The Precambrian of Transangaria, Yenisei Ridge (Siberia): Neoproterozoic microcontinent, Grenville-age orogen, or reworked margin of the Siberian craton?

Author:

Kuzmichev Alexander B.,Sklyarov Eugene V.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference56 articles.

1. Igneous zircon: trace element composition as an indicator of source rock type;Belousova;Contrib. Mineral. Petrol.,2002

2. Age boundaries in the geological evolution of early Precambrian of Yenisei Ridge;Bibikova;Stratigr. Geol. Correlat.,1993

3. Mafic crustal xenoliths and the origin of the lower continental crust;Condie;Lithos,1999

4. Dobretsov, N.L., 1974. Blueschist and Eclogite–Blueschist Complexes of the USSR, Nauka, Novosibirsk, 430 p. (in Russian).

5. Strike-slip tectonics and subalkaline mafic magmatism in the Early Paleozoic collisional system of the western Baikal region;Fedorovsky;Russ. Geol. Geophys.,2010

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