Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present
暂无分享,去创建一个
[1] A. Pourmand,et al. Routine isotopic analysis of iron by HR-MC-ICPMS: How precise and how accurate? , 2009 .
[2] A. Nutman,et al. New 1:20,000 scale geological maps, synthesis and history of investigation of the Isua supracrustal belt and adjacent orthogneisses, southern West Greenland: a glimpse of Eoarchaean crust formation and orogeny , 2009 .
[3] Katherine A. Kelley,et al. Water and the Oxidation State of Subduction Zone Magmas , 2009, Science.
[4] W. Griffin,et al. Fractionation of oxygen and iron isotopes by partial melting processes : implications for the interpretation of stable isotope signatures in mafic rocks , 2009 .
[5] C. Langmuir,et al. Origins of chemical diversity of back‐arc basin basalts: A segment‐scale study of the Eastern Lau Spreading Center , 2009 .
[6] M. Norman,et al. Evidence for subduction at 3.8 Ga: Geochemistry of arc-like metabasalts from the southern edge of the Isua Supracrustal Belt , 2009 .
[7] N. Dauphas,et al. High Precision Iron Isotopic Analyzes of Meteorites and Terrestrial Rocks: 60Fe Distribution and Mass Fractionation Laws , 2009 .
[8] V. Polyakov. Equilibrium Iron Isotope Fractionation at Core-Mantle Boundary Conditions , 2009, Science.
[9] R. Schoenberg,et al. Iron and lithium isotope systematics of the Hekla volcano, Iceland — Evidence for Fe isotope fractionation during magma differentiation , 2009 .
[10] F. Blanckenburg,et al. Fe isotope systematics of coexisting amphibole and pyroxene in the alkaline igneous rock suite of the Ilímaussaq Complex, South Greenland , 2009 .
[11] S. Sutton,et al. Oxidation state of iron in komatiitic melt inclusions indicates hot Archaean mantle , 2008, Nature.
[12] B. Beard,et al. The role of volatile exsolution and sub-solidus fluid/rock interactions in producing high 56Fe/54Fe ratios in siliceous igneous rocks , 2008 .
[13] R. T. Helz,et al. Iron Isotope Fractionation During Magmatic Differentiation in Kilauea Iki Lava Lake , 2008, Science.
[14] C. Manning,et al. Equilibrium high-temperature Fe isotope fractionation between fayalite and magnetite: An experimental calibration , 2008 .
[15] D. Frost,et al. The Redox State of Earth's Mantle , 2008 .
[16] M. Zuilen,et al. Iron isotope, major and trace element characterization of early Archean supracrustal rocks from SW Greenland: Protolith identification and metamorphic overprint , 2007 .
[17] R. Clayton,et al. Equilibrium Iron Isotope Fractionation Factors of Minerals: Reevaluation from the Data of Nuclear Inelastic Resonant X-ray Scattering and Mossbauer Spectroscopy , 2007 .
[18] D. Ionov,et al. Partial melting and melt percolation in the mantle: The message from Fe isotopes , 2007 .
[19] A. Nutman,et al. ∼3,850 Ma tonalites in the Nuuk region, Greenland: geochemistry and their reworking within an Eoarchaean gneiss complex , 2007 .
[20] B. Beard,et al. Comment on “Iron isotope fractionation during planetary differentiation” by S. Weyer et al., Earth Planet. Sci. Lett. V240, pages 251–264 , 2007 .
[21] F. Poitrasson. Does planetary differentiation really fractionate iron isotopes , 2007 .
[22] H. Rollinson. Recognising early Archaean mantle: a reappraisal , 2007 .
[23] S. Mojzsis,et al. Identification of chemical sedimentary protoliths using iron isotopes in the > 3750 Ma Nuvvuagittuq supracrustal belt, Canada , 2007 .
[24] F. Blanckenburg,et al. The experimental calibration of the iron isotope fractionation factor between pyrrhotite and peralkaline rhyolitic melt , 2007 .
