- PII
- S30345065S2686739725030062-1
- DOI
- 10.7868/S3034506525030062
- Publication type
- Article
- Status
- Published
- Authors
- Volume/ Edition
- Volume 521 / Issue number 1
- Pages
- 52-61
- Abstract
- The article presents the results of geochemical analysis of samples of stones and limestones from a fragment of the Lower carboniferous section of Cape Waring on Wrangel Island. It is shown that not all the ratios used in the analysis of the conditions of formation of silicon and carbonate rocks can be used in interpretation. The identification of the influence of hydrothermal action on the formation of rocks is determined unambiguously by geochemical data. The biogenic/abiogenic origin of flints and the presence of terrigenous impurities in limestones are also unambiguously established. However, the genesis of carbonate and flint rocks in terms of lithological and stratigraphic characteristics does not coincide with what is established by geochemical parameters. This is primarily due to the presence of a terrigenous impurity in limestones, which changes the characteristics of carbonate rocks.
- Keywords
- остров Врангеля кремни известняки геохимия нижнекаменноугольные отложения
- Date of publication
- 25.11.2024
- Year of publication
- 2024
- Number of purchasers
- 0
- Views
- 54
References
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