Publication Type:Journal Article
Source:The Canadian MineralogistThe Canadian Mineralogist, Mineralogical Association of Canada, Ottawa, ON, Canada, Volume 55, Number 4, p.561-593 (2017)
Keywords:B-11/B-10, beryl, boron, Canada, chemical composition, D/H, emerald, fluid phase, gems, granites, hydrogen, igneous rocks, isotope ratios, Isotopes, metal ores, Metamorphic rocks, metasomatic rocks, mineral composition, mineral deposits, genesis, mineralization, monzonites, northwest territories, O-18/O-16, oxygen, plutonic rocks, quartz veins, ring silicates, Selwyn Basin, silicates, skarn, Stable isotopes, tungsten ores, veins, Western Canada
Emerald at the Lened occurrence in the western Northwest Territories is hosted by quartz veins cutting skarn near the Lened granite pluton and older Selwyn Basin strata. Euhedral beryl crystals (<0.5 X 5 cm) are present in approximately half of the 26 outcropping veins. Most of the crystals are opaque to translucent and colorless to yellowish and grassy green. Less than 5% of the beryl is transparent, bluish green, and can be considered pale emerald. Using field relationships, Ar-Ar dating, whole-rock geochemistry, stable isotopes (O, H, C, and B), and mineral chemistry, the sources of the emerald-forming fluids and chromophores have been assessed; the results clearly show that the ca 100 Ma (Ar-Ar muscovite) Lened emerald occurrence is a Type I (igneous) skarn-hosted emerald deposit related to the proximal ca 100 Ma (Ar-Ar biotite) Lened pluton. Beryllium and other incompatible elements (i.e., W, Sn, Li, B, and F) in the emerald, vein minerals, and surrounding skarn were derived during the terminal stages of crystallization of the proximal Lened pluton. Decarbonation during pyroxene-garnet skarn formation in the host carbonate rocks probably caused local overpressuring and fracturing that allowed ingress of magmatic-derived fluids and formation of quartz-calcite-beryl-scheelite-tourmaline-pyrite veins. Channel-water delta D values in emerald are depleted and range between -87.4 ppm and -62 ppm, similar to other granite-related emerald occurrences. The calculated delta (super 18) O (sub H2O) for the vein fluid ( approximately 10 ppm, vein quartz, 350 degrees C) is compatible with a peraluminous granitic fluid source. The calculated delta (super 18) O (sub H2O) of granite-derived fluids ( approximately 12 ppm; magmatic quartz, 600-700 degrees C) is slightly isotopically heavier than the vein fluid, which can be explained by fractionation during vein crystallization or mixing with (super 18) O-depleted meteoric fluid. The delta (super 11) B values of accessory dravite in the emerald veins averages -4.9 + or - 0.3 ppm (1sigma , n = 10), which is compatible with a magmatic source, and the Al-Fe-Mg composition is that of tourmaline formed in sedimentary environments, with Mg likely derived from metasomatism of local marine carbonates. The vein fluid was largely igneous in origin, but the dominant emerald chromophore V (emerald vein = avg. 1560 ppm V versus 75 ppm Cr) was mobilized by metasomatism of V-rich sedimentary rocks (avg. 2000 ppm V) that underlie the emerald occurrence. Lened is a unique igneous skarn-hosted emerald occurrence that contributes to the understanding of emerald deposits and emerald exploration criteria in Canada and globally.
GeoRef, Copyright 2018, American Geological Institute.<br/>2017-068811<br/>Lened Pluton<br/>Logan Mountains