Синхронность развития палеопротерозойского феномена «Шуньга» в бассейнах-аналогах

  • Михаил Михайлович Филиппов ФГБУН Институт геологии КарНЦ РАН, Российская Федерация, 185920, Петрозаводск, ул. Пушкинская, 11
  • Кирилл Игоревич Лохов Санкт-Петербургский государственный университет, Российская Федерация, 199034, Санкт-Петербург, Университетская наб., 7–9 https://orcid.org/0000-0003-3622-3583

Аннотация

Последовательность взаимосвязанных событий — от накопления до вторичного концентрирования и рассеивания органического вещества — характеризуется уникальным для палеопротерозоя феноменом «Шуньга», наиболее полно исследованным в Онежском осадочном бассейне. Основной этап — накопление гигантских объемов первичного органического вещества, а также последующие этапы его перераспределения — многочисленные купольные и субпластовые локальные тела высокоуглеродистых пород с характерной дифференциацией состава; разнообразные формы проявления антраксолитов, указывающие на реализованную полномасштабную генерацию углеводородов (УВ); многочисленные типы коллекторов, свидетельствующие об их миграции; следы переотложения и первичного, и новообразованного органического вещества. В обзоре на примере бассейна Франсвиль приведены доказательства существования всех этапов феномена в бассейнах-аналогах, в которых основной этап развивался синхронно. Детально проанализированы результаты датировок отложений двух бассейнов, выявлены принципиальные ошибки в трактовке геохронологических данных. Показано, что корреляция разрезов палеопротерозойских осадочных бассейнов возможна по геохимическим маркирующим горизонтам с аномалиями δ13Сорг (Сорг — органический углерод) и повышенным содержанием U, Mo, Se, As, Ni и V.

Ключевые слова:

признаки феномена, Онежская структура, бассейн Франсвиль, возраст, геохимические аномалии, кероген, генерирование и миграция углеводородов, коллекторы

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Литература

Литература

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Опубликован
2018-11-15
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Филиппов, М., & Лохов, К. (2018). Синхронность развития палеопротерозойского феномена «Шуньга» в бассейнах-аналогах. Вестник Санкт-Петербургского университета. Науки о Земле, 63(3), 363-393. https://doi.org/10.21638/spbu07.2018.307
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