Generalized scheme of the Valerianov volcanic-plutonic complex and its ore content
Authors:
Abstract
The Early Carboniferous Valerian andesitodiorite volcanic-plutonic complex is located in the Turgai Trough. It is composed of gabbro-granodiorite intrusive rocks, basalt-rhyolite volcanic rocks and dikes of different composition. The complex consists of several magmatic nodes represented by paleovolcanic structures. Comparison of the structure of paleovolcanic structures located at different levels of erosional section allows us to create a generalized model of the complex. The complex is genetically associated with skarn-magnetite and associated minerals.
Область исследования:
(Archived) Without section
References
- Dymkin A.M. Petrology and genesis of magnetite deposits of Turgai. Novosibirsk: Nauka, 1967. 167 p.
- Luchitsky I.V. Fundamentals of Paleovolcanology. M: Nauka, 1971. V. 2. 383 p.
- Masurenkov Y.P. Volcanoes over intrusions. M: Nauka, 1979. 219 p.
- Porotov G.S. Criteria of the location of skarn-magnetite deposits in the structure tiers of paleovolcanic apparatuses // Journal of Mining Institute. 1985. V. 104. P.51-56.
- Porotov G.S. Genetic and mineral types of skarn-magnetite deposits // Zap. of the Leningr. Mining Institute. 1987. V. 112. P. 102-109.
- The problem of volcanic-plutonic formations on the example of Kazakhstan / A.A. Abdulin, R.A. Borukaev, V.K. Zaravnyaeva and others // Volcanic-plutonic formations and their ore-bearing capacity. Alma-Ata: Nauka, 1969. P.8-12.
- Strona P.A. Main types of ore formations. L.: Nedra, 1978. 199 p.
- Ustiev E.K. Problems of Volcano-Plutonism. Volcano-plutonic formations // Izv.AN USSR. Ser. geol. 1963. P. 3-30
- Fedotov S.A. About the input temperatures of magmas, formation, sizes and evolution of volcanic centers // Volcanology and Seismology. 1980. № 4. P. 3-29.