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  1. No Access

    Article

    Oxidation state of the lithospheric mantle beneath Diavik diamond mine, central Slave craton, NWT, Canada

    Oxygen fugacity (fO2) conditions were determined for 29 peridotite xenoliths from the A154-North and A154-South kimberlites of the Diavik diamond mine using the newly developed flank method modified specifically ...

    Steven Creighton, Thomas Stachel… in Contributions to Mineralogy and Petrology (2010)

  2. No Access

    Article

    Diamond formation episodes at the southern margin of the Kaapvaal Craton: Re–Os systematics of sulfide inclusions from the Jagersfontein Mine

    Sulfide inclusions in diamonds from the 90-Ma Jagersfontein kimberlite, intruded into the southern margin of the Kaapvaal Craton, were analyzed for their Re–Os isotope systematics to constrain the ages and pet...

    Sonja Aulbach, Steven B. Shirey… in Contributions to Mineralogy and Petrology (2009)

  3. No Access

    Article

    Oxidation of the Kaapvaal lithospheric mantle driven by metasomatism

    The oxidation state, reflected in the oxygen fugacity (fO2), of the subcratonic lithospheric mantle is laterally and vertically heterogeneous. In the garnet stability field, the Kaapvaal lithospheric mantle becom...

    Steven Creighton, Thomas Stachel… in Contributions to Mineralogy and Petrology (2009)

  4. No Access

    Article

    Diamondiferous peridotitic microxenoliths from the Diavik Diamond Mine, NT

    Twenty-five diamonds recovered from 21 diamondiferous peridotitic micro-xenoliths from the A154 South and North kimberlite pipes at Diavik (Slave Craton) match the general peridotitic diamond production at thi...

    Steven Creighton, Thomas Stachel… in Contributions to Mineralogy and Petrology (2008)