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Vol 22
Pages:
37-51
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RUS
Research article
Geology

Plications as a result of the process of internal movement of the substance of the layers during the plications process

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 plications 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 plications was often interpreted incorrectly, without connection with observations of the actual material.

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References

  1. A. Heim. Untersuchungen iiber den Mechanismus der Geblrgsbilduag im Ans hluss an die geologissheMonographic der Todi-Wiudgallen-Gruppe. Mut einem Atlas, 2Bd., Basel, 1878.
  2. Вебер В.Н. Методы геологической съемки, 1934.
  3. Высоцкий И.В. Полевая структурная геология, 1945.
  4. Забокрицкий Т.О. Тектоника Прокопьевско-Киселевского района, НИС ЛГИ, 1946—1947 гг.
  5. Лизс Я.К. Структурная геология, 1935.
  6. Ог. Общая геология, 1938.
  7. Тетяев М.М. Основы геотектоники, 1941.
  8. Уиллис Р. и Уиллис Б. Структурная геология, 1932.
  9. Усов М.А. Структурная геология, 1941.

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