Am. Ghazi et al., DETERMINATION OF RARE-EARTH ELEMENTS IN FLUID INCLUSIONS BY INDUCTIVELY-COUPLED PLASMA-MASS SPECTROMETRY (ICP-MS), Geochimica et cosmochimica acta, 57(18), 1993, pp. 4513-4516
An inductively coupled plasma-mass spectrometer (ICP-MS) is used to de
termine rare ear-th element (REE) abundances in fluid inclusions. Quar
tz concentrates from the Bingham porphyry Cu-Mo deposit, Utah, USA, an
d from a quartz vein in brecciated amphibolite dredged from the Mathem
atician Ridge, an abandoned spreading center in the eastern Pacific, w
ere prepared by a modified crush-leach method. Leachates and solutions
from acid digestion of quartz residue from leaching were analyzed by
ICP-MS, using conventional sample introduction. The results demonstrat
e that the crush-leach method, followed by ICP-MS analysis of leachate
s, is effective for REE determination. Chondrite-normalized REE patter
ns for the Bingham samples are light rare earth element (LREE) enriche
d, with a small negative Eu anomaly, and the pattern for the Mathemati
cian Ridge sample is nearly flat, with a positive Eu anomaly.