Published December 1998 | Version v1
Journal article Metadata-only

Determination of Iron Oxidation State in Omphacites Applied to Geothermometry of Sudetic Eclogites

Creators

  • 1. Warsaw University of Technology, Institute of Physics (Poland)
  • 2. The Hebrew University, Racah Institute of Physics (Israel)

Description

A common mineral geothermometer for eclogites is based on Fe2+-Mg exchange reaction between garnets and clinopyroxenes. For the accurate determination of Fe2+ in omphacites, ten omphacite samples were isolated from eight Sudetic eclogites and studied by electron microprobe and Moessbauer spectroscopy. Garnet-clinopyroxene equilibration temperatures for two Sudetic eclogites were calculated

Additional details

Identifiers

DOI
10.1023/A:1010846323948;

Publishing Information

Journal Title
Hyperfine Interactions
Journal Volume
112
Journal Issue
1-4
Journal Page Range
p. 223-226
ISSN
0304-3843
CODEN
HYINDN

INIS

Country of Publication
Netherlands
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
40058565
Subject category
S54: ENVIRONMENTAL SCIENCES;
Descriptors DEI
ELECTRON MICROPROBE ANALYSIS; GARNETS; GEOTHERMOMETERS; GEOTHERMOMETRY; IRON; IRON IONS; MOESSBAUER EFFECT; VALENCE
Descriptors DEC
CHARGED PARTICLES; CHEMICAL ANALYSIS; ELEMENTS; IONS; MEASURING INSTRUMENTS; METALS; MICROANALYSIS; MINERALS; NONDESTRUCTIVE ANALYSIS; SILICATE MINERALS; THERMOMETERS; TRANSITION ELEMENTS

Optional Information

Copyright
Copyright (c) 1998 Kluwer Academic Publishers