The influence of Fe3+ on garnet–orthopyroxene and garnet–olivine geothermometers-Reference-Cited by-同舟云学术

The influence of Fe3+ on garnet–orthopyroxene and garnet–olivine geothermometers

Published:2014-02 Issue:2 Volume:167 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Matjuschkin Vladimir,Brey Gerhard P.,Höfer Heidi E.,Woodland Alan B.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-014-0972-z.pdf

Reference23 articles.

1. Berman RG, Koziol AM (1991) Ternary excess properties of grossular–pyrope–almandine garnet and their influence in geothermobarometry. Am Miner 76:1223–1231

2. Brey GP, Köhler T (1990) Geothermobarometry in four-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers. J Pet 31:1353–1378

3. Brey GP, Köhler T, Nickel KG (1990a) Geothermobarometry in four-phase lherzolites. I. Experimental results from 10 to 60 kb. J Pet 31:1313–1352

4. Brey GP, Weber R, Nickel KG (1990b) Calibration of a belt apparatus to 1800°C and 6 GPa. Geophys Res 95:15603–15610

5. Canil D (1999) The Ni-in-garnet geothermometer: calibration at natural abundances. Contrib Miner Pet 136:240–246

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