Preview

Mining Science and Technology (Russia)

Advanced search

THE COMPARATIVE ANALYSIS OF PRECAMBRIAN GOLD RESERVES FORMATIONS OF CRYSTALLIZED SHIELDS

https://doi.org/10.17073/2500-0632-2017-2-11-25

Abstract

Gold reserves localized in Precambrian deposits are known in the most crystallized shields of the Earth. They are confined to Greenstone belts on the Canadian, Indian, Brazilian and Australian shields and represented by gold reserves deposits from the first ton to 1000 – 1500 tons (Pickle crow, nor-Acme, Homestake, etc. in North America, Kalgoorlie, Leonora and others in Western Australia). Despite the presence of trough structures of Precambrian age, some of which can be considered as analogues of Greenstone belts, the Aldan shield is quite specific of the named above. The comparison of ore fields help evaluate the genesis process of gold mineralization localized in Precambrian formations crystalline shields of the planet and thus define their similarity. There is a number of features that let evaluate the uniqueness of similarities: the anomaly of the magnetic field in the plan coincide with the gravity anomalies indicating the presence of dome uplifts of the basement; the rocks that led to the existence of anomalies of the magnetic field are similar in their geochemical features; the structures mapped by these anomalies are similar to the narrow anticlinal folds; the age of those structures is approximately the same; the identity of the ore-controlling factors and stratigraphic positions. These features allow to accurately assess the similarity of deposit named after P. Pinigin that has the largest gold resources in the world. Therefore, it gives the opportunity to hope for a significant expansion of the gold potential of the Precambrian age at the Aldan shield.

About the Authors

A. A. Syasko
Теchnical Institute (branch) of North-Eastern Federal University named after Ammosov
Russian Federation

Leading Researcher, Cand. Sci. (Tech.)

678960, RS (Y) Neryungri, st. Kravchenko 16



N. N. Grib
Теchnical Institute (branch) of North-Eastern Federal University named after Ammosov
Russian Federation

Deputy Director, Dr. Sci. (Tech.), Prof.

678960, RS (Y) Neryungri, st. Kravchenko 16



E. F. Redlikh
Теchnical Institute (branch) of North-Eastern Federal University named after Ammosov
Russian Federation

Senior Lecture

678960, RS (Y) Neryungri, st. Kravchenko 16



References

1. Kravchenko A.A. The Genesis of gold-bearing Precambrian metabasites of the Central part of the Aldan-Stanovoi shield: the deposit named after P. Pinigin asИan example // the thesis of candidate of geological-mineralogical Sciences. 2009. (189).

2. Nekrasov E. M. Foreign endogenous gold deposits / E. M. Nekrasov, Moscow: Nedra, 1988. 215 c.

3. Safonov Yu. G. Potential development of mineral resources of gold of Russia in the XXI century [Electronic resource]. URL: http://www.geoclab.ru/articles/96/1549/.

4. Syasko A. A., Grib N. N. Forecast resources of gold deposits according to geochemical sampling // Ores and metals. 2012. No. 5. C. 36-42.

5. Syasko A. A., Grib N. N., Kachaev A. V. The Selection of search criteria, gold deposits of the Precambrian Aldan shield // the Depository of the publishing house of MGGU. 2008. No. 639/07-08. C. 19.

6. Syasko A. A., Grib N. N., Kachaev A.V. The Analysis of the Precambrian Geology of gold fields of Kolar (India) and Aldano-Stanovoy shield (the southern Yakutia) // Modern problems of science and education. 2009. No. 6-3. C. 33-38.

7. Syasko A. A., Grib N. N., Kachaev A. V. On the prospects of gold fields of a new type of the Aldan shield // Ores and metals. 2012. No. 5. C. 30-35.

8. Syasko A. A., Grib N. N., Nikitin V. M., The Comparative features of Archean gold deposits // Science and education. 2006. No. 4/44. C. 58-65.

9. Bateman R., Hagemann S. Gold mineralisation throughout about 45 Ma of Archaean orogenesis: protracted flux of gold in the Golden Mile, Yilgarn craton, Western Australia // Mineralium Deposita. 2004. № 39. C. 536–559.

10. Berger B.R. Descriptive model of Homestake Au, in Cox, D.P., and Singer, D.A., eds., Mineral Deposit Models // U.S. Geological Survey Bulletin. 1986. № 1693. C. 244.

