Отправить статью по E-mail Formation mechanism of diapirs of relict lagoonal sediments on the underwater slope of the Curonian Spit
- Авторы: Sergeev A.Y.1,2, Zhamoida V.A.1,2
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Учреждения:
- Karpinsky Russian Geological Research Institute
- Immanuel Kant Baltic Federal University
- Выпуск: Том 52, № 3 (2017)
- Страницы: 226-233
- Раздел: Article
- URL: https://journals.rcsi.science/0024-4902/article/view/162519
- DOI: https://doi.org/10.1134/S0024490217030051
- ID: 162519
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Аннотация
Geological-geophysical methods were applied to provide deeper insight into the nature of unique relict lagoonal sediments exposed on the underwater slope of the Curonian Spit. The study of textural features and morphology of the deformed lagoonal sediments indicates a similarity of their formation mechanism with clay diapirism. Analysis of seismoacoustic data and side scan sonar survey allowed us to establish the configuration of paleolagoon and to determine the direction of dune migration in the past.
Об авторах
A. Sergeev
Karpinsky Russian Geological Research Institute; Immanuel Kant Baltic Federal University
Автор, ответственный за переписку.
Email: sergeevau@yandex.ru
Россия, Srednii pr. 74, St. Petersburg, 199178; ul. A. Nevskogo 13, Kaliningrad, 236016
V. Zhamoida
Karpinsky Russian Geological Research Institute; Immanuel Kant Baltic Federal University
Email: sergeevau@yandex.ru
Россия, Srednii pr. 74, St. Petersburg, 199178; ul. A. Nevskogo 13, Kaliningrad, 236016
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