[25] F. Blanckenburg,et al. Modes of planetary-scale Fe isotope fractionation , 2006 .
[26] M. Anand,et al. Searching for signatures of life on Mars: an Fe-isotope perspective , 2006, Philosophical Transactions of the Royal Society B: Biological Sciences.
[27] Katherine A. Kelley,et al. Mantle melting as a function of water content beneath back-arc basins , 2006 .
[28] Jean Susini,et al. Redox state of iron in peralkaline rhyolitic glass/melt: X-ray absorption micro-spectroscopy experiments at high temperature , 2006 .
[29] O. Rouxel,et al. Mass spectrometry and natural variations of iron isotopes. , 2006, Mass spectrometry reviews.
[30] A. Woodland,et al. Ferric iron in orogenic lherzolite massifs and controls of oxygen fugacity in the upper mantle , 2006 .
[31] B. Mysen. The structural behavior of ferric and ferrous iron in aluminosilicate glass near meta-aluminosilicate joins , 2006 .
[32] A. Anbar,et al. Iron isotope fractionation during planetary differentiation , 2005 .
[33] Cin-Ty A. Lee,et al. Similar V/Sc Systematics in MORB and Arc Basalts: Implications for the Oxygen Fugacities of their Mantle Source Regions , 2005 .
[34] F. Poitrasson,et al. Heavy iron isotope composition of granites determined by high resolution MC-ICP-MS , 2005 .
[35] Patricia Ann Mabrouk,et al. Multi-spectroscopic study of Fe(II) in silicate glasses: Implications for the coordination environment of Fe(II) in silicate melts , 2005 .
[36] M. Wilke,et al. Erratum to “Determination of the iron oxidation state in basaltic glasses using XANES at the K-edge” [Chem. Geol. 213 (2004) 71–87] , 2005 .
[37] C. McCammon,et al. Systematic iron isotope variations in mantle rocks and minerals: The effects of partial melting and oxygen fugacity , 2005 .
[38] F. Poitrasson,et al. Significance of iron isotope mineral fractionation in pallasites and iron meteorites for the core-mantle differentiation of terrestrial planets [rapid communication] , 2005 .
[39] F. Blanckenburg,et al. An assessment of the accuracy of stable Fe isotope ratio measurements on samples with organic and inorganic matrices by high-resolution multicollector ICP-MS , 2005 .
[40] A. Bézos,et al. The Fe3+/ΣFe ratios of MORB glasses and their implications for mantle melting , 2005 .
[41] A. Davis,et al. Clues from Fe Isotope Variations on the Origin of Early Archean BIFs from Greenland , 2004, Science.
[42] D. Rubie,et al. The Constancy of Upper Mantle fO2 Through Time Inferred from V/Sc Ratios in Basalts: Implications for the Rise in Atmospheric O2 , 2004 .
[43] M. Wilke,et al. Determination of the iron oxidation state in basaltic glasses using XANES at the K-edge , 2004 .
[44] B. Beard,et al. Inter-mineral Fe isotope variations in mantle-derived rocks and implications for the Fe geochemical cycle , 2004 .
[45] A. Taira,et al. Global tectonic significance of the Solomon Islands and Ontong Java Plateau convergent zone , 2004 .
[46] A. Davis,et al. Chromatographic separation and multicollection-ICPMS analysis of iron. Investigating mass-dependent and -independent isotope effects. , 2004, Analytical chemistry.
[47] F. Poitrasson,et al. Iron isotope differences between Earth, Moon, Mars and Vesta as possible records of contrasted accretion mechanisms , 2004 .
[48] S. Weyer,et al. Fe isotope variations in natural materials measured using high mass resolution multiple collector ICPMS. , 2004, Analytical chemistry.
[49] A. Hofmann,et al. Alteration and geochemical patterns in the 3.7–3.8 Ga Isua greenstone belt, West Greenland , 2003 .
