Nature of slab-mantle interactions recorded by coupled δ13C–δ15N–δ18O signatures and elemental compositions of Koidu diamonds and their inclusions
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[1] Kan Li,et al. Nitrogen enrichments in sheeted dikes and gabbros from DSDP/ODP/IODP Hole 504B and 1256D: Insights into nitrogen recycling in Central America and global subduction zones , 2022, Geochimica et Cosmochimica Acta.
[2] S. Aulbach,et al. Mineral Inclusions in Lithospheric Diamonds , 2022, Reviews in Mineralogy and Geochemistry.
[3] R. Stern,et al. Formation of mixed paragenesis diamonds during multistage growth – constraints from in situ δ13C–δ15N–[N] analyses of Koidu diamonds , 2022, Geochimica et Cosmochimica Acta.
[4] Jabrane Labidi. The origin of nitrogen in Earth's mantle: Constraints from basalts 15N/14N and N2/3He ratios , 2022, Chemical Geology.
[5] D. Sverjensky,et al. A genetic metasomatic link between eclogitic and peridotitic diamond inclusions , 2021, Geochemical Perspectives Letters.
[6] S. Aulbach. Temperature-dependent Rutile Solubility in Garnet and Clinopyroxene from Mantle Eclogite: Implications for Continental Crust Formation and V-based Oxybarometry , 2020 .
[7] J. Harris,et al. The lithospheric-to-lower-mantle carbon cycle recorded in superdeep diamonds , 2020, Nature.
[8] K. Viljoen,et al. Ultramafic Carbonated Melt‐ and Auto‐Metasomatism in Mantle Eclogites: Compositional Effects and Geophysical Consequences , 2020, Geochemistry, Geophysics, Geosystems.
[9] T. Pettke,et al. Subducting serpentinites release reduced, not oxidized, aqueous fluids , 2019, Scientific Reports.
[10] D. Pearson,et al. Diamond isotope compositions indicate altered igneous oceanic crust dominates deep carbon recycling , 2019, Earth and Planetary Science Letters.
[11] N. Arndt,et al. Origin of high-Mg bimineralic eclogite xenoliths in kimberlite – reply to comment from Claude Herzberg , 2019, Earth and Planetary Science Letters.
[12] D. Pearson,et al. An oxygen isotope test for the origin of Archean mantle roots , 2018, Geochemical Perspectives Letters.
[13] Xian‐Hua Li,et al. The oxygen isotope composition of mantle eclogites as a proxy of their origin and evolution: A review , 2018, Earth-Science Reviews.
[14] M. Izawa,et al. Nitrogen Concentrations and Isotopic Compositions of Seafloor-Altered Terrestrial Basaltic Glass: Implications for Astrobiology , 2017, Astrobiology.
[15] K. Viljoen,et al. Eclogite xenoliths from Orapa: Ocean crust recycling, mantle metasomatism and carbon cycling at the western Zimbabwe craton margin , 2017 .
[16] D. Sverjensky,et al. Highly oxidising fluids generated during serpentinite breakdown in subduction zones , 2017, Scientific Reports.
[17] D. Frost,et al. The depth of sub-lithospheric diamond formation and the redistribution of carbon in the deep mantle , 2017 .
[18] S. Kohn,et al. Trace element composition of silicate inclusions in sub-lithospheric diamonds from the Juina-5 kimberlite: Evidence for diamond growth from slab melts , 2016 .
[19] S. Shirey,et al. Type Ib diamond formation and preservation in the West African lithospheric mantle: Re–Os age constraints from sulphide inclusions in Zimmi diamonds , 2016 .
[20] D. Jacob,et al. Major- and trace-elements in cratonic mantle eclogites and pyroxenites reveal heterogeneous sources and metamorphic processing of low-pressure protoliths , 2016 .
[21] D. Rubatto,et al. Eclogitic diamonds from variable crustal protoliths in the northeastern Siberian craton: trace elements and coupled δ13C – δ18O signatures in diamonds and garnet inclusions , 2016 .
[22] B. Kjarsgaard,et al. In situ oxygen-isotope, major-, and trace-element constraints on the metasomatic modification and crustal origin of a diamondiferous eclogite from Roberts Victor, Kaapvaal Craton , 2016 .
[23] S. Kohn,et al. Slab melting as a barrier to deep carbon subduction , 2016, Nature.
[24] S. Kohn,et al. Stable isotope evidence for crustal recycling as recorded by superdeep diamonds , 2015 .
[25] R. Stern,et al. Extreme 18O-enrichment in majorite constrains a crustal origin of transition zone diamonds , 2015 .
[26] P. Cartigny,et al. Diamond Formation: A Stable Isotope Perspective , 2014 .
[27] A. Jones,et al. Constraining the internal variability of the stable isotopes of carbon and nitrogen within mantle diamonds , 2014 .
[28] H. Tkalčić,et al. Metapyroxenite in the mantle transition zone revealed from majorite inclusions in diamonds , 2013 .
[29] A. Locock,et al. Nomenclature of the garnet supergroup , 2013 .
[30] R. Stern,et al. Diamond from recycled crustal carbon documented by coupled δ18O–δ13C measurements of diamonds and theirinclusions , 2013 .
