OKUM-P

Cookie Policy

This page uses cookies for statistical purposes. With clicking on "Agree" you allow us to set this cookie and collect anonymized data. For more information or to change this behaviour click on "Adjust."

Privacy Policy

Profile

description
Komatiites are presently no longer formed on Earth. This reference material gives a window into the very beginnings of our planet.
origin
Komatiite from Serpentine Mt. in McArthur Township, Ontario Canada
sourceProducer
IAG
characteristics

Highly depleted in most trace elements, except for transition metals.

LILE (Rb, Sr, K, Ba): 1.00 - 365 µg/g.

HFSE (Zr, Hf, Th, U, Nb, Ta) 0.012 - 17 µg/g.

Transition metals (Sc, V, Cr, Co, Ni, Cu, Zn) 27.9 - 2460 µg/g.

suitable for
  • LA-ICP-MS
  • XRF
  • µXRF
  • LIBS
original certificate of analysis Link

Diagrams