Quartzite–Schist Sequences of the Aktau–Mointy Massif (Central Kazakhstan): Structural Position, Provenance, and Formation Stages of the Earth Crust in the Precambrian

Author:

Kanygina N. A.,Tretyakov A. A.,Degtyarev K. E.,Kovach V. P.,Plotkina J. V.,Pang K.-N.,Wang K.-L.,Lee H.-Y.

Publisher

Pleiades Publishing Ltd

Subject

Geology

Reference51 articles.

1. The age of porphyroids from the Atasu–Mointy watershed;A. V. Avdeev,1965

2. The key marker of the Late Precambrian of Kazakhstan and North Kyrgyzstan;A. V. Avdeev,1992

3. A. V. Avdeev, E. V. Al’perovich, V. D. Voznesenskii, and B. G. Koren’kov, “Precambrian deposits of the Akt-au–Mointy watershed,” in Pre-Paleozoic and Paleozoic of Kazakhstan, Ed. by A. A. Abdulin (Nauka, Alma-Ata, 1974), Vol. 1, pp. 53–57.

4. Some results of lithologic study of Proterozoic shale-quartzite sequences of the Aktau–Mointy anticlinorium;N. I. Gvozdik,1980

5. N. I. Gvozdik, “Upper Proterozoic quartzite strata of the Aktau–Mointy watershed,” Vestn. Mosk. Univ. Ser. 4: Geol., No. 3, 18–22 (1978).

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