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

Tarmo Kiipli; Rutt Hints; Toivo Kallaste; Arne T. Nielsen; Siim Pajusaar; Niels H. Schovsbo

doi:10.1002/gj.3737

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

Tarmo Kiipli, Rutt Hints, Toivo Kallaste, Arne T. Nielsen, Siim Pajusaar, Niels H. Schovsbo

Geology

Research output: Contribution to journal › Journal article › Research › peer-review

6 Citations (Scopus)

Original language	English
Journal	Geological Journal
Volume	55
Issue number	7
Pages (from-to)	5155-5165
Number of pages	11
ISSN	0072-1050
DOIs	https://doi.org/10.1002/gj.3737
Publication status	Published - 2020

Keywords

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

Access to Document

10.1002/gj.3737

Cite this

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. / Kiipli, Tarmo; Hints, Rutt; Kallaste, Toivo et al.
In: Geological Journal, Vol. 55, No. 7, 2020, p. 5155-5165.

Research output: Contribution to journal › Journal article › Research › peer-review

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