Аннотация:The paper series titled “Combined processes ofeclogite-glaucophane schist formation” describesinterconnected processes of metamorphic and metasomaticevolutions of the two crustal mafic eclogite complexes.Petrologic and petrochemical data on relatively deepMaksyutov (Southern Urals) rocks were discussed in thefirst part. This paper presents the results of study of theAtbashi complex formed under moderate pressure.Progressive thermobaric processes yield PT parameters offormation of the contrasting rock series - high-pressureeclogite boudins, blocks, interlayers and lenses within thelow metamorphism gneiss and schist matrix. Theregressive metamorphic stage is combined withmetasomatic processes resulting in the change of bulkchemical composition, causing mineral reactions,dissolution and redeposition of mineral components.Coherent combination of these processes results in thecomplete formation of eclogite-glaucophane schistcomplexes.
