Trace element chemistry of peridotitic garnets in diamonds from the Premier (Cullinan) and Finsch kimberlites, South Africa: Contrasting styles of mantle metasomatism

[1]  W. Griffin,et al.  Diamond-forming fluids in fibrous diamonds: The trace-element perspective , 2013 .

[2]  J. Harris,et al.  Silicate and Oxide Inclusions in Diamonds from the Finsch Kimberlite Pipe , 2013 .

[3]  Hong‐fu Zhang,et al.  Widespread refertilization of cratonic and circum-cratonic lithospheric mantle , 2013 .

[4]  M. Walter,et al.  Diamonds and the Geology of Mantle Carbon , 2013 .

[5]  S. Aulbach Craton nucleation and formation of thick lithospheric roots , 2012 .

[6]  C. Herzberg,et al.  Formation of cratonic lithosphere: An integrated thermal and petrological model , 2012 .

[7]  W. Griffin,et al.  High-Mg carbonatitic melts in diamonds, kimberlites and the sub-continental lithosphere , 2011 .

[8]  S. H. Richardson,et al.  Start of the Wilson Cycle at 3 Ga Shown by Diamonds from Subcontinental Mantle , 2011, Science.

[9]  R. Luth,et al.  Growth of diamond in hydrous silicate melts , 2011 .

[10]  S. H. Richardson,et al.  AGES OF CRATONIC DIAMOND AND LITHOSPHERE EVOLUTION: CONSTRAINTS ON PRECAMBRIAN TECTONICS AND DIAMOND EXPLORATION , 2010 .

[11]  W. Griffin,et al.  Trace-element patterns of fibrous and monocrystalline diamonds: Insights into mantle fluids , 2010 .

[12]  F. Viljoen,et al.  Trace element chemistry of mineral inclusions in eclogitic diamonds from the Premier (Cullinan) and Finsch kimberlites, South Africa: Implications for the evolution of their mantle source , 2010 .

[13]  S. H. Richardson,et al.  Diamonds through Time , 2010 .

[14]  R. Luth,et al.  Oxidation state of the lithospheric mantle beneath Diavik diamond mine, central Slave craton, NWT, Canada , 2010 .

[15]  P. Cartigny,et al.  Mixed fluid sources involved in diamond growth constrained by Sr–Nd–Pb–C–N isotopes and trace elements , 2010 .

[16]  K. Muehlenbachs,et al.  Sources of carbon in inclusion bearing diamonds , 2009 .

[17]  K. Viljoen,et al.  Ancient metasomatism recorded by ultra-depleted garnet inclusions in diamonds from DeBeers Pool, South Africa , 2009 .

[18]  F. Viljoen,et al.  Geochemical processes in peridotite xenoliths from the Premier diamond mine, South Africa: Evidence for the depletion and refertilisation of subcratonic lithosphere , 2009 .

[19]  A. Sokol,et al.  Fluid regime and diamond formation in the reduced mantle: Experimental constraints , 2009 .

[20]  T. Stachel,et al.  Formation of diamond in the Earth’s mantle , 2009, Journal of physics. Condensed matter : an Institute of Physics journal.

[21]  W. McDonough,et al.  Trace element partitioning between garnet lherzolite and carbonatite at 6.6 and 8.6 GPa with applications to the geochemistry of the mantle and of mantle-derived melts , 2009 .

[22]  I. Artemieva The continental lithosphere: Reconciling thermal, seismic, and petrologic data , 2009 .

[23]  N. Coltice,et al.  Origin of Archean subcontinental lithospheric mantle: Some petrological constraints , 2009 .

[24]  W. Griffin,et al.  A new model for the evolution of diamond-forming fluids , 2009 .

[25]  W. Müller,et al.  A snapshot of mantle metasomatism: Trace element analysis of coexisting fluid (LA-ICP-MS) and silicate (SIMS) inclusions in fibrous diamonds , 2009 .

[26]  D. Pearson,et al.  Origins of subcalcic garnets and their relation to diamond forming fluids—Case studies from Ekati (NWT-Canada) and Murowa (Zimbabwe) , 2009 .

[27]  C. McCammon,et al.  Oxidation of the Kaapvaal lithospheric mantle driven by metasomatism , 2009 .

[28]  T. Stachel,et al.  The origin of cratonic diamonds — Constraints from mineral inclusions , 2008 .

[29]  P. Silver,et al.  Evidence for a compositional boundary within the lithospheric mantle beneath the Kalahari craton from S receiver functions , 2008 .

