Layer boundaries as spatial-temporal formations
Authors:
Abstract
The change of layers in sections of sedimentary strata, as it is known, is evidence of the change of conditions of sedimentation. At the same time, the boundaries between the layers may have varying degrees of expression.
Область исследования:
(Archived) Without section
References
- Vassoevich N.B. Layering in the light of the doctrine of sedimentary differentiation. - Izv. of the Academy of Sciences of the USSR, ser. geol. 1950. № 5.
- Geological Dictionary. M., Nedra, 1973. V. 2.
- Golovkinsky N.A. On the Permian Formation in the central part of the Kamsko-Volga Basin. - In the book; Materials for the Geology of Russia. St. Petersburg, ed. of the Mineralogical Society, 1869. V. 1.
- Odessky I.A. Models of Terrigenous Sedimentary Basins of Shelf Zones. - In: Sedimentation in shelf zones. L., ed. PGO "Sevmorgeologiya", 1983.
- Stepanov D.L. Principles and Methods of Biostratigraphic Investigations. - Proc. VNIGRI, 1958. vol. 113.
Similar articles
Analysis of the spatial relationship of the leading sedimentation regimes in the search for building material deposits in the Anthropogenic strata
1988 N. F. Astafiev
Temporal and spatial periodicity - the main regularity of the regressive stage of metamorphism
1988 V. N. Morakhovsky
Spatial and temporal correlation of landforms and sedimentation cycles in Quaternary sediments of the Kaliningrad region
1988 E. L. Kamenetskaya, I. I. Grushevsky