[50] B. Öhlander,et al. Performance of high resolution MC-ICP-MS for Fe isotope ratio measurements in sedimentary geological materials , 2003 .
[51] Henry J Sun,et al. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe , 2003 .
[52] A. Nutman,et al. ≥ 3850 Ma BIF and mafic inclusions in the early Archaean Itsaq Gneiss Complex around Akilia, southern West Greenland? The difficulties of precise dating of zircon-free protoliths in migmatites , 2002 .
[53] A. Nutman,et al. Constraints on mantle evolution from 187Os/188Os isotopic compositions of Archean ultramafic rocks from southern West Greenland (3.8 Ga) and Western Australia (3.46 Ga) , 2002 .
[54] John H. Jones,et al. Oxygen fugacity and geochemical variations in the martian basalts: implications for martian basalt petrogenesis and the oxidation state of the upper mantle of Mars , 2002 .
[55] A. Hofmann,et al. Boninite-like volcanic rocks in the 3.7–3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth , 2002 .
[56] A. Nutman,et al. Evidence for 3650–3600 Ma assembly of the northern end of the Itsaq Gneiss Complex, Greenland: Implication for early Archaean tectonics , 2002 .
[57] J. Schwieters,et al. High precision Fe isotope measurements with high mass resolution MC-ICPMS , 2001 .
[58] S. Eggins,et al. Hafnium isotope evidence for ‘conservative’ element mobility during subduction zone processes , 2001 .
[59] John W. Delano,et al. Redox History of the Earth's Interior since ∼3900 Ma: Implications for Prebiotic Molecules , 2001, Origins of life and evolution of the biosphere.
[60] M. Wadhwa,et al. Redox State of Mars' Upper Mantle and Crust from Eu Anomalies in Shergottite Pyroxenes , 2001, Science.
[61] G. Manhès,et al. Chemical composition of the Earth and the volatility control on planetary genetics , 2001 .
[62] J. Myers. Protoliths of the 3.8-3.7 Ga Isua greenstone belt, West Greenland , 2001 .
[63] V. Polyakov,et al. The use of Mössbauer spectroscopy in stable isotope geochemistry , 2000 .
[64] M. Norman,et al. Meta-igneous (non-gneissic) tonalites and quartz-diorites from an extensive ca. 3800 Ma terrain south of the Isua supracrustal belt, southern West Greenland: constraints on early crust formation , 1999 .
[65] R. Arculus,et al. The redox state of subduction zones: insights from arc-peridotites , 1999 .
[66] T. Masuda,et al. Plate Tectonics at 3.8–3.7 Ga: Field Evidence from the Isua Accretionary Complex, Southern West Greenland , 1999, The Journal of Geology.
[67] A. Bowman,et al. Applied smoothing techniques for data analysis : the kernel approach with S-plus illustrations , 1999 .
[68] B. Beard,et al. High precision iron isotope measurements of terrestrial and lunar materials , 1999 .
[69] A. D. Saunders,et al. Geological tectonic framework of Solomon Islands, SW Pacific: crustal accretion and growth within an intra-oceanic setting , 1999 .
[70] S. Eggins,et al. Magma Genesis in the New Britain Island Arc: Further Insights into Melting and Mass Transfer Processes , 1998 .
[71] K. Collerson,et al. Geochemical Evolution within the Tonga–Kermadec–Lau Arc–Back-arc Systems: the Role of Varying Mantle Wedge Composition in Space and Time , 1998 .
[72] D. Canil. Vanadium partitioning and the oxidation state of Archaean komatiite magmas , 1997, Nature.
[73] A. Nutman,et al. The Itsaq Gneiss Complex of southern West Greenland; the world's most extensive record of early crustal evolution (3900-3600 Ma) , 1996 .
[74] D. Ohnenstetter,et al. Compositional variation and primary water contents of differentiated interstitial and included glasses in boninites , 1996 .
