Geochemistry International

, Volume 51, Issue 1, pp 33–43 | Cite as

Allivalites as indicators of fractional crystallization of the island-arc calc-alkaline low-K series

Article

Abstract

Allivalites are particularly distinguished by their composition and morphology among the wide spectrum of inclusions in the volcanic rocks of the Kurile-Kamchatka island arc. This work reports new chemical and mineral data of a comparative study of the allivalites and host rocks using modern analytical facilities. On the one hand, it was confirmed that allivalites are genetically related with host volcanics. On the other hand, it was established for the first time that allivalites were formed in several stages: from the deepest stage of their origination at the generation depth of primary melts to the crustal and subsurface conditions of the formation of magmatic chamber. Hence, allivalites (olivine-anorthite inclusions) bear valuable information on the evolution of deep island-arc magmatism.

Keywords

allivalites low-K calc-alkaline series plagioclase zoning central-type volcanoes magmatic chamber caldera stage island-arc series fluid regime 

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  1. 1.
    O. N. Volynets, S. A. Shcheka, and Yu. M. Dubik, “Olivine-Anorthite Inclusions in the Kamchatka and Kurile volcanoes, in Inclusions in the Voclanic Rocks of the Kurile-Kamchatka island Arc, Ed. by B. G. Lutts, K. N. Rudich, V. A. Ermakov, (Nauka, Moscow, 1978), pp. 124–166 [in Russian].Google Scholar
  2. 2.
    F. Sh. Kutyev and V. N. Sharapov, Petrogenesis beneath Volcanoes (Nedra, Moscow, 1979) [in Russian].Google Scholar
  3. 3.
    O. B. Selyangin, “Geological Structure and Evolution of the Caldera Complex of Ksudach Volcano,” Vulkanol. Seismol., No. 5, 16–27 (1987).Google Scholar
  4. 4.
    S. I. Dril’, Candidate’s Dissertation in Geology and Mineralogy (Moscow, 1988).Google Scholar
  5. 5.
    T. I. Frolova, D. Bailey, I. A. Burikova, and S. I. Dril’, “Genetic Features of Low-Silica Olivine-Anorthite Inclusions and Host Rocks of the Kurile Island Arc,” Tikhookean. Geol., No. 5, 27–35 (1988).Google Scholar
  6. 6.
    T. I. Frolova, I. A. Burikova, S. I. Dril’, D. K. Bailey, and O. B. Mitreikina, “Nature of Low-Silica Olivine-Anorthite Inclusions and Conditions of their Formation,” Tikhookean. Geol., No. 6, 89–95 (1989).Google Scholar
  7. 7.
    T. I. Frolova and I. A. Burikova, “Role of Calc-Alkaline Volcanism in the Earth’s Crust Formation,” Byul. Mosk. O-va Ispyt. Prir. Otd. Geol. 84(1), 3–17 (2009).Google Scholar
  8. 8.
    V. L. Syvorotkin, “Marginal-Oceanic Faults of the Transition Zone and their Role in the Modern Geological Processes,” in 12th JIQUA Congress, Program and Abstracts, Ottawa, Canada, 1987, (Ottawa, 1987), p. 274.Google Scholar
  9. 9.
    M. Yu. Khotin, S. I. Vinogradov, and O. N. Volynets, “Strontium Isotopic Composition in the Anorthite-Bearing Inclusions of Kamchatka Volcanic Rocks and Basement Rocks,” Dokl. Akad. Nauk SSSR 271(5), 1222–1225 (1983).Google Scholar
  10. 10.
    J. C. Bailey, O. Larsen, and T. I. Frolova, “Strontium Isotope Variation in Lower Tertiary-Quaternary Volcanic Rocks from the Kurile Island Arc,” Contrib. Mineral. Petrol. 95, 155–165 (1987).CrossRefGoogle Scholar
  11. 11.
    T. K. Zlobin, Structure of the Earth’s Crust and Upper Mantle of the Kurile Island Arc: Evidence from Seismic Data (Vladivostok, 1987) [in Russian].Google Scholar
  12. 12.
    T. M. Zlobina, Influence of “Pendulum” Dislocations on the Development of Hydrothermal Ore-Forming Systems in the Volcanic Regions, in Proceedings of 21rst International Conference in Memory of the Academician V.I. Smirnov, Moscow, Russia, 2010) (Mosk. Gos. Univ., Moscow, 2010), p. 193 [in Russian].Google Scholar
  13. 13.
    P. Yu. Plechov, T. A. Shishkina, V. A. Ermakov, M. V. Portnyagin, et al., “Formation Conditions of Allivalites, Olivine-Anorthite Crystal Enclaves, in the Volcanics of the Kuril-Kamchatka Arc,” Petrology 16(3), 248–276 (2008).CrossRefGoogle Scholar
  14. 14.
    T. I. Frolova, P. Yu. Plechov, P. L. Tikhomirov, and V. S. Churakov, “Melt Inclusions in Minerals of Allivalites of the Kuril-Kamchatka Island Arc,” Geochem. Int. 39(4), 336–346 (2001).Google Scholar
  15. 15.
    J. A. Vance, “Zoning in Igneous plagioclase: Normal and Oscillatory Zoning,” Am. J. Sci. 260(10), 746–758 (1962).CrossRefGoogle Scholar
  16. 16.
    J. C. Bailey, T. I. Frolova, and I. A. Burikova, “Mineralogy, Geochemistry and Petrogenesis Island-Arc Basalts,” Contrib. Mineral. Petrol. 102, 265–280 (1989).CrossRefGoogle Scholar
  17. 17.
    J. B. Gill, Orogenic Andesites and Plate Tectonics (Springer Verlag, Berlin, 1981).CrossRefGoogle Scholar
  18. 18.
    J. A. Pearce and J. R. Cann, “Tectonic Setting of Basic Volcanic Rocks Determined Using Trace Element Analyses,” Earth Planet. Sci. Lett. 19, 290–300 (1983).CrossRefGoogle Scholar

Copyright information

© Pleiades Publishing, Ltd. 2013

Authors and Affiliations

  1. 1.Faculty of GeologyMoscow State UniversityMoscowRussia

Personalised recommendations