vsgiuВестник Сибирского государственного индустриального университетаBulletin of the Siberian State Industrial University2304 - 44972307-1710Федеральное государственное бюджетное образовательное учреждение высшего образования "Сибирский государственный индустриальный университет"vsgiu-413Research ArticleГорное дело и геотехнологииMining and GeotechnologyУРОВЕНЬ МОРЯ В ПАЛЕОЗОЕ В СВЕТЕ ИНФОРМАЦИИ О РЕГИОНАЛЬНЫХ ПЕРЕРЫВАХ КАМЕННОУГОЛЬНОГО ПЕРИОДАSEA LEVEL IN THE PALEOZOIC IN LIGHT OF INFORMATION ON REGIONAL HITS OF THE CARBONIFEROUS PERIODГутакЯ.М.GutakYa. M.vestnicsibgiu@sibsiu.ruРубанД.А.RubanD. A.vestnicsibgiu@sibsiu.ruСибирский государственный индустриальный университетРоссияSiberian State Industrial UniversityRussian FederationЧереповецкий государственный университетRussian FederationCherepovets State UniversityRussian Federation201804082025032127Copyright © Гутак Я., Рубан Д., 20252025Гутак Я., Рубан Д.Gutak Y., Ruban D.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://vestnik.sibsiu.ru/jour/article/view/413

Перерывы в осадочных последовательностях являются ценными свидетельствами для эффективной реконструкции динамики развития осадочных бассейнов, в том числе с использованием секвенс-стратиграфической методологии. Информация о них может успешно использоваться и при обсуждении колебаний уровня моря в геологическом прошлом планеты (эвстатических флуктуаций). В этой связи представляет интерес обобщение сведений о региональных перерывах для решения вопроса о положении уровня Мирового океана в палеозое относительно мезозоя.

 

Gaps in sedimentary sequences are valuable evidence for the effective reconstruction of the dynamics of sedimentary basin development, including the use of sequence-stratigraphic methodology. Information about them can also be successfully used in discussing sea level fluctuations in the geological past of the planet (eustatic fluctuations). In this regard, it is of interest to generalize information about regional gaps to resolve the issue of the position of the World Ocean level in the Paleozoic relative to the Mesozoic.

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The authors declare that there are no conflicts of interest present.