Basic condition of layer formation in the light of the theory of symmetry
Authors:
Abstract
There are several points of view on the conditions of layer formation. One group of researchers sees the main cause of layer formation in geotectonic fluctuations of the Earth's crust, which control the process of sediment accumulation. Other researchers consider the main cause of layer formation to be a change in the conditions of sediment formation as a result of changes in the physical-geographical regime; at the same time, they do not attribute significant importance to the geotectonic factor.
Область исследования:
Geology
Funding:
None
References
- Vistelius A. B. The simplest problems of mathematical processing in lithology and ways of their solution. Litologicheskiy sbornik I. Gostopetkhizdat, 1948. (in Russian)
- Mikheev V. I. Remarks to the article “Curvilinear symmetry” by D. V. Nalivkin. Kristallografiya (Tr. Fedorovskoy nauch. sessii LGI 1949 g.). Metallurgizdat, 1961. (in Russian)
- Nalivkin D. V. Curvilinear Symmetry. Kristallografiya (Tr. Fedorovskoy nauchnoy sessii LGI za 1949 g.). Metallurgizdat, 1951. (in Russian)
- Sarmanov O. V. Creator of the concept of mathematical chain. Priroda, 1956, No. 11. (in Russian)
- Shafranovsky I. I. Symmetry Groups in Structural Petrology. Zapiski Vsesoyuznogo mineralogicheskogo obshchestva, 1956, vol. LXXXV, No. 4. (in Russian)
- Shafranovsky I. I. Universal principle of symmetry and the form of marine pebbles. Mineralogicheskiy sbornik Lvovskogo geologicheskogo obshchestva, 1956, No. 10. (in Russian)
- Shubnikov A. V. About the works of Pierre Curie in the field of symmetry. Uspekhi fizicheskikh nauk, 1956, vol. LIX, iss. 4. (in Russian)
- Yakovlev N. N. Organism and Environment. Izd-vo AN SSSR, 1956. (in Russian)