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Geochemical evolution of amphibolites and gneisses of the Belomorian mobile belt during Paleoproterozoic metamorphism
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Geochemical evolution of amphibolites and gneisses of the Belomorian mobile belt during Paleoproterozoic metamorphism
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Geochemical evolution of amphibolites and gneisses of the Belomorian mobile belt during Paleoproterozoic metamorphism
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Journal Article
Geochemical evolution of amphibolites and gneisses of the Belomorian mobile belt during Paleoproterozoic metamorphism
2016
Overview
We present the results of a comparative study of the geochemical changes of amphibolites and gneisses from the Belomorian mobile belt in response to plagiomigmatization, high-pressure metamorphism, two-feldspar migmatization, and secondary amphibolization during Paleoproterozoic (Svecofennian) tectonometamorphic activation. It is established that most of the Paleoproterozoic metamorphic processes are nonisochemical for major and trace elements, which is possibly caused by the interaction of protolithic rocks with metamorphic fluids. The finds of eclogites within the Belomorian mobile belt are spatially and genetically related to the large fields of apoamphibolite and apogneiss plagiomigmatites. Apoamphibolite eclogites,
Grt–Aug
eclogite-like rocks, apoamphibolite and apogneiss plagiomigmatites were formed by a single process initiated by the influence of an alkaline fluid on the amphibolite–gneiss complex. This was accompanied by the depletion of the rocks in HREE, enrichment in LREE, disappearance of the negative and formation of the positive europium anomaly. The formation of later two-feldspar migmatites was related to the reworking of the gneiss–migmatite–amphibolite complex by more acid fluids, which led to the depletion of microclinized rocks in LREE. Secondary amphibolization and epidotization of the basites and metabasites did not affect their REE distribution pattern.
