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Петрографический кодекс России. Магматические, метаморфические, метасоматические, импактные образования / Отв. ред. Шарпенок Л. П. СПб: Изд-во ВСЕГЕИ. 2009. 200 с.
Petrographic Code of Russia is a set of fundamental rules and recommendations approving and confirming the unified and standardized petrographic terminology and nomenclature of endogenic and coptogenic formations, as well as the taxonomy of petrographic units. The unified notional base, which forms the basis of the Petrographic Code, is used during compilation of the State Geological Maps at different scales, serial legends to them, during forecast-prospecting works, thematic investigations, as well as during map compilation in the framework of international projects.

The Code of the second and third editions has a new structure as compared to the first one, new appendices are prepared. Taking into account new requirements of the geological practice, new sections on sedimentary-volcanogenic formations, migmatites etc. are added. Sections related to metamorphic and metasomatic formations are reworked; distinguishing of fluid-explosive rocks bearing different mineral types into an individual genetic type is substantiated. The content of most of previous provisions is changed; many articles are reworked or abbreviated, new ones are included. Recommendations of the Commission on Systematics in Petrology of the International Union of Geological Sciences are taken into account during development of the Code.
Петухов С.И., Анохин В.М., Мельников М.Е. Особенности геодинамических обстановок в районе Северо-Западного звена Магеллановых гор (Тихий океан) // Вестник КРАУНЦ. Серия: Науки о Земле. 2012. Вып. 20. № 2. С. 78-88.
A lineament analysis of the relief was made using a detailed bathymetry map of the region drawn according to the results of multi-beam echo-sounding. The authors separated linear objects of the relief, measured their course azimuths, plotted the rose diagram of the lineament directivities of the region, and built the models of the surface and subsurface deformation field of the region at separating the blocks of dominant stress and strain. The blocks travel along the lines of alternation of stress sign (block borders). The directivities
of the block borders were compared with the lineaments directivities resulting in conclusion that they both have spatial and generic relations. The systems of linear forms directivities of the relief and the borders of surface and subsurface blocks partially correspond to the four main systems of the global disjunctive network (planetary fracturing), which suggests a considerable influence of the latter on the structural plan of the region.Redistribution of stresses is associated with the modern geological processes leading to the formation of new
configurations of seabed relief and partial destruction of the old surfaces of guyots.
Пийп Б.И. Активность вулкана Толбачик (январь 1941 г.) // Бюллетень вулканологических станций. 1946. № 12. С. 70-73.
Пийп Б.И. Вулкан Кизимен // Бюллетень вулканологических станций. 1946. № 13. С. 22-32.
Пийп Б.И. Вулкан Толбачик // Бюллетень вулканологических станций. 1954. № 20. С. 69-71.
Пийп Б.И. Вулканизм / Большая Советская Энциклопедия, 2-е изд.. М.: Советская энциклопедия. 1951. Т. 9. С. 393
Пийп Б.И. Вулканическая бомба / Большая Cоветская Энциклопедия, 2-е изд.. М.: Советская энциклопедия. 1951. Т. 9. С. 393
Пийп Б.И. Вулканические газы / Большая Cоветская Энциклопедия, 2-е изд.. М.: Советская энциклопедия. 1951. Т. 9. С. 393-394.
Пийп Б.И. Вулканические горные породы / Большая Cоветская Энциклопедия, 2-е изд.. М.: Советская энциклопедия. 1951. Т. 9. С. 394-395.
Пийп Б.И. Вулканологическая хроника // Бюллетень вулканологических станций. 1946. № 12. С. 79-80.