11. Fullerton W.R. The Kalgoorlie gold : A review of factors of formation for a giant gold deposit // Dissertations in Geology at Lund University. 2013. № 334 (21).

12. Hanes J.A., Archibald D.A., Hodgson C.J. Dating of Archean auriferous quartz vein deposits in the Abitibi greenstone belt, Canada; 40 Ar/39 Ar evidence for a 70- to 100-my-time gap between plutonism- // Economic Geology. 1992. № 87. C. 1849–1861.

13. Hayman P.C. [и др.]. Evolution of a ∼2.7Ga large igneous province: A volcanological, geochemical and geochronological study of the Agnew Greenstone Belt, and new regional correlations for the Kalgoorlie Terrane (Yilgarn Craton, Western Australia) // Precambrian Research. 2015. (270). C. 334–368.

14. Hodgson C.J., Hamilton J.V. Gold mineralization in the Abitibi greenstone belt: end-stage results of Archean collisional tectonics? подред. D.I. Keays, R.R.; Ramsay, W.R.H.; Groves, Economic Geology, 1989. 86–100 с.

15. Klein T., Day W. Descriptive and grade-tonnage models of Archean lowsulfide Au- quartz veins and a revised grade-tonnage model of Homestake Au // United States Department of the interior geological survey, Open-file Report. 1994.

16. Natural Resource Holdings Global Gold Mines & Deposits 2013 Ranking 2013. C. 1–40.

17. Qiu Y.., Groves D.I. Late Archean collision and delamination in the southwest Yilgarn Craton: the driving force for Arche-an orogenic lode-gold mineralization // Economic Geology. 1999. (94). C. 115–122.

18. Shackleton J.M., Spry P.G., Bateman R. Telluride mineralogy of the Golden Mile deposit, Kalgoorlie, Western Australia // Canadian Mineralogist. 2003. № 6 (41). C. 1503–1524.

19. 12th Australian Geological Convention подред. W.K. Witt, D.I. Groves, S.E. Ho, Geological-еизд., East Perth:, 1994. 87 c.

20. Kolar Gold Limited [Электронныйресурс]. URL: http://graftonresources.com/wp-content/uploads/2011/09/Ocean-Report-May-2011.pdf.

21. Depatment of Mines and Petroleum Goverment of Western Australia. URL: http://warims.dmp.wa.gov.au/GeoView/Viewer.html?Viewer=GeoVIEW.

22. Amarski, V. G., Syasko A. A. The Project on prospecting works within the Verkhne-Lubicich ore field in 2000-2003 Chulman, 2001.

23. Amarski, V. G., Shvets V. N. Report on gold ore prospecting held on the square in the Verchne-Lubicich ore field in 2000-2003 Chulman, 2003.

24. Gusev, V. P., Report about the prospecting works results in southern Yakutia with the features of gold mineralization unidentified types (Central Aldan district and the surrounding area) during 1983-1989. Aldan, 1990.

25. Morozov V. M., Yadryshnikova R. G. The report on the results of aeromagnetic images of scale 1:10,000 and 1:25,000, made in the southern Aldan iron ore area in 1976-1977 Nyurba, 1978.

26. Polyakov N. P. Geological materials to techno-economic considerations (TPP) on the possible industrial value of iron ore Leglierski ore field. Chulman, 1987.

27. Safonov A. M. Geological structure and mineral resources of the Central part of Temulyakit-Tungurchinskaya ore zones (report of Lomachinskiy party on the results of APGC-50 and in the search of gold, held in 1983-1988 in the Central part of the zone). Chulman, 1988.

28. Toropygin S.B., Syasko A.A. Report on the results of gold occurrence prospecting works at Kur and Pritrassovoe deposits. Chulman, 2001.


Review

For citations:


Syasko A.A., Grib N.N., Redlikh E.F. THE COMPARATIVE ANALYSIS OF PRECAMBRIAN GOLD RESERVES FORMATIONS OF CRYSTALLIZED SHIELDS. Mining Science and Technology (Russia). 2017;(2):11-27. (In Russ.) https://doi.org/10.17073/2500-0632-2017-2-11-25

Views: 701


Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.


ISSN 2500-0632 (Online)