1985
DOI: 10.1007/bf00381559
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Manganiferous pyroxenes and pyroxenoids from three Pb-Zn-Cu skarn deposits

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1985
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Cited by 17 publications
(10 citation statements)
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“…The Mn-rich mineralogy is characteristic of the Pb-Zn skarn deposits placed distal from a magmatic source (e.g., Einaudi et al, 1981;Abrecht, 1985;Logan, 2000;Vassileva and Bonev, 2001;Vassileva et al, 2005;Meinert et al, 2005;Canet et al, 2009) and reflects remobilization of Mn from the country rocks. The principal prograde mineral is hedenbergite enriched in Mn.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The Mn-rich mineralogy is characteristic of the Pb-Zn skarn deposits placed distal from a magmatic source (e.g., Einaudi et al, 1981;Abrecht, 1985;Logan, 2000;Vassileva and Bonev, 2001;Vassileva et al, 2005;Meinert et al, 2005;Canet et al, 2009) and reflects remobilization of Mn from the country rocks. The principal prograde mineral is hedenbergite enriched in Mn.…”
Section: Discussionmentioning
confidence: 99%
“…Figure 10 presents the ternary proportion of their diopside-johannsenite-hedenbergite components. The manganese-rich mineralogy is typical for Pb-Zn skarn deposits distal from intrusions (e.g., Einaudi et al, 1981;Abrecht, 1985;Logan, 2000;Vassileva and Bonev, 2001;Vassileva et al, 2005;Canet et al, 2009). Diopside and johannsenite contents vary up to 45 and 10 mol %, respectively.…”
Section: Compositions Of Skarn and Ore Mineralsmentioning
confidence: 99%
“…The compositions of the clinopyroxene are expressed in terms of mole fractions of the three end members, i.e., hedenbergite (Hd), johannsenite (Joh), and diopside (Di) as there is no miscibility gap between hedenbergite-diopside on one side and johannsenite on the other (Abrecht, 1985). The chemical data of all analyzed clinopyroxenes are plotted together and cluster into three different areas within the diopside-hedenbergite-johannsenite ternary plot (Fig.…”
Section: Chemical Compositions Of Garnet and Clinopyroxenementioning
confidence: 99%
“…Diopside and johannsenite contents vary up to 45 and 10 mol %, respectively. The manganese-rich mineralogy is typical for Pb-Zn skarn deposits distal from intrusions (e.g., Einaudi et al, 1981;Abrecht, 1985;Logan, 2000;Vassileva and Bonev, 2001;Vassileva et al, 2005;Canet et al, 2009).…”
Section: Compositions Of Skarn and Ore Mineralsmentioning
confidence: 99%