1-19-3

УДК 549.612(571.63) https://doi.org/10.21440/2307-2091-2019-1-28-38 


I. A. Baksheev, E. A. Vlasov / News of the Ural State Mining University. 2019. Issue 1(53), pp. 28-38

Relevance of the work is due to the need to study the mineralogy of gold deposits in the Russian Far East, information about which is extremely scarce.
Purpose of the work: study of the chemical composition of tourmaline from Mnogovershinnoe ore deposit, Khabarovsk Krai (Far East).
Methodology of research: The chemical composition of minerals and BSE images were obtained using a Jeol JSM-6480 electron microscope equipped with an Inca Energy-350 EDS (analyst is N. N. Koshlyakova, Department of Petrology, Lomonosov Moscow State University). Electron microscope shooting environment: accelerating voltage is 15 kV, measuring current for the sample is 30 ± 0.1 nA. XPP corrections were used for the adjustment procedure (INCA program, version 17a).
Results. The obtained data show that tourmalines of the Mnogovershinnoe deposit differ in their chemical composition and type of substitution. All studied tourmalines by these parameters can be divided into two groups. Group 1 includes schorl, foitite, and pegmatoids feruvite, as well as schorl and foitite of the first generation, tourmaline-muscovite-quartz veinlet in sandstones. Group 2 includes schorl of the second generation, tourmaline-muscovite quartz veinlet, schorl and foitite of quartz-tourmaline metasomatites, and cement dravite of quartz breccia.
Conclusions. Tourmalines of the post-ore mineral associations of the Mnogovershinnoe gold deposit are divided into two groups characterized by different chemical composition and substitutions. Tourmalines of the first group with substitutions Fe ↔ Mg and X-vacancy + Al ↔ Na + R2+ are confined to pegmatoids and were formed in reducing or weakly oxidative conditions. Later tourmalines of the second group with substitutions Fe3+ ↔ Al and Al + O2– ↔ R2++ OH– indicate a possible porphyry-style mineralization and its formation during lowering oxidative potential.

Keywords: tourmaline, chemical composition, altered rocks, Mnogovershinnoe deposit, Khabarovsk Krai, Far East..

 

 

REFERENCES

1. Henry D. J., Novák M., Hawthorne F. C., Ertl A., Dutrow B. L., Uher P., Pezzotta F. 2011, Nomenclature of the tourmaline-supergroup minerals. American Mineralogist, vol. 96, pp. 895–913. https://doi.org/10.2138/am.2011.3636
2. Kuzmin V. I., Dobrovolskaya N. V., Solntseva L. S. 1979, Turmalin i yego ispol’zovaniye pri poiskovo-otsenochnykh rabotakh [Tourmaline and its use in prospecting]. Moscow, 272 p.
3. Collins A. C. 2010, Mineralogy and geochemistry of tourmaline in contrasting hydrothermal systems: Copiapó area, Northern Chile. Unpub. Master thesis, Univ. Arizona, 225 p.
4. Slack J. F. 1996, Tourmaline associations with hydrothermal ore deposits. Reviews in Mineralogy, vol. 33, pp. 559–643.
5. Moiseenko V. G., Eyrish L. G. 1996, Zolotorudnyye mestorozhdeniya vostoka Rossii [Gold deposits of the east of Russia]. Vladivostok, 360 p.
6. Ratkin V. V. 1995, Pre- and postaccretionary metallogeny of the Southern Russian Far East. Resource Geology, no 18, pp. 127–133. https://doi.org/10.1127/0935-1221/2012/0024-2241
7. Nokleberg W. J. 2010, Metallogenesis and tectonics of the Russian Far East, Alaska, and the Canadian Cordillera. U.S. Geological Survey, 397 p.
8. Kazarinov A. I., Mikhailova M. S. 1970, Relationships of gold and gold-silver mineralization with propylites, secondary quartzites and quartz metasomatites (using the group of subvolcanic deposits of the East of the USSR as an example). Izvestiya Tomskogo politekhnicheskogo instituta [Bulletin of the Tomsk Polytechnic University], vol. 239, pp. 50–54. (In Russ.)
9. Konstantinov M. M., Vargunina N. P., Kosovets T. N., Struzhkov S. F., Syngayevskiy E. D., Shishakova L. N. 2000, Zoloto-serebryanyye mestorozhdeniya [Gold and silver deposits]. Series: fields models noble and non-ferrous metals. Moscow, 239 p.
10. Ivanov V. V., Zinkov A. V., Taskaev A. V. 1989, Mineralogiya pozdnepaleogenovykh zoloto-serebryanykh mestorozhdeniy v rayone Nizhnego Amura [Mineralogy of Late Paleogene gold-silver deposits in the area of Nizhni Amur]. Collection of works: Typical minerals of ore deposits in volcanic belts and zones of activation of northeast Asia. Vladivostok, pp. 87–89.
11. Jarozewich E. 2002, Smitsonian microbeam standards. Journal of Research of the National Institute of Standards and Technology, vol. 107, pp. 681–685. https://dx.doi.org/10.6028/jres.107.054
12. Henry D. J., Kirkland B. L., Kirkland D. W. 1999, Sector-zoned tourmaline from the cap rock of a salt dome. European Journal of Mineralogy, vol. 11, pp. 263-280.
13. Ertl A., Baksheev I. A., Giester G., Lengauer C. L., Prokofiev V. Yu., Zorina L. D. 2016, Bosiite, 3+3 NaFe (Al4Mg2)(Si6O18)(BO3)3(OH)3O, a new ferric member of the tourmaline supergroup from the Darasun gold deposit, Transbaikalia, Russia. European Journal of Mineralogy, vol. 28, pp.
581–591. https://doi.org/10.1127/ejm/2016/0028-2540
14. Korovushkin V. V., Kuzmin V. I., Belov V. F. 1979, Mössbauer studies of structural features in tourmaline of various genesis. Physics and Chemistry of Minerals, vol. 4, pp. 209–220. https://doi.org/10.1007/BF00307945
15. Baksheev I. A., Prokof’ev V. Yu., Zaraisky G. P., Chitalin A. F., Yapaskurt V. O., Nikolaev Y. N., Tikhomirov P. L., Nagornaya E. V., Rogacheva L. I., Gorelikova N. V., Kononov O. V. 2012, Tourmaline as a prospecting guide for the porphyry-style deposits. European Journal of Mineralogy, vol. 24, pp. 957–979. https://doi.org/10.1127/0935-1221/2012/0024-2241

 

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