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1.      Treatment of strain of a particle, in accordance with continuous medium mechanics, as one of the components of tectonic flow, alongside with translation and rotation of this particle. Description of quantitative interrelation of fields of these three components.
2.      An idea about a relativity of concept of strain uniformity, with reference to bodies of a different scale and about "a hierarchical alternation " of homogeneous and heterogeneous strain.
3.      Treatment of general stress as a combination of comprehensive compression and deviatory stress; definition of a role of these components in strain of a particle.
4.      Treatment of stress field as a derivative of strain velocity field (as against traditional idea about this field as a derivative of external forces).
5.      Accent on a relativity of concepts of ductile and brittle strain depending on a ratio of sizes of: (a) bodies, and (b) ruptures breaking these bodies. Treatment of brittle strain of some volume of medium as a mechanism of ductile strain of a larger volume, alternative of ductile strain of a proportionate volume and coordinator of ductile strain of smaller volumes. Treatment of rupturing as a limiting case of heterogeneity of strain, as well as treatment of faulting as a limiting case of instability of ductile strain. Indication on energetic underlying reason of such instability.
6.      Revealing cases of simplification of analogue modeling at automatic performance of similarity conditions.
7.      Accent on dependence of strain properties of geological bodies on their rank and size (minerals, rocks, or bedded formations). Indication on overestimate of an estimation of viscosity of all the lithosphere mantle according to viscosity of its main rock-forming minerals such as olivine.
8.      Description of conditions of functioning of convection in linear or dome forms, depending on Rayleigh number. Indication on linear form of convection as a possible cause of formation of linear rises and depressions, without influence of external horizontal compression.
9.      Ranging natural indicators of strain in the Earth's crust with indication on strain of objects of a different scale: (a) intralayer strain, (b) strain of rock layers, (c) strain of packets of layers, (d) strain of bedded formations, and (e) strain of rock massifs.
10.      Examples of quantitative estimation of stress value in some elementary cases. Indication on a rather low stress value in the Earth's crust, capable to cause significant ductile strain.
11.      Introduction to concept of elementary geodynamic conditions and definition of their minimum by means of combinatory analysis. Idea of real geodynamic conditions in the Earth's crust as a combination of elementary conditions.
12.      Definition of a spatial combination of elementary geodynamic conditions and corresponding structural parageneses as a result of balanced arrangement of tectonic flow in the Earth's crust. Idea of this arrangement as a consequence of such a fundamental property of geological continuous medium as its continuity.
13.      Idea of mutual balancing of vertical and horizontal tectonic movements and of balancing (in chessboard order) of horizontal compression, at some sites, by horizontal stretching at adjacent (in horizontal and vertical direction) sites.
14.      Indication on two "competing" forms of superficial horizontal stream: (a) in the solid state (thrusts); and (b) in the "disintegrated" state (denudation and balanced sedimentation).
15.      Indication on consecutive imposing different structural parageneses within domains of geological medium at participation of these domains in translation, rotation and strain in the process of balanced tectonic flow.
16.      Analysis of mechanism of structural forms formation and their aggregates (structural parageneses) from positions of structured medium mechanics.
17.      Treatment of thrust kinematics as one of the parts of balanced arrangement of tectonic flow.
18.      Treatment of transform faults of mid-ocean ridges as an original "mega-cleavage", displacement along which occurs, as well as in the case of cleavage of fold belts, in "forbidden" direction, that is parallel to the maximal stretching axis.
19.      Rank analysis of geodynamic conditions and corresponding structural parageneses, with allocation of a triad "enclosed" each other "geodynamic" (and corresponding geological) bodies: a geodynamic (structural) system, a geodynamic (structural) cell, a geodynamic (structural) domain. Treatment of a geodynamic (structural) domain of lower (large-scale) rank as a geodynamic (structural) system of higher (small-scale rank). Introduction to concept of a  rank  hierarchy of systems, cells and domains.
20.      Ordering lacks of prevailing modern geodynamic paradigm, i. e. plate tectonics, and attempt of their elimination by means of creating a concept of geodynamics of hierarchically interacting geospheres, with revealing, within these geospheres, geodynamic and structural systems, cells and domains of a different rank. Treatment of the whole spectrum of structures of the Earth within the framework of this concept.
21.      Revealing a non-rank "geodynamic constant", that is a ratio of thickness of each geodynamic system to duration of geodynamic cycle of corresponding rank.
22.      Ascertaining connection of hierarchical geodynamics and metallogeny. 

 См. также
Аннотации книгУчебное пособие "Введение в тектонофизику". Гончаров М. А., Талицкий В. Г., Фролова Н. С. Ответ. Ред Короновский Н.В.
ДиссертацииНовейшая сдвиговая тектоника осадочных бассейнов: тектонофизический и флюидодинамический аспекты (в связи с нефтегазоносностью):
ДиссертацииНовейшая сдвиговая тектоника осадочных бассейнов: тектонофизический и флюидодинамический аспекты (в связи с нефтегазоносностью): Общая характеристика работы.
Научные статьиТезисы научной конференции ЛОМОНОСОВСКИЕ ЧТЕНИЯ, ноябрь 2011 года СЕКЦИЯ ГЕОЛОГИЯ:

Проект осуществляется при поддержке:
Геологического факультета МГУ,
РФФИ
   

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