This report presents data on the geological structure and location of the orthopyroxenite inclusion in gneissic enderbites of the Bug granulite–gneiss domain. Three stages of orthopyroxenite formation were identified on the basis of studies of the mineral composition along with the U–Pb and Lu–Hf isotope systems of zircons.

Original languageEnglish
Pages (from-to)700-705
Number of pages6
JournalDoklady Earth Sciences
Volume474
Issue number2
DOIs
StatePublished - 1 Jun 2017

    Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)
  • Earth and Planetary Sciences(all)

ID: 71624954