Mozgova, N N; Borodaev, YuS; Gablina, I F; Cherkashov, Georgy A; Stepanova, Tamara V (2005): Chemical composition of hydrothermal sulfide minerals from the Rainbow, Logachev-1, and Logachev-2 hydrothermal fields. PANGAEA, https://doi.org/10.1594/PANGAEA.787200, Supplement to: Mozgova, NN et al. (2005): Mineral assemblages as indicators of the maturity of oceanic hydrothermal sulfide mounds. Translated from Litologiya i Poleznye Iskopaemye, 2005, 4, 339-367, Lithology and Mineral Resources, 40(4), 293-319, http://www.springerlink.com/content/g672hl12q71l860t/
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Composition of ore minerals in MAR sulflde occurrences related to ultramaflc rocks was studied using methods of mineragraphy, electron microscopy, microprobe analysis, and X-ray analysis. Objects are located at various levels of maturity of sulflde mounds owing to differences in age, duration and degree of activity of the following hydrothermal systems: generally inactive Logatchev-1 field (up to 66.5 ka old), inactive Logatchev-2 field (3.9 ka), and generally active Rainbow field (up to 23 ka). Relative to MAR submarine ore occurrences in the basalt substrate, mineralization in the hydrothermal fields mentioned above is characterized by high contents of Au, Cd, Co, and Ni, along with presence of accessory minerals of Co and Ni. The studied mounds differ in quantitative ratios of major minerals and structural-textural features of ores that suggest their transformation. Ores in the Logatchev-1 field are characterized by the highest Cu content and development of a wide range of multistage contrast exsolution structures of isocubanite and bornite. In the Logatchev-2 field, sphalerite-chalcopyrite and gold-arsenic exsolution structures are present, but isocubanite exsolution structures are less diverse and contrast. The Rainbow field is marked by presence of homogenous isocubanite and the subordinate development of exsolution structures. The authors have identified four new phases in the Cu-Fe-S system. Phases X and Y (close to chalcopyrite and isocubanite, respectively) make up lamellae among isocubanite exsolution products in the Logatchev-1 and Logatchev-2 fields. Phase Y includes homogenous zones in zonal chimneys of the Rainbow field. Phases A and B formed in the orange bornite domain at low-temperature alteration of chalcopyrite in the Logatchev-1 field. Mineral assemblages of the Cu-S system are most abundant and diverse in the Logatchev-1 field, but their development is minimal in the Logatchev-2 field where mainly Cu-poor sulfides of the geerite-covellite series have been identified. Specific features of mineral assemblages mentioned above reflect the maturity grade of sulfide mounds and can serve as indicators of maturity.
Median Latitude: 25.483424 * Median Longitude: -39.430454 * South-bound Latitude: 14.720000 * West-bound Longitude: -44.979240 * North-bound Latitude: 36.230150 * East-bound Longitude: -33.900300
Datasets listed in this publication series
- Mozgova, NN; Borodaev, YS; Gablina, IF et al. (2005): (Table 3) Chemical composition of readily oxidizable chalcopyrite from the Rainbow hydrothermal field. https://doi.org/10.1594/PANGAEA.787197
- Mozgova, NN; Borodaev, YS; Gablina, IF et al. (2005): (Table 4) Chemical composition of lamellae of phase X (anomalous chalcopyrite) in iss exsolution structures of the Logachev-1 and Logachev-2 hydrothermal fields. https://doi.org/10.1594/PANGAEA.787198
- Mozgova, NN; Borodaev, YS; Gablina, IF et al. (2005): (Table 5) Chemical composition of isocubanite from the Rainbow and Logachev-1 hydrothermal fields. https://doi.org/10.1594/PANGAEA.787199
- Mozgova, NN; Borodaev, YS; Gablina, IF et al. (2005): (Table 6) Chemical composition of homogenous phase Y from copper sulfide hydrothemal chimneys of the Rainbow hydrothermal field and of lamellae in exsolution structures of the Logatchev-2 hydrothermal field. https://doi.org/10.1594/PANGAEA.787201