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Vol 22
Pages:
37-51
Download volume:
RUS
Article
Geology

Microfolding as a result of the process of internal movement of layer material during folding

Authors:
T. O. Zabokritskii
Date submitted:
1947-07-03
Date accepted:
1947-09-17
Date published:
1949-01-11

Abstract

When studying various issues of tectonics in the mines of the Prokopyevsk‑Kiselevsk region, I paid special attention to the study of folds developed within one layer or even in part of a layer. Hence, these folds are called microfolds or intralayer folds. The development of microfolding is observed not only in the mines of Kuzbass, Donbass or other coal basins, but also in all folded areas. However, different researchers attached different significance to this phenomenon, and the origin of microfolds was often interpreted incorrectly, without connection with observations of the actual material.

Область исследования:
Geology
Keywords:
plications geology tectonics
Funding:

None

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References

  1. Heim A. Understanding the Mechanism of Geological Construction in a Geological Monographic Book of the Three-Dimensional Group. About an Atlas, 2nd vol., Basel, 1878.
  2. Weber V.N. Methods of Geological Surveying, 1934. (in Russian)
  3. Vysotskii I.V. Field Structural Geology, 1945. (in Russian)
  4. Zabokritskii T.O. Tectonics of the Prokopyevsk-Kiselevsk Region, NIS LGI, 1946-1947. (in Russian)
  5. Lizs Ya.K. Structural Geology, 1935. (in Russian)
  6. General Geology, 1938. (in Russian)
  7. Tetyaev M.M. Fundamentals of Geotectonics, 1941. (in Russian)
  8. Willis R. and Willis B. Structural Geology, 1932. (in Russian)
  9. Usov M.A. Structural Geology, 1941. (in Russian)

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