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Article
Lu–Hf Isotope-Geochemical Zircon Systematics and Genesis of the Neoarchean Alkaline Granites in the Keivy Megablock, Kola Peninsula
Abstract—Alkaline and subalkaline granites of the Keivy megablock belong to the potassic alkali-calcic ferroan rocks enriched in large-ion lithophile, high-field strength and rare-earth elements. Based on these c...
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Article
Sites and Origin of Noble Gases in Minerals: A Case Study of Amphibole from Alkaline Granitoids of the Kola Peninsula
The paper presents newly acquired data on the budget and mobility of isotopes of noble gases in samples of amphibole, a mineral commonly characterized by relatively high He concentrations compared to other roc...
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Article
Trace element composition and Lu-Hf isotope systematics of zircon from plagiogneisses of the Kola superdeep well: Contribution of a Paleoarchean crust in Mesoarchean metavolcanic rocks
Zircons have been studied in three samples of Archean plagiogneisses from the Kola superdeep well (SG-3). The crystals consist of cores, magmatic shells, and metamorphic rims. The cores and shells are characte...
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Article
Residence sites and origin of noble gases in minerals as exemplified by ilmenite from the alkaline granites of the Kola Peninsula
Thermal analysis of helium release from ilmenite of alkaline granites (Ponoy Massif, Kola Peninsula) and extraction of gases by crushing, melting and vacuum stepwise heating of sample revealed that this mineral c...
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Article
Duration of the formation and sources of the granitoids of the Litsk-Araguba Complex, Kola Peninsula
Postorogenic granitoids of the Litsk-Araguba Complex compose a chain of intrusive bodies around 850 km2 in area, which are confined to the NE-trending deep-seated fault zone. Results of U-Pb zircon dating indicat...
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Article
Deep structure and crustal growth of the northeastern Baltic shield
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Article
Geology and geochronology of neoarchean anorogenic magmatism of the Keivy structure, Kola Peninsula
Anorogenic magmatic complexes were formed during protoplatformal evolution of the Keivy structure. This evolution ended with development of aluminous schists, which were derived by deep disintegration and rede...
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Article
Sm-Nd systematics and petrology of postorogenic granitoids in the northern Baltic Shield
In the northern part of the Baltic Shield, quartz diorites, diorites, and monzodiorites compose massifs of postorogenic granites, in which younger granite phases are restricted to their central parts, and dike...
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Article
Helium and argon isotopes in lower crustal xenoliths from the belomorian mobile belt
The isotopic systematics of noble gases (He and Ar) were studied in Neoarchean and Paleoproterozoic lower crustal xenoliths from the Belomorian mobile belt. The xenolith suite is dominated by garnet granulites (G...
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Article
Composition and structure of the lower crust of the Belomorian Mobile Belt, Baltic Shield
The lower crust of the Belomorian Mobile Belt consists predominantly of garnet peridotites with subordinate amounts of pyroxenites and spinel peridotites, which occur as xenoliths in Devonian diatremes and dik...