Granulite complexes of the Dzhugdzhur-Stanovoi Fold Region and the Peristanovoi Belt: Age, formation conditions, and geodynamic settings of metamorphism

Author:

Glebovitsky V. A.,Kotov A. B.,Sal’nikova E. B.,Larin A. M.,Velikoslavinsky S. D.

Publisher

Pleiades Publishing Ltd

Subject

Geology

Reference58 articles.

1. A. Yu. Antonov, S. I. Dril, and E. V. Bankovskaya, “Rb-Sr Isotopic Characteristics of Allochthonous and Autochthonous Late Mesozoic Granitoids of the Stanovoi Range (Southern Framework of the Aldan Shield),” Tikhookean. Geol. 20(4), 61–75 (2001).

2. N. G. Berezhnaya, V. E. Bibikova, A. B. Sochava, et al., “Isotopic Age of the Chinei Subgroup of the Udokan Group of the Kodar-Udokan Trough,” Dokl. Akad. Nauk SSSR 302(5), 1209–1212 (1988).

3. E. V. Bibikova, S. N. Gavrikova, V. Ya. Fedorchuk, et al., “Early Proterozoic Age of Granulitic Rocks of the Stanovik (U-Pb Data of Zircons),” Geokhimiya 31(10), 1428–1438 (1993).

4. E. V. Bibikova, G. M. Drugova, V. L. Duk, et al., “Geochronology of the Aldan-Vitim Shield,” in Isotopic Geology and Geochronologic Scale (Nauka, Moscow, 1986), pp. 135–159 [in Russian].

5. E. V. Bibikova, I. M. Morozova, T. V. Gracheva, and V. A. Makarov, “U-Pb Age of the Kurul’ta Granulites,” in The Ancient Rocks of the Aldan-Stanovoi Shield. Guidebook of the International Geological Excursion, IGCP Project 280 (Sevmorgeologiya, Leningrad, 1989), pp. 183–191 [in Russian].

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