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Kallaste & Pukkonen, 1992

Pyrite varieties in Estonian Tremadocian argillite (Dictyonema shale)

Kallaste, T., Pukkonen, E.
DOI10.3176/geol.1992.1.02
Aasta1992
Pealkiri tõlgitudPüriidierimitest Eesti Tremadoci argilliidis
AjakiriProceedings of the Estonian Academy of Sciences. Geology
Köide41
Number1
Leheküljed11-22
Tüüpartikkel ajakirjas
Eesti autor
Keelinglise
Id11500

Abstrakt

Estonian Tremadocian organic-rich argillite (Dictyonema shale) contains up to 20% organic matter, and 4-6% pyrite. Most of the pyrite occurs in fine-dispersed form invisible with the naked eye. About 60% of the thin sandstone interlayers in argillite are cemented with pyrite (type 1), half of them are covered with a thin finegrained pyrite seam (type 2). The constitution of the latter prompted to consider its composition and genesis similar to the fine-dispersed pyrite that cannot be separated from argillite. Besides these two types, very thin ( < 1 mm) light-grey siltstone interlayers, pyrite knobs, and some pyrite findings other than the described varieties have been studied by X-ray diffractometry and emission spectroscopy methods.

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