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ИЗОТОПНЫЙ СОСТАВ ГАЗОВ МАГМАТИЧЕСКИХ И ОСАДОЧНЫХ ВУЛКАНИЧЕСКИХ СИСТЕМ: АНАЛИТИЧЕСКОЕ ОБОБЩЕНИЕ И СРАВНИТЕЛЬНЫЙ АНАЛИЗ
Институт геологии и геофизики НАН Азербайджана
Журнал: Геофизические процессы и биосфера
Том: 22
Номер: 2
Год: 2023
Страницы: 59-74
УДК: 550.8.053
DOI: 10.21455/GPB2023.2-2
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Фейзуллаев А.А. ИЗОТОПНЫЙ СОСТАВ ГАЗОВ МАГМАТИЧЕСКИХ И ОСАДОЧНЫХ ВУЛКАНИЧЕСКИХ СИСТЕМ: АНАЛИТИЧЕСКОЕ ОБОБЩЕНИЕ И СРАВНИТЕЛЬНЫЙ АНАЛИЗ // Геофизические процессы и биосфера. 2023. Т. 22. № 2. С. 59-74. DOI: 10.21455/GPB2023.2-2
@article{ФейзуллаевИЗОТОПНЫЙ2023,
author = "Фейзуллаев, А. А.",
title = "ИЗОТОПНЫЙ СОСТАВ ГАЗОВ МАГМАТИЧЕСКИХ И ОСАДОЧНЫХ ВУЛКАНИЧЕСКИХ СИСТЕМ: АНАЛИТИЧЕСКОЕ ОБОБЩЕНИЕ И СРАВНИТЕЛЬНЫЙ АНАЛИЗ",
journal = "Геофизические процессы и биосфера",
year = 2023,
volume = "22",
number = "2",
pages = "59-74",
doi = "10.21455/GPB2023.2-2",
language = "Russian"
}
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Ключевые слова: магматические/гидротермальные и осадочные вулканические системы, газ, химический и изотопный состав, сравнительный генетический анализ.
Аннотация: В статье представлены итоги анализа большого объема литературных данных и результатов собственных исследований автора по изучению изотопно-химического состава газов магматических и осадочных вулканических систем. Обработка данных и соответствующие графические построения выполнялись с помощью стандартных компьютерных программ. На основе известных критериев проведено сравнение и установлена генетическая природа газов рассмотренных систем. Показано, что содержание абиогенного метана в магматической/гидротермальной системе по сравнению с его содержанием в осадочной системе незначительно (не превышает 1 %). Этот факт, а также изотопный состав углеродсодержащих газов и гелия (R/Ra) позволили сделать следующие выводы:
– углеводородные (УВ) газы рассмотренных вулканических систем имеют различный генетический источник: а) абиогенный – в магматической и углекислый – в осадочной системах; б) преимущественно абиогенно-биогенный – в гидротермальной системе; в) биогенный (термогенно-микробиальный) – в осадочных вулканах;
– содержание абиогенного метана в магматической/гидротермальной системе незначительно и не превышает 1 %;
– изотопный состав СО2 и отношение изотопов радиогенного и воздушного аргона (40Ar/36Ar) в магматической вулканической системе изменяется в очень узких пределах по сравнению с осадочной. Тем не менее использование этих параметров в качестве однозначного генетического критерия не представляется возможным.
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