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Petrology and retrograde P‐T path in granulites of the Kanskaya formation, Yenisey range, Eastern Siberia
Author(s) -
PERCHUK LEONID,
GERYA TARAS,
NOZHKIN ALEX
Publication year - 1989
Publication title -
journal of metamorphic geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.639
H-Index - 114
eISSN - 1525-1314
pISSN - 0263-4929
DOI - 10.1111/j.1525-1314.1989.tb00621.x
Subject(s) - sillimanite , geology , granulite , cordierite , geochemistry , metamorphism , biotite , plagioclase , quartz , mineralogy , facies , geomorphology , paleontology , biochemistry , chemistry , structural basin , catalysis
The Kanskaya formation in the Yenisey range, Eastern Siberia is a newly studied example of retrogression of granulite facies rocks. The formation consists of two stratigraphical units: the lower Kuzeevskaya group and the upper Atamanovskaya group. Rocks from both of these units show rare reaction textures such as replacement of cordierite by garnet, sillimanite and quartz, silimanite coronas around spinel and corundum, and garnet rims around plagioclase in metabasites, while plagioclase rims around garnet can be seen in associated metapelites. The paragenesis quartz + orthopyroxene + sillimanite is a feature of the Kuzeevskaya group. In many samples, chemical zoning of garnet and cordierite shows an increase in Mg from core to rim as well as the reverse. Biotite‐garnet‐cordierite‐sillimanite‐quartz as well as spinel±biotite‐garnet°Cordierite±sillimanite‐quartz assemblages were studied using geothermometers and geobarometers based on both exchange and net‐transfer reactions (Perchuk & Lavrent'eva, 1983; Aranovich & Podlesskii, 1983; Gerya & Perchuk, 1989). Detailed investigation of 10 samples including 1000 microprobe analyses revealed decompression (first stage) followed by the near isobaric cooling of the granulites. From geological studies, the 7 km total thickness of the sequence closely corresponds to the pressure difference (∼ 2.2kbar) measured by geobarometers in the samples taken from different levels in the sequence. Individual samples yield P‐T paths ranging from 100°C/kbar to 140°C/kbar depending on their locations with respect to the large Tarakskiy granite pluton. In places the 100°C/kbar path changed to the 140°C/kbar due to the influence of the intrusion. In a P‐T diagram these trajectories are subparallel lines, whose P‐T maxima define the Archaean geotherm between 3.1 and 2.7 Ga, determined isotopically. A petrological model for P‐T evolution of the Kanskaya formation is proposed.