ORTHOPYROXENE-GARNET GEOTHERMOMETER. EXPERIMENTS AND THEORETICAL EVALUATION OF THE DATA BASE

dc.contributor.author	Lavrentyeva I.V.
dc.contributor.author	Perchuk L.L.
dc.date.accessioned	2020-11-02T00:32:31Z
dc.date.available	2020-11-02T00:32:31Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31153508
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 122-125
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18372
dc.description.abstract	Control experiments were run at 700°C and 30 kb on a UTF-40 in silver-palladium ampoules. The starting materials were natural amphibole and garnet, as well as mixtures of oxides, oxalates, hydroxides and NaAlO2. Equilibrium phase compositions were determined with the microprobe by the earlier developed method of tracing the evolution of compositional heterogeneities in minerals during the experiment. Examples of the orthopyroxene-garnet equilibrium are shown and the experimental results are presented. They are processed in thermodynamic terms together with the published experimental data base on the orthopyroxene-garnet equilibrium. Study results are discussed.
dc.title	ORTHOPYROXENE-GARNET GEOTHERMOMETER. EXPERIMENTS AND THEORETICAL EVALUATION OF THE DATA BASE
dc.type	Статья

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