Теплогенерация пород фундамента центральной части Восточно-Европейского кратона

  • Виктор Николаевич Глазнев Воронежский государственный университет https://orcid.org/0000-0002-1016-1866
  • Ольга Михайловна Муравина Воронежский государственный университет https://orcid.org/0000-0003-4772-0825
  • Михаил Вениаминович Минц Геологический институт РАН (ГИН РАН) http://orcid.org/0000-0001-7015-6586
  • Дарья Максимовна Чернышова Воронежский государственный университет
Ключевые слова: Восточно-Европейский кратон, докембрийский фундамент, теплогенерация пород

Аннотация

Введение: Рассматриваются общие принципы создания комплексных геофизических моделей литосферы центральной части Восточно-Европейского кратона и роль геотермических моделей в таких построениях. С целью формирования достоверного начального приближения термической модели верхней коры выполнено обобщение данных о содержании теплогенерирующих элементов в породах раннедокембрийского фундамента. Исходные данные: Рассмотрены особенности валового содержания редких и рассеянных элементов, полученные методом индуктивно-связанной плазменной масс-спектрометрии, в образцах типичных пород региона исследований. Составлена сводная база данных по содержанию теплогенерирующих элементов (калия, тория, урана) и валовому содержанию кремнезёма в типичных породах кристаллического фундамента платформы. Оценка теплогенерации пород фундамента: На основе исходных материалов о концентрации радиогенных элементов был выполнен расчёт теплогенерации пород кристаллического фундамента территории. Для оценки величин теплогенерации использовались сведения о плотности пород фундамента Восточно-Европейского кратона и его отдельных частей. Полученные результаты оценок теплогенерации характеризуют верхнюю неоднородную часть фундамента, распространяющуюся до нижней границы гравиактивного слоя региона. Анализ данных и обсуждение: Для Воронежского кристаллического массива получена величина теплогенерация пород раннедокембрийского фундамента, варьирующая в диапазоне от 0.1 до 7.54 мкВт/м3 со средним значением 0.528 мкВт/м3. Анализ данных показал отсутствие корреляции между плотностью пород фундамента региона и рассчитанными величинами их теплогенерации. Выявлена устойчивая связь содержания кремнезёма (SiO2) с величиной рассчитанной теплогенерации пород. Для главных групп пород фундамента установлена тенденция связи теплогенерации с составом пород, и отсутствие связи с возрастом формирования пород. Заключение: Сформулированы основные результаты проведённого исследования и намечены пути формирования начального приближения для теплогенерации верхнего слоя земной коры в термической модели литосферы региона.

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Биографии авторов

Виктор Николаевич Глазнев, Воронежский государственный университет

д.ф.-м.н., профессор, заведующий кафедрой геофизики, Воронежский государственный университет, Воронеж, Российская Федерация

Ольга Михайловна Муравина, Воронежский государственный университет

д. т. н., профессор кафедры геофизики, Воронежский государственный университет, Воронеж, Российская Федерация

Михаил Вениаминович Минц, Геологический институт РАН (ГИН РАН)

д. г.-м. н., главный научный сотрудник, Геологический институт РАН (ГИН РАН), Москва, Российская Федерация

Дарья Максимовна Чернышова, Воронежский государственный университет

магистр кафедры геофизики Воронежский государственный университет, Воронеж, Российская Федерация

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Опубликован
2021-10-05
Как цитировать
Глазнев, В. Н., Муравина, О. М., Минц, М. В., & Чернышова, Д. М. (2021). Теплогенерация пород фундамента центральной части Восточно-Европейского кратона. Вестник ВГУ. Серия: Геология, (3), 60-78. https://doi.org/10.17308/geology.2021.3/3651
Раздел
Геофизика

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