ИТОГИ ТЕМАТИЧЕСКОГО ЛИТОЛОГИЧЕСКОГО СЕМИНАРА «ЛИТОЛОГИЯ ПАЛЕОКАРСТА»
Журнал: ВЕСТНИК ГЕОНАУК
№ 7
(331) , 2022
Авторы:
1.
ФГБУ ФИЦ «Коми научный центр Уральского отделения Российской академии наук»
Сыктывкар, Республика Коми, Россия
Сыктывкар, Республика Коми, Россия
2.
ФГБУ ФИЦ «Коми научный центр Уральского отделения Российской академии наук»
Тип:
Статья
Страницы:
с 45
по 50
Статус:
Опубликован
Получено:
03.08.2022
Одобрено:
08.01.2023
Опубликовано:
08.09.2022
Язык материала:
русский
Аннотация (русский):
Paleokarst is defined as an ancient karst that is generally buried under younger sediments or sedimentary rocks. Ancient karst and associated subsurface geological features have great scientific importance, because they not only record the past erosional surfaces of the Earth, but also preserve data on the ancient climate and water transport in paleoaquiferous horizons. In addition, some paleokarst areas are repositories of a variety of minerals. Paleokarst is characterized by a variety of morphogenetic occurrences and lithological filling; therefore, the objective of the lithological workshop is to review available modern data on proven and presumed paleokarst, since these data are important for paleogeographic and paleotectonic reconstructions.
Paleokarst is defined as an ancient karst that is generally buried under younger sediments or sedimentary rocks. Ancient karst and associated subsurface geological features have great scientific importance, because they not only record the past erosional surfaces of the Earth, but also preserve data on the ancient climate and water transport in paleoaquiferous horizons. In addition, some paleokarst areas are repositories of a variety of minerals. Paleokarst is characterized by a variety of morphogenetic occurrences and lithological filling; therefore, the objective of the lithological workshop is to review available modern data on proven and presumed paleokarst, since these data are important for paleogeographic and paleotectonic reconstructions.
