1. I. A. Andreeva and V. V. Krupskaya, et al., “Grain-Size Features of the Bottom Sediments As an Indicator of the Conditions of Their Formation (By the Example of the Late Pleistocene-Holocene Sediments of the Northern Part of the Barents-Kara Shelf)” in Experience of Systematic Oceanological Studies in the Arctic, Ed. by A. P. Lisitsyna (Nauchnyi Mir, Moscow, 2001) [in Russian].
2. A. M. Blazhchishin and M. B. Kheirov, “Associations of Clay Minerals in the Upper Quaternary Deposits of the Barents Sea,” Litol. Polezn. Iskop., No. 3, 24–43 (1990).
3. S. A. Bondarenko, “Lithology and Paleogeography of the Deposits of the St. Anna Trough,” in Problems of Lithology, Geochemistry, and Ore Formation of the Sedimentation Process. Materials of the 1st All-Russian Lithological Workshop (GEOS, Moscow, 2000), Vol. 1, pp. 121–124 [in Russian].
4. M. V. Burtman, “Heavy Metals it Surface Layer of the Sediments of the St. Anna Trough,” in Geology of Seas and Oceans. Abstracts of Papers of the 12th International School on Marine Geology (Moscow, 1997), Vol. 1, p. 116 [in Russian].
5. E. A. Goilo, V. F. Sapega, and I. A. Andreeva, “Minerals of the Clayey Fraction of the Bottom Sediments of Kola Bay and the Barents Sea,” Zapiski Vserossiiskogo Mineralogicheskogo Obshchestva, No. 2, 101–111 (2001).