016/j.gca.2008.02.018Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton
resolves10.1016/j.chemgeo.2008.08.004In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard
resolves10.1016/S0009-2541(02)00151-1Trace-element incorporation in titanite: constraints from experimentally determined solid/liquid partition coefficients
resolves10.1016/j.epsl.2015.08.027Geochemistry and thermodynamics of an earthquake: A case study of pseudotachylites within mylonitic granitoid
resolves10.1016/j.epsl.2014.10.002Onset of oxidative weathering of continents recorded in the geochemistry of ancient glacial diamictites
resolves10.1130/G36641.1Europium anomalies constrain the mass of recycled lower continental crust
The 4 references without a DOI — listed, not checked
no DOI — not checkedTaylor, S. R. & McLennan, S. M. The Continental Crust. (Wiley, Oxford, 1985).
no DOI — not checkedMoyen, J.-F. & Stevens, G. in Archean Geodynamics and Environments 149–175 (American Geophysical Union, Washington, 2013).
no DOI — not checkedLee, C. T. A. in Treatise on Geochemistry 2nd edn (eds Holland, H. D. & Turekian, K. K.) 423–456 (Elsevier, Oxford, 2014).
no DOI — not checkedGeoRem: https://georem.mpch-mainz.gwdg.de/sample_query_pref.asp.
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