1982
DOI: 10.1007/bf01825035
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Ore deposition in a proterozoic incipient rift zone environment: a tentative model for the Filipstad-Grythyttan-Hjulsjö region, Bergslagen, Sweden

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Cited by 75 publications
(57 citation statements)
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“…Here, the Mg-rich schists form discordant, Iensoid zones trending parallel to the general foliation, a proposed axis of rifting and the long axes of tectonic basins (OEN et al, 1982). BAKet~ and D~GRooT argue convincingly that the Mg-rich schists were formed by seawater-rock interaction.…”
Section: Secondary Alterationsmentioning
confidence: 95%
“…Here, the Mg-rich schists form discordant, Iensoid zones trending parallel to the general foliation, a proposed axis of rifting and the long axes of tectonic basins (OEN et al, 1982). BAKet~ and D~GRooT argue convincingly that the Mg-rich schists were formed by seawater-rock interaction.…”
Section: Secondary Alterationsmentioning
confidence: 95%
“…The rocks described in this paper belong to the UpperLeptite-H/illeflinta-Slate Group of Oen et al (1982) and were affected by low-grade greenschist facies metamorphism (Sundius, 1923), which * Present address: Technical University of Wroctaw, Institute of Inorganic Chemistry and Metallurgy of Rare Elements, 50-370 Wroctaw, Wybrze~,e Wyspiafiskiego 27, Poland.…”
mentioning
confidence: 99%
“…Introduction and geological setting INDIUM-bearing sphalerite associated with roquesite and In-bearing stannite or sakuraiite has previously been described from only a few localities (Kato and Shinohara, 1968;Sutherland and Boorman, 1969;Oen et al, 1980;Burke and Kieft, 1980;Shimizu et al, 1986;Johan, 1988). This paper describes the petrogenesis of a new occurrence.…”
mentioning
confidence: 99%
“…The volcano-sedimetary sequence in the Gfisborn area consists of acid metavolcanics with intercalated marbles, metacherts, metamorphosed basic lavas and a metamorphosed manganiferous iron ore horizon (Damman, 1988a), belonging to the upper leptite and slate group of the Bergslagen supracrustal series (Oen et al, 1982;Oen, 1987). During their deposition these rocks have been intruded by the Ostra Hrjden granite (Damman, 1988b (Fig.…”
mentioning
confidence: 99%
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