[31] S. Aulbach,et al. Chalcophile and siderophile elements in sulphide inclusions in eclogitic diamonds and metal cycling in a Paleoproterozoic subduction zone , 2012 .
[32] R. Stern,et al. Eclogite formation beneath the northern Slave craton constrained by diamond inclusions: Oceanic lithosphere origin without a crustal signature , 2012 .
[33] L. Heaman,et al. Microxenoliths from the Slave craton: Archives of diamond formation along fluid conduits , 2011 .
[34] A. Rohrbach,et al. Redox freezing and melting in the Earth’s deep mantle resulting from carbon–iron redox coupling , 2011, Nature.
[35] B. Kamber,et al. Majoritic garnet: A new approach to pressure estimation of shock events in meteorites and the encapsulation of sub-lithospheric inclusions in diamond , 2010 .
[36] L. Heaman,et al. The origin of high-MgO diamond eclogites from the Jericho Kimberlite, Canada , 2009 .
[37] Andrew J. Locock,et al. An Excel spreadsheet to recast analyses of garnet into end-member components, and a synopsis of the crystal chemistry of natural silicate garnets , 2008, Comput. Geosci..
[38] S. Clark,et al. Primary carbonatite melt from deeply subducted oceanic crust , 2008, Nature.
[39] D. Frost,et al. The Redox State of Earth's Mantle , 2008 .
[40] Long Li,et al. Nitrogen concentration and δ15N of altered oceanic crust obtained on ODP Legs 129 and 185 : Insights into alteration-related nitrogen enrichment and the nitrogen subduction budget , 2007 .
[41] M. Bonifacie,et al. Nitrogen content and isotopic composition of oceanic crust at a superfast spreading ridge: A profile in altered basalts from ODP Site 1256, Leg 206 , 2005 .
[42] Dorrit E. Jacob. Nature and origin of eclogite xenoliths from kimberlites , 2004 .
[43] A. Menzies,et al. An updated classification scheme for mantle-derived garnet, for use by diamond explorers , 2004 .
[44] K. Viljoen,et al. The trace element composition of silicate inclusions in diamonds: a review , 2004 .
[45] B. Harte,et al. Evidence of subduction and crust–mantle mixing from a single diamond , 2004 .
[46] E. Skinner,et al. Kimberlites of the Man craton, West Africa , 2004 .
[47] S. Foley,et al. Eclogite xenoliths from the Kuruman kimberlites, South Africa: geochemical fingerprinting of deep subduction and cumulate processes ☆ , 2004 .
[48] Y. Fei,et al. Titanium solubility in coexisting garnet and clinopyroxene at very high pressure: the significance of exsolved rutile in garnet , 2003 .
[49] J. Alt. Stable isotopic composition of upper oceanic crust formed at a fast spreading ridge, ODP Site 801 , 2003 .
[50] W. McDonough,et al. Geochemistry of xenolithic eclogites from West Africa, part 2: origins of the high MgO eclogites , 2002 .
[51] W. McDonough,et al. Geochemistry of xenolithic eclogites from West Africa, Part I: A link between low MgO eclogites and Archean crust formation , 2001 .
[52] Manfred Schidlowski,et al. Carbon isotopes as biogeochemical recorders of life over 3.8 Ga of Earth history: evolution of a concept , 2001 .
[53] J. Valley,et al. Coesite eclogites from the Roberts Victor kimberlite, South Africa , 2000 .
[54] D. Laporte,et al. Ultrafast mantle impregnation by carbonatite melts , 2000 .
[55] J. Valley,et al. Oxygen and hydrogen isotope study of high-pressure metagabbros and metabasalts (Cyclades, Greece): implications for the subduction of oceanic crust , 2000 .
[56] D. Lowry,et al. Oxygen isotope composition of syngenetic inclusions in diamond from the Finsch Mine, RSA , 1999 .
[57] Jeff W. Harris,et al. Rare and unusual mineral inclusions in diamonds from Mwadui, Tanzania , 1998 .
[58] T. Stachel,et al. Diamond precipitation and mantle metasomatism – evidence from the trace element chemistry of silicate inclusions in diamonds from Akwatia, Ghana , 1997 .
[59] B. Harte,et al. Partitioning of trace elements between clinopyroxene and garnet: data from mantle eclogites , 1997 .
[60] S. Haggerty,et al. Petrography and mineral compositions of eclogites from the Koidu Kimberlite Complex, Sierra Leone , 1995 .
[61] P. Deines,et al. Petrochemistry of ultradeep (>300 km) and transition zone xenoliths , 1995, International Kimberlite Conference Extended Abstracts: 1995.
[62] P. Deines,et al. Sulfide inclusion chemistry and carbon isotopes of African diamonds , 1995 .
[63] E. Watson,et al. Interconnectivity of carbonate melt at low melt fraction , 1995 .
[64] J. Bédard. A procedure for calculating the equilibrium distribution of trace elements among the minerals of cumulate rocks, and the concentration of trace elements in the coexisting liquids , 1994 .
