Time steps of depletion and enrichment in the Kaapvaal craton as recorded by subcalcic garnets from Finsch (SA)

[1]  M. Trieloff,et al.  40Ar/39Ar-ages of phlogopite in mantle xenoliths from South African kimberlites: Evidence for metasomatic mantle impregnation during the Kibaran orogenic cycle , 2008 .

[2]  S. Gibson,et al.  Melt Depletion and Enrichment beneath the Western Kaapvaal Craton: Evidence from Finsch Peridotite Xenoliths , 2008 .

[3]  Y. Lahaye,et al.  Experimental Melting of Carbonated Peridotite at 6-10 GPa , 2007 .

[4]  W. Griffin,et al.  Diamond, subcalcic garnet, and mantle metasomatism: Kimberlite sampling patterns define the link , 2007 .

[5]  R. Carlson,et al.  The Origin and Evolution of the Kaapvaal Cratonic Lithospheric Mantle , 2007 .

[6]  J. Baker,et al.  Dating the mantle roots of young continental crust , 2006 .

[7]  A. Menzies,et al.  Cr-Saturation Arrays in Concentrate Garnet Compositions from Kimberlite and their Use in Mantle Barometry , 2006 .

[8]  B. Bourdon,et al.  High-precision 142Nd/144Nd measurements in terrestrial rocks : Constraints on the early differentiation of the Earth's mantle , 2006 .

[9]  J. Liégeois,et al.  Geochemistry and Sr, Nd, Pb isotopic composition of the Central Atlantic Magmatic Province (CAMP) in Guyana and Guinea , 2005 .

[10]  D. Weis,et al.  Hf isotope compositions and HREE variations in off-craton garnet and spinel peridotite xenoliths from central Asia , 2005 .

[11]  S. H. Richardson,et al.  Integrated models of diamond formation and craton evolution , 2004 .

[12]  K. Viljoen,et al.  The trace element composition of silicate inclusions in diamonds: a review , 2004 .

[13]  S. Bowring,et al.  Subduction and terrane collision stabilize the western Kaapvaal craton tectosphere 2.9 billion years ago , 2004 .

[14]  D. Pearson,et al.  Re--- Os and Lu--- Hf Isotope Constraints on the Origin and Age of Pyroxenites from the Beni Bousera Peridotite Massif: Implications for Mixed Peridotite--- Pyroxenite Mantle Sources , 2004 .

[15]  D. Schulze.  A classification scheme for mantle-derived garnets in kimberlite: a tool for investigating the mantle and exploring for diamonds , 2003 .

[16]  M. Bizzarro,et al.  A New Digestion and Chemical Separation Technique for Rapid and Highly Reproducible Determination of Lu/Hf and Hf Isotope Ratios in Geological Materials by MC‐ICP‐MS , 2003 .

[17]  D. Jacob,et al.  Evolution of the Archaean crust by delamination and shallow subduction , 2003, Nature.

[18]  C. German,et al.  Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections , 2002 .

[19]  S. S. Schmidberger,et al.  Probing Archean lithosphere using the Lu-Hf isotope systematics of peridotite xenoliths from Somerset Island kimberlites, Canada , 2002 .

[20]  K. Mezger,et al.  Separation of high field strength elements (Nb, Ta, Zr, Hf) and Lu from rock samples for MC‐ICPMS measurements , 2001 .

[21]  S. H. Richardson,et al.  Archean subduction recorded by Re–Os isotopes in eclogitic sulfide inclusions in Kimberley diamonds , 2001 .

[22]  R. Carlson,et al.  Lithospheric mantle evolution of the Kaapvaal Craton: A Re‐Os isotope study of peridotite xenoliths from Lesotho kimberlites , 2001 .

[23]  A. Moore,et al.  The origin of mantle-derived megacrysts and sheared peridotites-evidence from kimberlites in the northern Lesotho - Orange Free State (South Africa) and Botswana pipe clusters , 2001 .

[24]  H. Yurimoto,et al.  Enrichment processes at the base of the Archean lithospheric mantle: observations from trace element characteristics of pyropic garnet inclusions in diamonds , 2000 .

[25]  J. Blichert‐Toft,et al.  Lu–hf garnet geochronology: closure temperature relative to the Sm–Nd system and the effects of trace mineral inclusions , 2000 .

[26]  J. Blundy,et al.  SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C , 2000 .

[27]  D. Canil.  The Ni-in-garnet geothermometer: calibration at natural abundances , 1999 .

[28]  F. Albarède,et al.  Relationships between Lu–Hf and Sm–Nd isotopic systems in the global sedimentary system , 1999 .

[29]  Albarède,et al.  Lu-Hf Isotope Systematics of Garnet Pyroxenites from Beni Bousera, Morocco: Implications for Basalt Origin. , 1999, Science.

[30]  R. Carlson,et al.  Sulphide inclusions in diamonds from the Koffiefontein kimberlite, S Africa: Constraints on diamond ages and mantle Re-Os systematics , 1998 .

[31]  K. Viljoen,et al.  Metasomatic processes in lherzolitic and harzburgitic domains of diamondiferous lithospheric mantle: REE in garnets from xenoliths and inclusions in diamonds , 1998 .

