An unusual suite of eclogitic, websteritic and transitional websteritic-lherzolitic diamonds from the Voorspoed kimberlite in South Africa: Mineral inclusions and infrared characteristics

[1]  S. Kohn,et al.  The behaviour of platelets in natural diamonds and the development of a new mantle thermometer , 2018, Contributions to Mineralogy and Petrology.

[2]  J. Koornneef,et al.  Archaean and Proterozoic diamond growth from contrasting styles of large-scale magmatism , 2017, Nature Communications.

[3]  R. Luth,et al.  Carbon isotope fractionation during diamond growth in depleted peridotite: counterintuitive insights from modelling water-maximum CHO fluids as multi-component systems , 2017 .

[4]  L. Taylor,et al.  Mineral inclusions in diamonds may be synchronous but not syngenetic , 2017, Nature Communications.

[5]  S. Kohn,et al.  FTIR thermochronometry of natural diamonds: A closer look , 2016 .

[6]  D. Pearson,et al.  “The nature of diamonds and their use in earth's study” , 2016 .

[7]  K. Viljoen,et al.  Formation of diamondiferous kyanite–eclogite in a subduction mélange , 2016 .

[8]  K. Viljoen,et al.  Eclogite xenoliths from the Lace kimberlite, Kaapvaal craton: From convecting mantle source to palaeo-ocean floor and back , 2015 .

[9]  R. Luth,et al.  Diamond formation — Where, when and how? , 2015 .

[10]  R. Creaser,et al.  Origin of eclogite and pyroxenite xenoliths from the Victor kimberlite, Canada, and implications for Superior craton formation , 2014 .

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

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

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

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

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

[16]  G. Howarth,et al.  The geology and emplacement of the volcaniclastic infill at the Voorspoed Group II kimberlite (orangeite) pipe, Kroonstad Cluster, South Africa , 2012 .

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

[18]  G. Howarth,et al.  Petrology of the hypabyssal kimberlite of the Kroonstad group II kimberlite (orangeite) cluster, South Africa: Evolution of the magma within the cluster , 2011 .

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

[20]  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 .

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

[22]  D. Fisher Brown diamonds and high pressure high temperature treatment , 2009 .

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

[24]  D. Phillips,et al.  Diamond provenance studies from 40Ar/39Ar dating of clinopyroxene inclusions: An example from the west coast of Namibia , 2009 .

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

[26]  L. Heaman,et al.  The origin of high-MgO diamond eclogites from the Jericho Kimberlite, Canada , 2009 .

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

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

[29]  T. Stachel,et al.  The origin of cratonic diamonds — Constraints from mineral inclusions , 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]  C. Garrido,et al.  Origin of Pyroxenite–Peridotite Veined Mantle by Refertilization Reactions: Evidence from the Ronda Peridotite (Southern Spain) , 2008 .

[32]  WevNn R. Tlvr,et al.  Nitrogen-defect aggregation characteristics of some Australasian diamonds : Time-temperature constraints on the source regions of pipe and alluvial diamonds , 2007 .

[33]  N. Sleep Mantle plumes from top to bottom , 2006 .

[34]  I. Campbell Large Igneous Provinces and the Mantle Plume Hypothesis , 2005 .

[35]  K. Viljoen,et al.  Contrasting Group I and Group II Eclogite Xenolith Petrogenesis: Petrological, Trace Element and Isotopic Evidence from Eclogite, Garnet-Websterite and Alkremite Xenoliths in the Kaalvallei Kimberlite, South Africa , 2005 .

[36]  S. H. Richardson,et al.  Diamonds Crustal Distribution and Formation Processes in Time and Space and an Integrated Deposit Model , 2005 .

[37]  T. Stachel,et al.  Peridotitic diamonds from Namibia: Constraints on the composition and evolution of their mantle source , 2004 .

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

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

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

[41]  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 .

[42]  W. Griffin,et al.  The evolution of lithospheric mantle beneath the Kalahari Craton and its margins , 2003 .

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

[44]  L. Taylor,et al.  Petrogenesis of group A eclogites and websterites: evidence from the Obnazhennaya kimberlite, Yakutia , 2003 .

[45]  S. Bowring,et al.  Ultrahigh-temperature metamorphism in the lower crust during Neoarchean Ventersdorp rifting and magmatism, Kaapvaal Craton, southern Africa , 2003 .

[46]  B. Harte,et al.  Extreme crustal oxygen isotope signatures preserved in coesite in diamond , 2003, Nature.

[47]  J. Harris,et al.  Diamond formation and source carbonation: mineral associations in diamonds from Namibia , 2003 .

[48]  K. Viljoen An infrared investigation of inclusion-bearing diamonds from the Venetia kimberlite, Northern Province, South Africa : implications for diamonds from craton-margin settings , 2002 .

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

[50]  S. Aulbach,et al.  Eclogitic and websteritic diamond sources beneath the Limpopo Belt – is slab-melting the link? , 2002 .

[51]  J. Bruley,et al.  The nitrogen aggregation sequence and the formation of voidites in diamond , 2000 .

[52]  D. Phillips,et al.  A petrographic and 40 Ar/ 39 Ar geochronological study of the Voorspoed Kimberlite, South Africa; implications for the origin of Group II kimberlite magmatism , 1998 .

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

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

[55]  R. S. White Mantle plume origin for the Karoo and Ventersdorp flood basalts, South Africa , 1997 .

[56]  W. Taylor,et al.  The influence of the Glennie Domain deep structure on the diamonds in Saskatchewan kimberlites , 1997 .

[57]  J. Dawson,et al.  Equilibration and reaction in Archaean quartz‐sapphirine granulite xenoliths from the Lace kimberlite pipe, South Africa , 1997 .

[58]  G. Woods,et al.  Infrared absorption by the B nitrogen aggregate in diamond , 1995 .

[59]  G. van Tendeloo,et al.  Conversion of platelets into dislocation loops and voidite formation in type IaB diamonds , 1995, Proceedings of the Royal Society of London. Series A: Mathematical and Physical Sciences.

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

[61]  G. Woods,et al.  The relationship between infrared absorption and the A defect concentration in diamond , 1994 .

[62]  P. Deines,et al.  Depth-related carbon isotope and nitrogen concentration variability in the mantle below the Orapa kimberlite, Botswana, Africa , 1993 .

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

[64]  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 .

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

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

[67]  D. J. Schulze,et al.  Constraints on the abundance of eclogite in the upper mantle , 1989 .

[68]  E. J. Krogh The garnet-clinopyroxene Fe-Mg geothermometer — a reinterpretation of existing experimental data , 1988 .

[69]  J. V. Smith,et al.  Reduced sapphirine granulite xenoliths from the Lace Kimberlite, South Africa; implications for the deep structure of the Kaapvaal Craton , 1987 .

[70]  E. Skinner Contrasting Group 1 and Group 2 kimberlite petrology: Towards a genetic model for kimberlites , 1986 .

[71]  G. Woods Platelets and the infrared absorption of type Ia diamonds , 1986, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

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

[73]  T. Kusky,et al.  Is the Ventersdorp Rift System of Southern Africa related to a continental collision between the Kaapvaal and Zimbabwe Cratons at 2.64 Ga ago , 1985 .

[74]  J. Harris,et al.  Silicate and Oxide Inclusions in Diamonds from the Orapa Mine, Botswana. , 1984 .

[75]  T. Evans,et al.  The kinetics of the aggregation of nitrogen atoms in diamond , 1982, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

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

[77]  D. Robinson Surface textures and other features of diamonds , 1979 .

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

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

[80]  A. F. Williams Genesis of the Diamond , 1898, The American Naturalist.