1996
DOI: 10.1144/gsl.sp.1997.119.01.22
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Zincian rancieite from the Kato Nevrokopi manganese deposits, Macedonia, northern Greece

Abstract: At the 25th km main Mn-mine of Kato Nevrokopi, Macedonia, northern Greece, rancieite forms flaky to laminated aggregates encrusting vugs, and replacing pyrolusite and todorokite in massive deposits of the Falakron marbles. It has an unusually high ZnO (1.53-3.07 wt%) content and therefore it was named 'zincian rancieite'. The average (18 spots) chemical composition of rancieite by EPMA is (wt%): MnO2 62.01, CaO 6.83, ZnO 2.54, A1203 1.18, MgO 0.63 plus minor oxides (Fe203, K20 & SiO2), total of 73.98. Assuming… Show more

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Cited by 7 publications
(2 citation statements)
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“…Ranciéite is characteristically found, for example, in Ca‐rich environments such as travertines, limestones or marbles (Nimfopoulos et al . ), but in the case of the thermal spring water of the Ploutonion , the Ca concentration is not the main factor in determining the precipitation of the ranciéite mineral phase rather than birnessite or todorokite. The mineral species in the manganese was precipitated from hot‐spring water and is therefore dependent on the presence or absence of micro‐organisms (Miura and Hariya ).…”
Section: Resultsmentioning
confidence: 97%
“…Ranciéite is characteristically found, for example, in Ca‐rich environments such as travertines, limestones or marbles (Nimfopoulos et al . ), but in the case of the thermal spring water of the Ploutonion , the Ca concentration is not the main factor in determining the precipitation of the ranciéite mineral phase rather than birnessite or todorokite. The mineral species in the manganese was precipitated from hot‐spring water and is therefore dependent on the presence or absence of micro‐organisms (Miura and Hariya ).…”
Section: Resultsmentioning
confidence: 97%
“…The samples collected represent ore from waste piles which are disposed of adjacent to the closed mine sites of Mavro Xylo and "25th Km", Kato Nevrokopi, Drama, Greece. The ore paragenesis in these sites mainly consists of pyrolusite, nsutite (MnO 2 ), and todorokite [Ca,K,Na,Mg,Ba,Mn)(Mn,Mg,Al) 6 O 12 *3H 2 O] at various abundances [23,24]. The mineralogy of the studied samples is verified prior to the experiments by XRD analysis showing that the MLX3 is mostly comprised of nsutite and sample MLX1 is a mixture of nsutite and todorokite with minor matrix calcite.…”
Section: Sample Selectionmentioning
confidence: 99%