Skip to main content

previous disabled Page of 2
and
  1. No Access

    Chapter and Conference Paper

    A Change in Composition of Rocks, Mineral Phases and Trapped Gases in The Kola Super-Deep Borehole(SD-3) Section of the Archean Complex with Depth

    A considerable amount of new information about the features of rocks and ore formation at various depths has been obtained due to the investigations carried out by the Geological Institute of the Kola Science ...

    F. P. Mitrofanov, Yu. N. Yakovlev in Super-Deep Continental Drilling and Deep G… (1990)

  2. No Access

    Article

    Mineralogy and geochemistry of Devonian ultramafic minor intrusions of the southern Kola Peninsula, Russia: implications for the petrogenesis of kimberlites and melilitites

    Minor magmatic intrusions of kimberlite, melilitite and cpx-melilitite occur in the southern part of the Kola Peninsula, Russia, on the Terskii Coast and near the town of Kandalaksha. They yield K-Ar ages of ...

    A. D. Beard, H. Downes, E. Hegner in Contributions to Mineralogy and Petrology (1998)

  3. No Access

    Article

    Loihi-like plume component in Devonian Kola ultrabasic-alkaline rocks and carbonatites: Noble gas evidence

    I. N. Tolstikhin, I. L. Kamensky, S. V. Ikorsky, V. A. Nivin in Chinese Science Bulletin (1998)

  4. No Access

    Article

    Composition of melt inclusions and age of zircons from plagiogneisses of the archean complex in the Kola superdeep borehole, Baltic Shield

    V. P. Chupin, V. R. Vetrin, N. V. Rodionov, D. I. Matukov in Doklady Earth Sciences (2006)

  5. No Access

    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...

    V. R. Vetrin in Petrology (2006)

  6. No Access

    Article

    Petrology of postorogenic granitoids of the northern Baltic Shield

    V. R. Vetrin, N. G. Berezhnaya, N. V. Rodionov in Doklady Earth Sciences (2006)

  7. No Access

    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...

    V. R. Vetrin, I. L. Kamenskii, S. V. Ikorskii in Petrology (2007)

  8. No Access

    Article

    Initial subalkaline magmatism of the Neoarchean alkaline province of the Kola Peninsula

    V. R. Vetrin, E. N. Lepekhina, A. N. Larionov, S. L. Presnyakov in Doklady Earth Sciences (2007)

  9. No Access

    Article

    U-Pb age and genesis of granitoids in the southern framing of the Pechenga structure, Baltic Shield

    V. R. Vetrin, O. M. Turkina, N. V. Rodionov in Doklady Earth Sciences (2008)

  10. No Access

    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...

    V. R. Vetrin, N. V. Rodionov in Geochemistry International (2008)

  11. No Access

    Article

    Stages of the lower crust formation of the Belomorian mobile belt, Kola Peninsula

    V. R. Vetrin, E. N. Lepekhina, I. P. Paderin, N. V. Rodionov in Doklady Earth Sciences (2009)

  12. No Access

    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...

    V. R. Vetrin, N. V. Rodionov in Petrology (2009)

  13. No Access

    Article

    Deep structure and crustal growth of the northeastern Baltic shield

    V. R. Vetrin in Geochemistry International (2011)

  14. No Access

    Article

    Sources of terrigenous material in formation of metasedimentary rocks of the archean complex cored by the Kola superdeep borehole

    The basement of the Paleoproterozoic Pechenga structure was cored by the Kola superdeep borehole SD-3 at the depths of 6842–12 262 m. It consists mainly of alternating strata of metavolcanic daciteplagiorhyoda...

    V. R. Vetrin, V. P. Chupin, Yu. N. Yakovlev in Doklady Earth Sciences (2011)

  15. No Access

    Article

    Archean rock homologs in the Kola superdeep borehole section in the northern part of the White Sea mobile belt, Voche-Lambina test site

    The Archean Complex homologs of the Kola superdeep borehole (SG-3) were identified in the northern part of the White Sea mobile belt. Tonalite-trondhjemite-granodiorite gneisses of the Voche-Lambina test site ...

    L. N. Morozova, F. P. Mitrofanov, T. B. Bayanova, V. R. Vetrin in Doklady Earth Sciences (2012)

  16. No Access

    Article

    Elastic-anisotropic properties of garnet granulites from the lower crust of the belomorian mobile belt: Results of experimental study

    The elastic-anisotropic properties of fifteen samples of garnet granulites from xenoliths in the diatreme on Elovyi Island, in Kandalaksha Bay in the White Sea are investigated. The PT-conditions of the formation...

    F. F. Gorbatsevich, V. R. Vetrin, O. M. Trishina in Izvestiya, Physics of the Solid Earth (2012)

  17. No Access

    Article

    Duration of the formation and sources of matter for post-orogenic granitoids of the Litsa-Araguba Complex, Kola Peninsula

    V. R. Vetrin, P. A. Serov in Doklady Earth Sciences (2012)

  18. No Access

    Article

    Age, Sm-Nd systematics, and geochemistry of tonalite-trondhjemite-granodiorite gneisses of the northern part of the Baltic Shield

    V. R. Vetrin, N. V. Rodionov, P. A. Serov in Doklady Earth Sciences (2013)

  19. No Access

    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...

    V. R. Vetrin in Geochemistry International (2014)

  20. No Access

    Article

    The model of the depth variations in the properties and state of the rocks in the upper, middle, and lower continental crust of the Kola-Norwegian block, Kola Peninsula

    Based on the experimental and calculated data, the model of depth variations in density, as well as the velocities of longitudinal (P) and transverse (S) waves, within the upper, middle, and lower crusts of the K...

    F. F. Gorbatsevich, V. R. Vetrin, O. M. Trishina in Izvestiya, Physics of the Solid Earth (2014)

previous disabled Page of 2