List of publications on a keyword: «стратиграфия»

Summary: elements of development of critical thinking of students on examples of the solution of geological tasks of courses of a stratigraphy, the facial analysis, historical geology and paleontology are approved.

Summary: between the general stratigraphic scale of a phanerozoic eonothem and the general geochronologic scale there is one-to-one correspondence (bijection). For demonstration of bijection the piece of a stratigraphic scale, to the corresponding Phanerozoic is chosen. Expansion of a scale to the Archean inclusive is possible. Bijective scales are united in a geocontinuum which forms with Cambrian, Ordovician, Silurian, Devonian, etc. The scale of a new type is made by association of three scales: stratigraphic, geochronologic, geocontinuum scales. The scale of new type possesses wider didactic, etc. opportunities.

Summary: between the general stratigraphy scale of the Permian system and the general geochronologic scale of the Permian there is one-to-one correspondence (so-called "bijection" by the theory of the Cantor). Couples of such divisions are considered: System – Period, Series – Epoch, Stage – Age. For demonstration of bijections the piece of the International Chronostratigraphic Chart corresponding to the Perm system is chosen. Divisions which volume and content are proved by a biostratigraphic method treat the straton possessing property of bijection. The Permian system, its departments, tiers treat such divisions.

Summary: idea of the Perm system of rocks as independent and special part of the general international stratigraphic scale entered geological science in 1841, thanks to opening of the Scottish scientist R.I. Murchison. Murchison called a new system of the general stratigraphic scale (and, respectively, the Permian Period of a geochronologic scale) on the Perm province. The short valid name of these divisions – perm. This name was included forever into geological science and practice as outstanding achievement, according to the academician B. S. Sokolov, "a heroic era" of great discovery in geology. It is an absolute geological and historical priority of Perm and Perm Krai. Most the concept "Permian Period" which is now used not only in geology was widely adopted, but also is a widespread brand. The "Permian Period" brand is used in tourist and nature protection subject, in cultural science, in scenic activity of various creative groups and performers of music and songs, in educational

The Preural regional deflection passes three stages of development during the Permian Period of the Palaeozoic Era: sea, lagunny and continental. These stages correspond to three stages of geotectonic development. The field route from Perm to Kungur, allows to unite further in the wildlife area Cis-Urals and Ust-Kishertsky district in lectures, laboratory and field researches of the data from fundamental geological disciplines, to illustrate them on laboratory researches and to show on such natural exposures of rocks as Pervogorod, Bershet, Ergach-Sarkayevsky and Falcon, Filippovsky, Kungur Ice Cave, the Stone Yermak, dolomitic and other careers of Ust-Kishertsky district.

At the Geological Faculty of the Perm State National Research University reports on several geological sections annually are heard. The traditional section "Geology in English" works. Participation in conference in English helps students and graduate students to gain experience for the subsequent performances at scientific conferences abroad and in Russia.