МЕТАКОНГЛОМЕРАТИ ДОКЕМБРІЮ УКРАЇНСЬКОГО ЩИТА – НАЙВАЖЛИВІШІ СТРАТИГРАФІЧНІ РЕПЕРИ ТА ПОТЕНЦІЙНО РУДОНОСНІ ОБ’ЄКТИ

Автор(и)

  • В.В. Покалюк Державна установа "Інститут геохімії навколишнього середовища НАН України", Україна https://orcid.org/0000-0002-9282-0246
  • В.Г. Верховцев Державна установа «Інститут геохімії навколишнього середовища НАН України», Україна https://orcid.org/0000-0002-1015-6725
  • Д.В. Чарний Державна установа «Інститут геохімії навколишнього середовища НАН України», Україна https://orcid.org/0000-0001-6150-6433

DOI:

https://doi.org/10.30836/igs.1025-6814.2025.3.330831

Ключові слова:

Український щит, архей–протерозой, метаконгломерати, стратиграфія, кореляція, рудоносність

Анотація

Узагальнено відомості про докембрійські метаконгломерати Українського щита та його схилів. Розглянуто стратиграфічне положення, речовинний склад, літолого-генетичні особливості та рудоносність метаконгломератів і метатеригенних комплексів, що їх вміщують. Надано порівняльну характеристику літологічних типів метаконгломератів різних стратиграфічних рівнів докембрію України. Запропоновано типізацію метаконгломератів за низкою критеріїв (стратиграфічних, речовинних, структурних) для цілей історико-геологічного аналізу, металогенічної та пошукової оцінки на деякі види корисних копалин, насамперед на золото, уран, торій, рідкісні землі. Власне метаконгломерати на Українському щиті відомі починаючи від основи палеопротерозою. Різні стратиграфічні рівні нагромадження конгломератів виявляють характерні відмінності в особливостях локалізації та просторового розміщення. Всі рівні специфічні за речовинним складом і літологічними особливостями конгломератів, що є найважливішим корелятивним критерієм під час стратиграфічних зіставлень. Серед докембрійських метапсефітових порід Українського щита діагностуються/реконструюються різноманітні літолого-фаціальні та літолого-петрографічні типи, притаманні фанерозойським конгломератам. Характерна відсутність серед метаконгломератів тилітів або тилоїдів. Цілком виразно простежується послідовне зростання потужностей псефітів, а також ступеня їхньої поліміктності від архею до мезопротерозою. Як для нижньої, так і верхньої половин палеопротерозою Українського щита характерні в основному трансгресивні послідовності грубоуламкових конгломератовмісних формацій.

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