PARTITION OF ALUMINA BETWEEN ORTHOPYROXENE AND GARNET IN PLAGIOCLASE-BEARING ROCKS AS A GEOBAROMETER
Author:
Affiliation:
1. a Far East Institute of Geology, Far East Scientific Center , USSR Academy of Sciences , Vladivostok
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206818509466423
Reference12 articles.
1. The solubility of alumina in orthopyroxene coexisting with garnet
2. The Al2O3 contents of enstatite in equilibrium with garnet in the system MgO-Al2O3-SiO2 at 15–40 kbar and 900°–1,600° C
3. Garnet–orthopyroxene barometry for granulites and peridotites
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1. Ferromagnesian silicate association in S-type granites: the Darongshan granitic complex (Guangxi, South China);Bulletin de la Société Géologique de France;2008-01-01
2. Pan-African high pressure isobaric cooling: evidence from the mineralogy and thermobarometry of the granulite-facies rocks from the Uluguru Mountains, eastern Tanzania;Journal of African Earth Sciences;1996-10
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