Physicochemical controls on bismuth mineralization: An example from Moutoulas, Serifos Island, Cyclades, Greece
-
Michalis Fitros
, Stylianos F. Tombros
, Anthony E. Williams-Jones , Basilios Tsikouras , Eleni Koutsopoulou and Konstantin Hatzipanagiotou
Abstract
The 11.6 to 9.5 Ma Serifos pluton intruded schists and marbles of the Cycladic Blueschist unit, causing thermal metamorphism, the development of magnetite Ca-exo- and endo-skarns and the formation of low-temperature vein and carbonate-replacement ores. Potentially, the most important ores occur in the Moutoulas prospect where the mineralization in retrograde skarn and quartz veins culminated with the deposition of native bismuth. A combination of fluid inclusion microthermometry and isotope geothermometry suggests that the Moutoulas mineralization formed at a hydrostatic pressure of ~100 bars, from moderate-to-low temperature (~190–250 °C), and low-salinity (1.3–5.6 wt% NaCl equivalent) fluids. The calculated δ34SH2S compositions are consistent with the ore fluids having been derived from the Serifos pluton. Bismuth mineralization is interpreted to have occurred as a result of wall-rock interaction and mixing of a Bi-bearing ore fluid with meteoric waters. Native bismuth and bismuthinite deposited at ~200 °C, near neutral pH (6.5), low fS2 (<–16.5), and low fO2(<–44). Supergene alteration in Serifos led to the oxidation of native bismuth to bismite and bismutite.
Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.
Acknowledgments
We kindly thank D. Katsikis for his assistance with sampling in the Moutoulas mine. Critical comments from J. Mavrogenes, P. Voudouris, and the Associate Editor J. Roberge, as well as an anonymous reviewer, are gratefully acknowledged.
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Articles in the same Issue
- How many boron minerals occur in Earth’s upper crust?
- Outlooks in Earth and Planetary Materials
- Network analysis of mineralogical systems
- Special collection: From magmas to ore deposits
- Geochemistry of the Cretaceous Kaskanak Batholith and genesis of the Pebble porphyry Cu-Au-Mo deposit, Southwest Alaska
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- Nitrides and carbonitrides from the lowermost mantle and their importance in the search for Earth’s “lost” nitrogen
- Accounting for the species-dependence of the 3500 cm−1 H2Ot infrared molar absorptivity coefficient: Implications for hydrated volcanic glasses
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- Ilmenite breakdown and rutile-titanite stability in metagranitoids: Natural observations and experimental results
- Single-crystal equations of state of magnesiowüstite at high pressures
- Analysis of erionites from volcaniclastic sedimentary rocks and possible implications for toxicological research
- Reconstructive phase transitions induced by temperature in gmelinite-Na zeolite
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