List of publications on a keyword: «Stratigraphic scale»

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: 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 tracings of indexes offered by the last two Stratigraphic Codes of the Russian Federation do not create the system of indexes combining the general, regional and local stratigraphic divisions. The "short" indexes which entered practice of stratigraphy under the influence of requirements of cartography do not possess sign of unicity of indexes and specific geological section. Ways of overcoming of the available contradictions are offered.

New educational standards of the higher school assume significant increase in hours of independent work of students. These hours are used for the solution of creative tasks, student's scientific researches. Students study requirements imposed to formulations of scientific definitions, use the subject and predicate analysis in the solution of problems of classification of definitions of facies, choose or make such definition of facies which is used further as the instrument of creation of facial

Tasks of the paleostruktural analysis have not only theoretical and practical, but also didactic value. It is caused by specifics of simultaneous use of stratigraphical and geochronological scales and applications of methods of the tectonic analysis of geological record taking into account facies. The solution of problem of search of anticlinal traps of oil with use of the paleostruktural analysis and methods of historical geotectonics surely is followed by the facial analysis.