Gold deposits in dikes of the Yana-Kolyma belt

Author:

Volkov A. V.,Egorov V. N.,Prokof’ev V. Yu.,Sidorov A. A.,Goryachev N. A.,Biryukov A. V.

Publisher

Pleiades Publishing Ltd

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference40 articles.

1. V. V. Akinin, E. Miller, J. Wooden, et al., “U-Pb SHRIMR Dating of Zircon from Batholiths and Ore-Bearing Dikes in the Yana-Kolyma Collision Belt: First Results and Geological Implications,” in Proceedings of Conference on Isotopic Dating of Ore Formation, Magmatism, Sedimentation, and Metamorphism (GEOS, Moscow, 2006), Vol. 1, pp. 26–30 [in Russian].

2. F. R. Apel’tsin, “Distinguishing Petrographic and Petrochemical Features of Differently Aged Associations of Minor Intrusions of the Main Gold Belt of the Northeastern USSR,” Trudy VNII-1 8, 75–190 (1957).

3. P. V. Babkin, M. L. Gel’man, F. F. Vel’dyaksov, and L. A. Pavlyuchenko, “Prospects for Discovery of Gold in Sulfidized Zones in Black Shale Sequences of the Northeastern Russia,” Kolyma, No. 2, 14–22 (2001).

4. T. Baker, “Emplacement Depth and Carbon Dioxide-Rich Fluid Inclusions of Intrusion-Related Gold Deposits,” Econ. Geol. 97, 1111–1117 (2002).

5. R. J. Bodnar and M. O. Vityk, “Interpretation of Microthermometric Data for H2O-NaCl Fluid Inclusions,” in Fluid Inclusions in Minerals: Methods and Applications (Pontignano-Siena, 1994), pp. 117–130

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