Section of the “Albatross” Quaternary Sediments
- 作者: Komarov V.N1, Vaitieva Y.A1, Goryachev I.A1, Dumnova A.A1
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隶属关系:
- Sergo Ordzhonikidze Russian State Geological Prospecting University
- 期: 编号 3 (2023)
- 页面: 64-68
- 栏目: Articles
- URL: https://journals.eco-vector.com/0032-874X/article/view/631028
- DOI: https://doi.org/10.7868/S0032874X23030079
- ID: 631028
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详细
The outcrop of quaternary sediments located on the coast of the Kazantip Bay, in the vicinity of the village of Novootradnoye, 300 m south-southeast from the guest house “Albatross” has been studied. The studied continental rocks are probably of eluvial origin. However, a significant amount of sand in their composition may indicate the participation of the deluvial process in their formation — temporary flow associated erosion of bedrock on the uplands located to the south, as well as strong aeolian activity, traces of which are manifested in the form of dusty high-carbonate loess-like loams. The formation of sediments, apparently, occurred during the middle subboreal warming (4800–3400 years ago) and coincides with the period of increasing climate aridization.
作者简介
V. Komarov
Sergo Ordzhonikidze Russian State Geological Prospecting University
Email: komarovmgri@mail.ru
Moscow, Russia
Yu. Vaitieva
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
I. Goryachev
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
A. Dumnova
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
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