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- W2000671027 abstract "The temperature at which organic substance begins to burn, i.e., the exothermal effect in the thermograms, is found to represent directly the degree of recrystallization of organic substance of the rock, which in turn represents the degree of regional metamorphism, namely: epigenesis, 360-400°C; slate-schist, 440°C; beginnings of progressive zonal regional metamorphism: in muscovite-chlorite rocks, 440-550°C; in biotite-chlorite zone, up to 650°C; in andalusite-staurolite zone, up to 700-740°C." @default.
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- W2000671027 date "1971-11-01" @default.
- W2000671027 modified "2023-09-26" @default.
- W2000671027 title "Thermographic expression of the level of metamorphism of carbonaceous rocks, as in western Uzbekistan" @default.
- W2000671027 doi "https://doi.org/10.1080/00206817109475632" @default.
- W2000671027 hasPublicationYear "1971" @default.
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