[32]  R. Stalder,et al.  Mineral-aqueous fluid partitioning of trace elements at 900–1200°C and 3.0–5.7 GPa: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism , 1998 .

[33]  D. Günther,et al.  Infiltration of refractory melts into the lowermost oceanic crust: evidence from dunite- and gabbro-hosted clinopyroxenes in the Bay of Islands Ophiolite , 1998 .

[34]  D. Jacob,et al.  NEODYMIUM AND STRONTIUM ISOTOPIC MEASUREMENTS ON SINGLE SUBCALCIC GARNET GRAINS FROM YAKUTIAN KIMBERLITES , 1998 .

[35]  K. Collerson,et al.  LuHf geochronology applied to dating Cenozoic events affecting lower crustal xenoliths from Kilbourne Hole, New Mexico , 1997 .

[36]  C. Ryan,et al.  Trace element partitioning between aqueous fluids, silicate melts and minerals , 1997 .

[37]  F. Albarède,et al.  Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sector-multiple collector ICP-MS , 1997 .

[38]  C. Pin,et al.  Sequential separation of light rare-earth elements, thorium and uranium by miniaturized extraction chromatography: Application to isotopic analyses of silicate rocks , 1997 .

[39]  S. Eggins,et al.  A simple method for the precise determination of ≥ 40 trace elements in geological samples by ICPMS using enriched isotope internal standardisation , 1997 .

[40]  K. Mezger,et al.  The role of inclusions in U-Pb and Sm-Nd garnet geochronology: Stepwise dissolution experiments and trace uranium mapping by fission track analysis , 1996 .

[41]  R. Carlson,et al.  ReOs, SmNd, and RbSr isotope evidence for thick Archaean lithospheric mantle beneath the Siberian craton modified by multistage metasomatism , 1995 .

[42]  W. McDonough,et al.  The composition of the Earth , 1995 .

[43]  P. Kelemen,et al.  Relative depletion of niobium in some arc magmas and the continental crust : partitioning of K, Nb, La, and Ce during melt/rock reaction in the upper mantle , 1993 .

[44]  C. Dupuy,et al.  Carbonated peridotite xenoliths from Spitsbergen: implications for trace element signature of mantle carbonate metasomatism , 1993 .

[45]  P. H. Nixon,et al.  Low-calcium garnet harzburgites from southern Africa: their relations to craton structure and diamond crystallization , 1993 .

[46]  W. McDonough,et al.  Carbonatite metasomatism in the northern Tanzanian mantle: petrographic and geochemical characteristics , 1993 .

[47]  K. Viljoen,et al.  Diamondiferous garnet harzburgites from the Finsch kimberlite, Northern Cape, South Africa , 1992 .

[48]  W. Griffin,et al.  Variations in trapping temperatures and trace elements in peridotite-suite inclusions from African diamonds: evidence for two inclusion suites, and implications for lithosphere stratigraphy , 1992 .

[49]  D. Canil,et al.  Constraints on the origin of mantle-derived low Ca garnets , 1992 .

[50]  A. Crawford,et al.  Evidence for carbonatite metasomatism in spinel peridotite xenoliths from western Victoria, Australia , 1991 .

[51]  T. Köhler,et al.  Geothermobarometry in Four-phase Lherzolites II. New Thermobarometers, and Practical Assessment of Existing Thermobarometers , 1990 .

[52]  K. Card.  A review of the Superior Province of the Canadian Shield, a product of Archean accretion , 1990 .

[53]  S. H. Richardson,et al.  Eclogitic diamonds of Proterozoic age from Cretaceous kimberlites , 1990, Nature.

[54]  A. E. Ringwood,et al.  Slab-mantle interactions: 2. The formation of diamonds , 1989 .

[55]  D. R. Cousens,et al.  Ni in chrome pyrope garnets: a new geothermometer , 1989 .

[56]  R. Carlson,et al.  Os, Sr, Nd, and Pb isotope systematics of southern African peridotite xenoliths: Implications for the chemical evolution of subcontinental mantle , 1989 .

[57]  S. H. Richardson,et al.  Trace element abundance patterns of garnet inclusions in peridotite-suite diamonds , 1987 .

[58]  S. H. Richardson.  Latter-day origin of diamonds of eclogitic paragenesis , 1986, Nature.

[59]  F. R. Boyd,et al.  Diamonds and the African Lithosphere , 1986, Science.

[60]  D. Schulze.  Calcium anomalies in the mantle and a subducted metaserpentinite origin for diamonds , 1986, Nature.

[61]  S. H. Richardson,et al.  Origin of diamonds in old enriched mantle , 1984, Nature.

[62]  A. E. Ringwood,et al.  Synthesis of pyrope-knorringite solid solution series , 1977 .

[63]  H. Pollack,et al.  Regional geotherms and lithospheric thickness , 1977 .

[64]  W. E. Stephens,et al.  Statistical Classification of Garnets from Kimberlite and Associated Xenoliths , 1975, The Journal of Geology.

[65]  J. Gurney,et al.  The discovery of garnets closely related to diamonds in the Finsch pipe, South Africa , 1973 .

[66]  N. Sobolev,et al.  Chrome-rich garnets from the kimberlites of yakutia and their parageneses , 1973 .