All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Genesis of emerald at Lened, NWT

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F17%3A00120381" target="_blank" >RIV/00216224:14310/17:00120381 - isvavai.cz</a>

  • Result on the web

    <a href="https://numerique.banq.qc.ca/patrimoine/details/52327/3081324?docref=gK2VAH3sH8YmdLGneE9jRw" target="_blank" >https://numerique.banq.qc.ca/patrimoine/details/52327/3081324?docref=gK2VAH3sH8YmdLGneE9jRw</a>

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Genesis of emerald at Lened, NWT

  • Original language description

    The sources of emerald-forming fluids and chromophores at the Lened occurrence were assessed using field relationships, Ar-Ar dating, whole rock geochemistry, stable isotopes (O, C, S), and mineral chemistry; the results clearly show that the similar to 100 Ma (Ar-Ar muscovite) Lened emerald occurrence is a Type I (igneous) emerald deposit and relates to the proximal similar to 100 Ma (Ar-Ar biotite) Lened Pluton. Stable isotope analyses suggest the veins formed from a primarily granite-derived fluid with lesser components of meteoric and shale-equilibrated fluids. Beryllium and other incompatible elements (including W, Sn, and F) concentrated in evolved magmatic fluid that exsolved during the last stages of crystallization of the Lened pluton. Local overpressuring of vein-forming fluids under a brittle carapace of early pyroxene-garnet skarn led to fracture and emplacement of quartz-calcite-beryl-scheelite-tourmaline-pyrite veins. Less than 5% of the beryl can be considered pale bluish green emerald. Vanadium concentration in the emerald averages 1563 ppm; Cr averages 75 ppm, and Sc attains concentrations of 782 ppm. The key emerald chromophore vanadium was mobilized by metasomatic breakdown of V-rich black shales (averaging 2000 ppm V) that underlie the emerald occurrence.

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

  • OECD FORD branch

    10504 - Mineralogy

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2017

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Article name in the collection

    MINERAL RESOURCES TO DISCOVER, VOLS 1-4

  • ISBN

    9782981689801

  • ISSN

  • e-ISSN

  • Number of pages

    4

  • Pages from-to

    1471-1474

  • Publisher name

    Society for Geology Applied to Mineral Deposits

  • Place of publication

    GENEVA

  • Event location

    Quebec City, CANADA

  • Event date

    Aug 20, 2017

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article

    000439764100364