Mantle composition, age and geotherm beneath the Darby kimberlite field, west central Rae Craton

[1]  B. Kjarsgaard,et al.  Geochronology, classification and mantle source characteristics of kimberlites and related rocks from the Rae Craton, Melville Peninsula, Nunavut, Canada , 2018, Mineralogy and Petrology.

[2]  D. Pearson,et al.  Statistical approaches to the discrimination of mantle- and crust-derived low-Cr garnets using major and trace element data , 2018, Mineralogy and Petrology.

[3]  D. Pearson,et al.  Statistical approaches to the discrimination of crust- and mantle-derived low-Cr garnet – Major-element-based methods and their application in diamond exploration , 2018 .

[4]  S. Regan,et al.  Neoarchean arc magmatism and subsequent collisional orogenesis along the eastern Rae domain, western Churchill Province: Implications for the early growth of Laurentia , 2017 .

[5]  B. Kjarsgaard,et al.  The aluminum-in-olivine thermometer for mantle peridotites — Experimental versus empirical calibration and potential applications , 2017 .

[6]  D. Snyder,et al.  Construction and destruction of some North American cratons , 2017 .

[7]  D. Pearson,et al.  Making Archean cratonic roots by lateral compression: A two-stage thickening and stabilization model , 2016, Tectonophysics.

[8]  W. Griffin,et al.  Cr-rich rutile: A powerful tool for diamond exploration , 2016 .

[9]  M. Pilkington,et al.  The 3‐dimensional construction of the Rae craton, central Canada , 2015 .

[10]  L. Heaman,et al.  Duration and periodicity of kimberlite volcanic activity in the Lac de Gras kimberlite field, Canada and some recommendations for kimberlite geochronology , 2015 .

[11]  D. Bosch,et al.  Fractionation of highly siderophile elements in refertilized mantle: Implications for the Os isotope composition of basalts , 2014 .

[12]  R. Berman,et al.  Neoarchean continental crust formation and Paleoproterozoic deformation of the central Rae craton, Committee Bay belt, Nunavut , 2014 .

[13]  A. Gerdes,et al.  Geochronological and geochemical constraints on the formation and evolution of the mantle underneath the Kaapvaal craton: Lu-Hf and Sm-Nd systematics of subcalcic garnets from highly depleted peridotites , 2013 .

[14]  R. Berman,et al.  The Arrowsmith orogeny: Geochronological and thermobarometric constraints on its extent and tectonic setting in the Rae craton, with implications for pre-Nuna supercontinent reconstruction , 2013 .

[15]  Fuat Yavuz,et al.  WinPyrox: A Windows program for pyroxene calculation classification and thermobarometry , 2013 .

[16]  D. Jacob,et al.  Minor and trace elements in olivines as probes into early igneous and mantle melting processes , 2013 .

[17]  K. Priestley,et al.  Constraints on the depth and thermal history of cratonic lithosphere from peridotite xenoliths, xenocrysts and seismology , 2011 .

[18]  H. Grütter.  Pyroxene xenocryst geotherms: Techniques and application , 2009 .

[19]  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 .

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

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

[22]  R. Romer,et al.  Mediterranean Tertiary lamproites derived from multiple source components in postcollisional geodynamics , 2008 .

[23]  R. Creaser,et al.  Queen Maud block: A newly recognized Paleoproterozoic (2.4-2.5 Ga) terrane in northwest Laurentia , 2007 .

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

[25]  R. Creaser,et al.  Ancient (Meso- to Paleoarchean) crust in the Rae Province, Canada: Evidence from Sm–Nd and U–Pb constraints , 2005 .

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

[27]  R. Creaser,et al.  Macrocrystal phlogopite Rb–Sr dates for the Ekati property kimberlites, Slave Province, Canada: evidence for multiple intrusive episodes in the Paleocene and Eocene , 2004 .

[28]  Dorrit E. Jacob.  Nature and origin of eclogite xenoliths from kimberlites , 2004 .

[29]  G. Dreibus,et al.  Re-Os isotope systematics and platinum group element fractionation during mantle melt extraction: a study of massif and xenolith peridotite suites , 2004 .

[30]  G. Dreibus,et al.  A Re–Os isotope and PGE study of kimberlite-derived peridotite xenoliths from Somerset Island and a comparison to the Slave and Kaapvaal cratons , 2003 .

[31]  A. Menzies.  Re–Os systematics of diamond-bearing eclogites from the Newlands kimberlite , 2003 .

[32]  D. Jacob,et al.  Trace element geochemistry of coesite-bearing eclogites from the Roberts Victor kimberlite, Kaapvaal craton , 2003 .

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

[34]  T. Andersen.  Correction of common lead in U-Pb analyses that do not report 204Pb , 2002 .

[35]  P. Nimis,et al.  Single clinopyroxene thermobarometry for garnet peridotites. Part I. Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer , 2000 .

[36]  D. Cherniak.  Pb diffusion in rutile , 2000 .

[37]  D. Pearson.  Solvent extraction/anion exchange separation and determination of PGEs (Os, Ir, Pt, Pd, Ru) and Re-Os isotopes in geological samples by isotope dilution ICP-MS , 2000 .

[38]  Krogh Ravna.  The garnet–clinopyroxene Fe2+–Mg geothermometer: an updated calibration , 2000 .

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

[40]  M. Bostock.  Mantle stratigraphy and evolution of the Slave province , 1998 .

[41]  H. G. David,et al.  Reactions between eclogite and peridotite; mantle refertilisation by subduction of oceanic crust , 1998 .

[42]  B. Harte,et al.  Partitioning of trace elements between clinopyroxene and garnet: data from mantle eclogites , 1997 .

[43]  J. Gurney,et al.  The interpretation of the major element compositions of mantle minerals in diamond exploration , 1995 .

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

[45]  P. H. Nixon,et al.  Geochemical constraints on the petrogenesis of diamond facies pyroxenites from the Beni Bousera Peridotite Massif, North Morocco , 1993 .

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

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

[48]  P. M. Jackson,et al.  Age of mineral equilibria in granulite facies nodules from kimberlites , 1981, Nature.

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

[50]  G. D. Jackson.  Geology and mineral possibilities of the Mary River region, northern Baffin Island , 1966 .

[51]  B. Kjarsgaard,et al.  Age and evolution of the deep continental root beneath the central Rae craton, northern Canada , 2016 .

[52]  D. Pearson,et al.  Distribution and Processing of Highly Siderophile Elements in Cratonic Mantle Lithosphere , 2016 .

[53]  D. Pearson,et al.  3.6 – The Formation and Evolution of Cratonic Mantle Lithosphere – Evidence from Mantle Xenoliths , 2014 .

[54]  R. P. Hartlauba,et al.  Ancient (Meso- to Paleoarchean) crust in the Rae Province, Canada: Evidence from Sm–Nd and U–Pb constraints , 2005 .

[55]  S. Hoernes,et al.  Anorthositic oceanic crust in the Archean Earth , 1985 .

[56]  M. Schau.  Geology of the Prince Albert Group in parts of Walker Lake and Laughland Lake map areas, District of Keewatin , 1982 .