[30]  D. Pearson,et al.  Formation of Archaean continental lithosphere and its diamonds: the root of the problem , 2008, Journal of the Geological Society.

[31]  S. H. Richardson,et al.  Continental mantle signature of Bushveld magmas and coeval diamonds , 2008, Nature.

[32]  K. Viljoen,et al.  Methane-related diamond crystallization in the Earth's mantle: Stable isotope evidences from a single diamond-bearing xenolith , 2007 .

[33]  E. Hauri,et al.  Fluid inclusions in diamonds from the Diavik mine, Canada and the evolution of diamond-forming fluids , 2007 .

[34]  A. Jones,et al.  Co-existing fluid and silicate inclusions in mantle diamond , 2006 .

[35]  M. Becker,et al.  Geochemistry of South African On- and Off-craton, Group I and Group II Kimberlites: Petrogenesis and Source Region Evolution , 2006 .

[36]  A. Menzies,et al.  An updated classification scheme for mantle-derived garnet, for use by diamond explorers , 2004 .

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

[38]  S. Lee,et al.  Mantle seismic structure beneath the Kaapvaal and Zimbabwe Cratons , 2004 .

[39]  K. Viljoen,et al.  Diamondiferous lithospheric roots along the western margin of the Kalahari Craton—the peridotitic inclusion suite in diamonds from Orapa and Jwaneng , 2004 .

[40]  S. H. Richardson,et al.  Diamond Genesis, Seismic Structure, and Evolution of the Kaapvaal-Zimbabwe Craton , 2002, Science.

[41]  T. Stachel Diamonds from the asthenosphere and the transition zone , 2001 .

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

[43]  R. Harmer The Petrogenetic Association of Carbonatite and Alkaline Magmatism: Constraints from the Spitskop Complex, South Africa , 1999 .

[44]  W. Griffin,et al.  Harzburgite to lherzolite and back again: metasomatic processes in ultramafic xenoliths from the Wesselton kimberlite, Kimberley, South Africa , 1999 .

[45]  K. Johnson Experimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures , 1998 .

[46]  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 .

[47]  O. Navon Diamond formation in the Earth's mantle , 1998 .

[48]  K. Viljoen,et al.  Mineral inclusions in diamonds from the Venetia kimberlites, Northern Province, South Africa , 1998 .

[49]  T. Stachel,et al.  Diamond precipitation and mantle metasomatism – evidence from the trace element chemistry of silicate inclusions in diamonds from Akwatia, Ghana , 1997 .

[50]  T. Stachel,et al.  Syngenetic inclusions in diamond from the Birim field (Ghana) – a deep peridotitic profile with a history of depletion and re-enrichment , 1997 .

[51]  B. Kjarsgaard,et al.  Micro-PIXE analysis of silicate reference standards for trace Ni, Cu, Zn, Ga, Ge, As, Rb, Sr, Y, Zr, Nb, Mo and Pb, with emphasis on Ni for application of the Ni-in-garnet geothermometer , 1996 .

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

[53]  H. Milledge,et al.  Geologically Significant Information from Routine Analysis of the Mid-Infrared Spectra of Diamonds , 1995 .

[54]  R. Hinton Ion microprobe analysis in geology , 1995 .

[55]  S. H. Richardson,et al.  Three generations of diamonds from old continental mantle , 1993, Nature.

[56]  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 .

[57]  K. Nickel,et al.  Geothermobarometry in Four-phase Lherzolites I. Experimental Results from 10 to 60 kb , 1990 .

[58]  M. Ridd,et al.  Nitrogen-defect aggregation characteristics of some Australasian diamonds; time-temperature constraints on the source regions of pipe and alluvial diamonds , 1990 .

[59]  J. Gurney The diamondiferous roots of our wandering continent , 1990 .

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

[61]  E. Yochelson,et al.  28th International Geological Congress , 1989 .

[62]  P. Deines,et al.  Nitrogen and 13C content of Finsch and Premier diamonds and their implications , 1989 .

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

[64]  J. Harris,et al.  Inclusions in Premier Mine diamonds , 1985 .

[65]  J. Kramers,et al.  Emplacement ages of Jurassic-Cretaceous South African kimberlites by the Rb-Sr method on phlogopite and whole-rock samples , 1985 .

[66]  S. Harley An experimental study of the partitioning of Fe and Mg between garnet and orthopyroxene , 1984 .

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

[68]  B. Wood,et al.  An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer , 1979 .

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

[70]  W. Eppler Inclusions in Diamond , 1961 .