ПРО СТРУКТУРУ ЧОРНОМОРСЬКОГО БАСЕЙНУ ЯК ІЄРАРХІЧНУ СИСТЕМУ МЕГАПУЛ-АПАРТІВ
DOI:
https://doi.org/10.30836/igs.0375-7773.2020.216036Ключові слова:
Чорноморський басейн, тектонолінеаменти, pull-apart, планетарна розломна мережа, розломно-блокова тектоніка, зсувна тектонікаАнотація
У статті наведено геолого-структурну аргументацію морфогенезу западин і прогинів Чорного моря як різнорангових пул-апартів області перетину трансреґіональних ПЗ і СПС тектонолінеаментів. Ансамбль структур Чорного моря (глибоководних западин, розломних зон, периферійних прогинів і підняттів) представлений як похідне істотно зсувних деформацій і малоамплітудних дислокацій зон трансреґіональних тектонолінеаментів. Структурні малюнки, відомі для моделей простого зсуву, виявлено в зонах динамічного впливу розломів, що обмежують чорноморські западини. Структурні позиції западин показано на тлі перетину розломних зон у системах північно-західних і північно-східних тектонолінеаментів як регіональних елементів регматичної глобальної мережі. Аналіз впорядкованих сукупностей розломно-блокових структур у плані басейну за аналогією з моделями (mega)pull-apart виявляє ієрархічні, (пара)генетичні і успадковані зв’язки у морфогенезі западин, прогинів і підняттів Чорного моря. Особливості будови (мега) пул-апартових глибоководних западин Чорного моря й позиції структур другого рангу, периферійних прогинів (і валів) акваторії опосередковано виражають «пілотний» і контролівний вплив регмагенезу в «рамі» пересічних ПЗ і ПС зон тектонолінеаментів і складників їхніх транскурентних глибинних розломів-зсувів у режимі транстенсії. (При)зсувні позиції розломно-блокових структур басейну, локальних геологічних тіл, ареалів вулкано-плутонітів, «продуктів» тектономагматичних активізацій розкривають закономірну регуляторну дію ротаційних чинників істотно зсувної малоамплітудної тектоніки земної кори, а також важливу роль зональних додаткових критеріїв прогнозування потенційних зон вуглеводнів і ділянок з тектонофізичними умовами розтягування.
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