[75] W. McDonough,et al. Ferric iron in peridotites and mantle oxidation states , 1994 .
[76] S. Newman,et al. The role of water in the petrogenesis of Mariana trough magmas , 1994 .
[77] R. Johnson,et al. Isotopic and trace-element profiles across the New Britain island arc, Papua New Guinea , 1993 .
[78] R. Johnson,et al. Timescale for producing the geochemical signature of island arc magmas: U-Th-Po and Be-B systematics in recent Papua New Guinea lavas , 1993 .
[79] P. Bievre,et al. Determination of the absolute isotopic composition and Atomic Weight of a reference sample of natural iron , 1992 .
[80] D. Ohnenstetter,et al. Overgrowth Textures, Disequilibrium Zoning, and Cooling History of a Glassy Four-Pyroxene Boninite Dyke from New Caledonia , 1992 .
[81] J. Morris,et al. The subducted component in island arc lavas: constraints from Be isotopes and B–Be systematics , 1990, Nature.
[82] C. M. Schiffries,et al. Petrogenesis of Ultramafic Metamorphic Rocks from the 3800 Ma Isua Supracrustal Belt, West Greenland , 1988 .
[83] C. Langmuir,et al. Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness , 1987 .
[84] C. Langmuir,et al. Oxidation states of mid-ocean ridge basalt glasses , 1986 .
[85] A. Rubin. The Blithfield meteorite and the origin of sulfide rich metal-poor clasts and inclusions in brecciated enstatite chondrites , 1984 .
[86] F. Strelow. Improved separation of iron from copper and other elements by anion-exchange chromatography on a 4% cross-linked resin with high concentrations of hydrochloric acid. , 1980, Talanta.
[87] N. Kuroda,et al. Clinoenstatite in boninites from the Bonin Islands, Japan , 1980, Nature.
[88] W. Bryan,et al. Mineralogy and Geochemistry of the Younger Volcanic Islands of Tonga, S.W. Pacific , 1973 .
[89] W. Bryan,et al. Geology, petrography, and geochemistry of the volcanic islands of Tonga , 1972 .
[90] W. Melson,et al. Volcanic Eruption at Metis Shoal, Tonga, 1967-1968: Description and Petrology , 1970 .
[91] A. J. Martin,et al. A new form of chromatogram employing two liquid phases: A theory of chromatography. 2. Application to the micro-determination of the higher monoamino-acids in proteins. , 1941, The Biochemical journal.
[92] J. N. Wilson,et al. A Theory of Chromatography , 1940 .
[93] Dunyi Liu,et al. Eoarchaean crustal growth in West Greenland (Itsaq Gneiss Complex) and in northeastern China (Anshan area): review and synthesis , 2009 .
[94] M. Wadhwa. Redox conditions on small bodies, the moon and mars , 2008 .
[95] E. Schauble. Applying Stable Isotope Fractionation Theory to New Systems , 2004 .
[96] A. Nutman,et al. Abyssal peridotites >3,800 Ma from southern West Greenland: field relationships, petrography, geochronology, whole-rock and mineral chemistry of dunite and harzburgite inclusions in the Itsaq Gneiss Complex , 2002 .
[97] M. Rosing,et al. Earliest part of Earth's stratigraphic record: A reappraisal of the >3.7 Ga Isua (Greenland) supracrustal sequence , 1996 .
[98] W. Bryan,et al. Regional geochemistry of the Lau-Tonga arc and backarc systems , 1994 .
[99] A. Crawford,et al. Classification, petrogenesis and tectonic setting of boninites. , 1989 .
[100] D. Sears,et al. Overview and classification of meteorites. , 1988 .
[101] Basaltic Volcanism Study. Basaltic volcanism on the terrestrial planets , 1981 .
[102] M. Tatsumoto,et al. ISOTOPIC COMPOSITION OF LEAD IN VOLCANIC ROCKS FROM CENTRAL HONSHU WITH REGARD TO BASALT GENESIS. , 1969 .