Tectono-magmatic division of the Late Ordovician (Sandbian) volcanism at the south-western margin of Baltica using immobile trace elements: Relations to the plate movements in the Iapetus Palaeo-Ocean

Research output: Contribution to journalJournal articleResearchpeer-review

Original languageEnglish
JournalGeological Journal
Volume55
Issue number7
Pages (from-to) 5155-5165
Number of pages11
ISSN0072-1050
DOIs
Publication statusPublished - 2020

    Research areas

  • Avalonia, Baltica, K-bentonites, Ordovician, source magma, trace elements, volcanic ash

ID: 234945711