Tim-Yastrebov structure of the Kursk magnetic anomaly: geology, tectonics, deep structure, geochemistry and mineralogy

Authors

  • V. K. Kushnerenko Urangeology, Russian Federation

DOI:

https://doi.org/10.24028/gzh.0203-3100.v35i3.2013.116415

Abstract

The Tim-Yastrebovskaya structure is located in the Oskol Ore Province of the KMA (the Voronezh crystalline massif). Integrated interpretation of gravimetric and magnetometric data together with seismic characteristics, have shown that the Tim-Yastrebovskaya structure rests on a compacted magnetic basement. As the carbonaceous-volcanic-sedimentary formation, which fills the Tim-Yastrebovskaya structure, is highly promising for noble metals, forecasting-exploration criteria for hydrothermal gold-sulphide ore formation (with platinoids) are discussed.

References

Кушнеренко В.К., Шувалов Ю.М., Мятлин В.М. Золото и другие элементы-примеси в железорудных месторождениях КМА (к проблеме комплексного использования) // Региональная геология и металлогения. - 1999. - № 9. - С. 120-124.

Кушнеренко В. К. Комплексное освоение минерально-сырьевых ресурсов КМА и вопросы горно-геологической безопасности // Горн. журн. - 2001. - № 4. - С. 51-53.

Цибизова С.А. Малые элементы в коре выветривания железистых кварцитов Лебединского и Стойленского месторождений КМА: Ав-тореф. дис. канд. геол.-минерал. наук. - Иркутск, 1990. - 21 с.

Тарков А.П. Глубинное строение Воронежского массива по геофизическим данным. - Москва: Недра, 1974. - 172 с.

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Published

2013-04-01

How to Cite

Kushnerenko, V. K. (2013). Tim-Yastrebov structure of the Kursk magnetic anomaly: geology, tectonics, deep structure, geochemistry and mineralogy. Geofizicheskiy Zhurnal, 35(3), 146–155. https://doi.org/10.24028/gzh.0203-3100.v35i3.2013.116415

Issue

Vol. 35 No. 3 (2013)

Section

Articles

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