Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Résumé Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by McLean, H. Articles by Stachel, T. Search for Related Content GeoRef GeoRef Citation

GARNET XENOCRYSTS FROM THE DIAVIK MINE, NWT, CANADA: COMPOSITION, COLOR, AND PARAGENESIS

Hayley McLean¹, Anetta Banas¹, Steven Creighton¹, Sean Whiteford², Robert W. Luth^3, and Thomas Stachel³

¹ Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada
² Diavik Diamond Mines Inc., 5007 50^th Avenue, Yellowknife, Northwest Territories X1A 2P8, Canada
³ Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada

E-mail address:: robert.luth{at}ualberta.ca

Recently sampled mantle-derived xenoliths from the A154–S kimberlite pipe, at the Diavik diamond mine, Northwest Territories, Canada, are dominantly eclogitic in paragenesis, suggesting that either the abundance of eclogite at depth exceeds that of peridotite, or that eclogite is sampled or preserved preferentially. To determine the relative abundance of eclogite and peridotite sampled by the ascending kimberlite more accurately and to evaluate the utility of color alone as a guide to composition, we studied xenocrysts of garnet recovered from coarse heavy-mineral concentrates. Over 10,000 garnet crystals were divided into 15 groups according to their color. From these groups, 174 crystals were analyzed for major and minor elements using an electron microprobe (WDS). Concentrations of trace elements of 55 garnet xenocrysts were measured by LA–ICP–MS. Orange xenocrysts have <1 wt.% Cr₂O₃, and are classified as having an eclogitic derivation according to two sets of criteria. Pink, red, and purple xenocrysts contain >2 wt.% Cr₂O₃, and are inferred to have a peridotitic derivation. The range of Cr content of purple xenocrysts extends to higher values (~14 wt.% Cr₂O₃) than do those of pink (~10 wt.%) or red crystals (~9 wt.%). Orange-red and red-orange xenocrysts have Cr concentrations overlapping those of the orange and red groups, and may be either eclogitic or peridotitic. Chondrite-normalized REE (REE_N) patterns are either "normal", with low LREE_N, increasing concentrations into the MREE_N, and relatively flat HREE at ~10–30x chondrite, or sinusoidal, with normalized concentrations increasing from La to Nd, decreasing from Nd to Ho, and then increasing again to Lu. "Normal" patterns are typical of orange and orange-red xenocrysts, although some show a LREE enrichment. The sinusoidal patterns are characteristic of purple and some pink and red xenocrysts. Garnet xenocrysts of pyroxenitic (including eclogitic and websteritic) and peridotitic affinity are sufficiently distinct in color to permit assignment of the >10,000 garnet crystals in our sample to one of the two suites based solely on color. Color alone, however, could not differentiate unambiguously between different peridotitic parageneses. In contrast to the xenolith data, we infer from the relative abundances of the xenocrystic garnet that the A154–S mantle sample is ~96% peridotite.

Keywords: xenocrysts, garnet, color, discriminants, peridotitic paragenesis, eclogitic paragenesis, kimberlite pipe, Diavik diamond mine, Northwest Territories.