In addition to the elaboration of monomineral isotopic geothermometers, the combination of intra- and inframineral studies of oxygen isotope distribution is one important application of the intrastructural isotopic method in genetic mineralogy and geochemistry, which allows us to specify the formation conditions of mineral assemblages and to clarify the mineral-formation mechanisms.

Original languageEnglish
Pages (from-to)533-534
Number of pages2
JournalGeokhimiya
Volume35
Issue number5
StatePublished - 1997

    Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

ID: 9332717