Mass balance and compositional variation in the outer part of the contact aureole shows that mass transfer of the main petrogenetic components was confined to small domains of a few hundredths of mm3 in chlorite-biotite-mica and epidote-plagioclase-titanomagnetite aggregates. The chemical homogeneity of the environment was practically unaffected by the thermal metamorphism. -Authors
Likhanov, I., Reverdatto, V., Turbanti, I. (1994). Short-range mobilization of elements during thermal metamorphism of the Kharlovo gabbro aureole. EUROPEAN JOURNAL OF MINERALOGY, 6(1), 133-144 [10.1127/ejm/6/1/0133].
Short-range mobilization of elements during thermal metamorphism of the Kharlovo gabbro aureole
TURBANTI, I.
1994-01-01
Abstract
Mass balance and compositional variation in the outer part of the contact aureole shows that mass transfer of the main petrogenetic components was confined to small domains of a few hundredths of mm3 in chlorite-biotite-mica and epidote-plagioclase-titanomagnetite aggregates. The chemical homogeneity of the environment was practically unaffected by the thermal metamorphism. -Authors
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https://hdl.handle.net/11365/29458
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