UB-N-P

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description
Serpentinites are formed during subduction of oceanic crust and can give insights to processes occurring, when the crust meets the mantle.
origin
Serpentinite from the Col des Bagnelles in the Vosges Mountains, France
sourceProducer
CNRS-CRPG
characteristics

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

LILE (Rb, Sr, K, Ba): 4.00 - 166 µg/g.

HFSE (Zr, Hf, Th, U, Nb, Ta) 0.02-13 µg/g.

Transition metals (Sc, V, Cr, Co, Ni, Cu, Zn) 0.3-55.0 µg/g.

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

Diagrams