Ukrainian Antarctic Journal

No 2 (2004): Ukrainian Antarctic Journal
Articles

Rotational rifting in Antarctica

V. P. Kobolev
S. I. Subbotin Institute of Geophysics of NAS of Ukraine, Kyiv
Yu. P. Orovetsky
S. I. Subbotin Institute of Geophysics of NAS of Ukraine, Kyiv
Published December 15, 2004
Keywords
  • Antarctica,
  • rotational rifting,
  • multimagmatogene
How to Cite
Kobolev, V. P., & Orovetsky, Y. P. (2004). Rotational rifting in Antarctica. Ukrainian Antarctic Journal, (2), 73-81. https://doi.org/10.33275/1727-7485.2.2004.599

Abstract

The rotational rifting as a consequence of the rotational Earth’s movement is accompanied by the formation of the planetary equatorial deep separations. Their repeated and no simultaneous intersections of the Antarctica ancient mother crystal had led to the origin of the large-scale spreading area with the synchronous formation of the deep multimagmatogene. This had been completed by the continent formation that transformed into the ancient platform.

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