Evolution of high magnesian melts during processes of crystallization of rocks from the ultramafic massifs of the Siberian platform

Cover Page

Abstract


We determined the chemical composition of high-mg picrite-basaltic melts that formed the ultramafic massifs of the Siberian platform in the study of primary melt inclusions in accessory chrome spinel from dunites. We determined the temperature of crystallization of olivine from dunites of the Gulinsky (1520-1420 °C), Kondersky (1545-1430 °C), Inaglinsky (1530-1430 °C), Chadsky (1460-1420 °C) intrusives and chrome spinels of these complexes: Gulinsky (1410-1370 °C), Kondersky (1420-1380 °C), Inaglinsky (up to 1430 °C), Chadsky (1430-1330 °C), using a computer simulation (program PETROLOG and PLUTON) on the basis of data on the composition of the inclusions. Тhe computational modeling allowed us to establish that there were two types of high-magnesium melt evolution on the Siberian platform. The first type is characteristic of the Gulinsky pluton, where there is the following sequence of formation: the dunites → pyroxenites → alkaline rocks. The second type is represented Kondersky massif, where the sequence is different: dunites → kosvites → pyroxenites and olivine-diopside rocks.


About the authors

V. A. Simonov

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Novosibirsk State University

Email: meimech@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090; 1, Pirogova street, Novosibirsk, 630090

Yu. R. Vasiliev

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Novosibirsk State University

Author for correspondence.
Email: meimech@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090; 1, Pirogova street, Novosibirsk, 630090

A. V. Kotlyarov

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: kotlyarov@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

V. S. Prihodko

Institute of Tectonics and Geophysics, Far Eastern Branch of the Russian Academy of Sciences

Email: meimech@igm.nsc.ru

Russian Federation, 65, Kim Yu Chen street, Khabarovsk, 680000

References

  1. Симонов В. А., Приходько В. С., Ковязин С. В. // Петрология. 2011. Т. 19. № 6. С. 579-598.
  2. Соболев Н. В., Логвинова А. М., Николенко Е. И., Лобанов С. С. // Геология и геофизика. 2013. Т. 54. № 8. С. 1162-1178.
  3. Симонов В. А., Васильев Ю. Р., Ступаков С. И., Котляров А. В., Карманов Н. С. // ДАН. 2015. Т. 464. № 3. С. 341-345.
  4. Симонов В. А., Васильев Ю. Р., Ступаков С. И., Котляров А. В., Карманов Н. С. // Геология и геофизика. 2016. Т. 57. № 12. С. 2153-2177.
  5. Соболев А. В. // Петрология. 1996. Т. 4. С. 228-239.
  6. Boynton W. V. Rare Earth Element Geochemistry. L.: Elsevier, 1984. P. 63-114.
  7. Соболев А. В., Соболев С. В., Кузьмин Д. В., Малич К. Н., Петрунин А. Г. // Геология и геофизика. 2009. Т. 50. № 12. С. 1293-1334.
  8. Наумов В. Б., Коваленко В. И., Дорофеева В. А., Гирнис А. В., Ярмолюк В. В. // Геохимия. 2010. № 12. С. 1266-1288.
  9. Norman M. D., Garcia M. O. // Earth and Planet. Sci. Lett. 1999. V. 168. P. 27-44.
  10. Danyushevsky L. V., Plechov P.Yu. // Geochem., Geophys., Geosyst. 2011. V. 12. № 7. Q07021. doi: 10.1029/2011GC003516.
  11. Лавренчук А. В. В сб.: Тез. докл. Второй Сибирской междунар. конф. молодых учёных по наукам о Земле. Новосибирск, 2004. С. 105-106.
  12. Соболев А. В., Каменецкий В. С., Кононкова Н. Н. // Геохимия. 1991. № 8. С. 1084-1095.
  13. Егоров Л. С. Ийолит-карбонатитовый плутонизм. Л.: Недра, 1991. 260 с.
  14. Panina L. I., Motorina I. V. // Geochem. Int. 2013. V. 51. P. 109-128.
  15. Панина Л. И. В кн.: Науки о Земле. М.: Науч. мир, 2006. С. 106-107.

Statistics

Views

Abstract - 72

PDF (Russian) - 78

PlumX


Copyright (c) 2019 Russian academy of sciences

This website uses cookies

You consent to our cookies if you continue to use our website.

About Cookies