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- W889781616 abstract "Fluid inclusions in quartz and calcite and the mineral chemistry of chlorite in the gangue of (Fe-Cu-Zn) sulfide deposits of the Northern Apennine ophiolites (Italy) have been investigated. Quartz and calcite contain fluid inclusions in the system H2O-NaCl-CaCl2, with low salinity and homogenization temperatures clustering in three different ranges: <100 °C, 120°-170°C and 240°-360°C. Preliminary data indicate that the highest temperatures are found preferentially in stratiform, massive ores, whereas results obtained for stockwork veins mostly reflect temperatures <170°C. Temperatures obtained from chlorite in stockwork veins are remarkably higher (176°-351°C). The nature of the fluid inclusions encountered so far, seem do not indicate any contribution of a magmatic source, but suggests that there was some influence by meteoric waters." @default.
- W889781616 created "2016-06-24" @default.
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- W889781616 date "2003-08-01" @default.
- W889781616 modified "2023-10-07" @default.
- W889781616 title "Fluid inclusions and chlorite geothermometry in Fe-Cu-Zn volcanic-hosted massive sulfide deposits of the Northern Apennine ophiolites (Italy): Preliminary results" @default.
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