[65] D. Lowry,et al. Diamondiferous eclogites from Siberia: Remnants of Archean oceanic crust , 1994 .
[66] D. Lowry,et al. Oxygen isotope composition of mantle peridotite , 1994 .
[67] M. Fogel,et al. Nitrogen-isotope compositions of metasedimentary rocks in the Catalina Schist, California: Implications for metamorphic devolatilization history , 1992 .
[68] F. Caporuscio,et al. Trace element crystal chemistry of mantle eclogites , 1990 .
[69] S. Haggerty,et al. Petrochemistry of eclogites from the Koidu Kimberlite Complex, Sierra Leone , 1989 .
[70] D. J. Schulze,et al. Constraints on the abundance of eclogite in the upper mantle , 1989 .
[71] T. Irifune. An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle , 1987 .
[72] W. Manton,et al. Roberts victor eclogites: Ancient oceanic crust , 1986 .
[73] J. Alt,et al. An oxygen isotopic profile through the upper kilometer of the oceanic crust, DSDP hole 504B , 1986 .
[74] Tetsuo Irifune,et al. The eclogite-garnetite transformation at high pressure and some geophysical implications , 1986 .
[75] Rory O. Moore,et al. Pyroxene solid solution in garnets included in diamond , 1985, Nature.
[76] C. T. Pillinger,et al. Carbon isotopic variation in spectral type II diamonds , 1983, Nature.
[77] H. Taylor,et al. An oxygen isotope profile in a section of Cretaceous oceanic crust, Samail Ophiolite, Oman: Evidence for δ18O buffering of the oceans by deep (>5 km) seawater-hydrothermal circulation at mid-ocean ridges , 1981 .
[78] G. Wasserburg,et al. Sm‐Nd, Rb‐Sr, and 18O/16O isotopic systematics in an oceanic crustal section: Evidence from the Samail Ophiolite , 1981 .
[79] S. Akimoto,et al. High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent minerals , 1979 .
[80] JOSEPH V. Smith,et al. Na, K, P and Ti in garnet, pyroxene and olivine from peridotite and eclogite xenoliths from African kimberlites , 1978 .
[81] N. Christensen,et al. The seismic velocity structure of a traverse through the Bay of Islands Ophiolite Complex, Newfoundland, An exposure of oceanic crust and upper mantle , 1978 .
[82] P. Baertschi. Absolute18O content of standard mean ocean water , 1976 .
[83] J. Dawson,et al. Na, P, Ti and coordination of Si in garnet from peridotite and eclogite xenoliths , 1976, Nature.
[84] R. Doig,et al. Eclogite nodules from kimberlite pipes of the Colorado plateau—samples of subducted Franciscan-type oceanic lithosphere , 1973 .
[85] M. Drake,et al. Europium Anomaly in Plagioclase Feldspar: Experimental Results and Semiquantitative Model , 1973, Science.
[86] T. McGetchin,et al. A crustal-upper-mantle model for the Colorado Plateau based on observations of crystalline rock fragments in the Moses Rock Dike , 1972 .
[87] R. Clayton,et al. Oxygen Isotope Geochemistry of Submarine Greenstones , 1972 .
[88] R. Clayton,et al. Oxygen Isotope Studies of Fresh and Weathered Submarine Basalts , 1972 .
[89] A. E. Ringwood,et al. Synthesis of majorite and other high pressure garnets and perovskites , 1971 .
[90] H. Taylor,et al. Oxygen and Carbon Isotope Studies of Contact Metamorphism of Carbonate Rocks , 1969 .
[91] J. A. Philpotts,et al. Europium anomalies and the genesis of basalt , 1968 .
[92] H. S. Yoder,et al. Formation and fractionation of basic magmas at high pressures , 1967, Scottish Journal of Geology.
[93] P. Bartholomé. Genesis of the Gore Mountain garnet deposit, New York , 1960 .
[94] E. Watson,et al. Experimental investigation into the substitution mechanisms and solubility of Ti in garnet , 2017 .
[95] B. Wood,et al. The pyroxenite-diamond connection , 2016 .
[96] J. Valley,et al. Eclogite-facies fluid infiltration: constraints from δ18O zoning in garnet , 2012, Contributions to Mineralogy and Petrology.
[97] S. Aulbach,et al. Eclogitic and websteritic diamond sources beneath the Limpopo Belt – is slab-melting the link? , 2002 .
[98] Stefan Aulbach,et al. Kankan diamonds (Guinea) III: δ13C and nitrogen characteristics of deep diamonds , 2002 .
[99] J. Eiler. Oxygen Isotope Variations of Basaltic Lavas and Upper Mantle Rocks , 2001 .
[100] D. Teagle,et al. Hydrothermal alteration and fluid fluxes in ophiolites and oceanic crust , 2000 .
[101] M. Otter,et al. The application of C isotope measurements to the identification of the sources of C in diamonds: a review , 1991 .
[102] Scott M. McLennan,et al. Rare earth elements in sedimentary rocks; influence of provenance and sedimentary processes , 1989 .
[103] S. Haggerty,et al. The Koidu Kimberlite Complex, Sierra Leone: Geological Setting, Petrology and Mineral Chemistry , 1984 .