Dike complex in the activated part of the Stanovoy a folded area
Authors:
Abstract
In recent years, an independent complex of dikes of diorite porphyrites, granite porphyries and granosyenite porphyries of Cretaceous age, confined to the zone of intense Mesozoic activation of the Precambrian platform, has been identified in the central part of the Stanovoy folded area. The dikes were described by E. P. Gurova and E. P. Gurov, who, unfortunately, did not take into account the works of the FESU, described in this article.
Область исследования:
(Archived) Without section
Funding:
None
References
- Gurova E. P., Gurov E. P. Mesozoic small intrusions of the western part of the Stanovy Ridge. Geologiya i geofizika, No. 2, 1966.
- Gurov E. P. and Gurov E. P. On the tectonic position of the dike belts of the Stanovoi Ridge. Geotektonika, No. 6, 1967.
- Krasny L. I. Tectonics. In the book Geologic Structure of the USSR, vol. 19, part I. Nedra, 1966.
- Kuznetsov Yu. A. Main types of magmatic formations. Nedra, 1964.
- Moiseenko F. S. Magnetic susceptibility as an indicator of rock formation conditions. Geologiya i geofizika, No. 3, 1966.
- Nagata T. Magnetism of rocks. Mir, 1965.
- Shatalov E. T. et al. Criteria of Connection between Mineralization and Magmatism as Applied to the Study of Ore Districts. Nedra, 1965.