Tagasi otsingusse
Kallaste & Pukkonen, 1992
Pyrite varieties in Estonian Tremadocian argillite (Dictyonema shale)
Kallaste, T., Pukkonen, E.
DOI | 10.3176/geol.1992.1.02 |
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Aasta | 1992 |
Pealkiri tõlgitud | Püriidierimitest Eesti Tremadoci argilliidis |
Ajakiri | Proceedings of the Estonian Academy of Sciences. Geology |
Köide | 41 |
Number | 1 |
Leheküljed | 11-22 |
Tüüp | artikkel ajakirjas |
Eesti autor | |
Keel | inglise |
Id | 11500 |
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.
Viimati muudetud: 28.11.2022