Density heterogeneity of the Earth’s crust of Ukraine and adjacent territories from three-dimensional gravity modelling

І.Б.  Макаренко

doi:10.24028/gzh.v43i2.230190

Автор(и)

І.Б. Макаренко Інститут геофізики ім. С.І. Субботіна НАН України, Україна

DOI:

https://doi.org/10.24028/gzh.v43i2.230190

Анотація

Робота виконана з метою вивчення густинної неоднорідності земної кори України і суміжних регіонів на основі детальних тривимірних гравітаційних моделей земної кори різного масштабу таких тектонічних регіонів і окремих структур: Дніпровсько-Донецької западини і Донбасу, Українського щита (Інгульський мегаблок, Голо- ванівська шовна зона, широтні зони розломів), Чорноморської мегазападини і прилеглих структур. Моделі побудовано з використанням комплексу геологічних, петрофізичних і сейсмічних даних уздовж геотраверсів, профілів ГСЗ, сучасних сейсмічних досліджень методами WARR і розраховано із застосуванням комплексу автоматизованої інтерпретації потенціальних полів GMT-Auto. В результаті отримано нові відомості стосовно розподілу густини в земній корі. Побудовано схеми розподілу густини в об’ємі земної кори України і суміжних регіонів на певних глибинах (поверхня фундаменту, поверхні 10, 20, 30 км, поділ Мохо). Обчислено потужності умовно виділених «гранітного», «діоритового», «базальтового» шарів земної кори і коромантійної суміші для всього регіону дослідження, які в графічному вигляді зображено ізолініями на відповідних схемах. Отримана густинна неоднорідність стала основою для побудови (вперше у тривимірному варіанті) схеми прогнозного складу земної кори з типізацією за співвідношенням потужностей складових її шарів. Неоднорідність сучасної консолідованої кори регіону в цілому охарактеризована схемою поширення областей гранітного, гранітно-діоритового, діоритового і базальтоїдного типів кори. З метою чіткої фіксації розчленування нижнього шару кори, який за класифікацією методом ГСЗ вважають нероздільним, базальтоїдний тип розчлено- вано на 3 підтипи: підтип 1 — із вмістом базальту 40—70 %; підтип 2 — 70—90 %; під- тип 3 повністю базальтовий. Встановлено, що основність земної кори Українського щита змінюється із заходу на схід, відповідно від базальтоїдного до діоритового типу. В межах Дніпровсько-Донецької западини основність кори збільшується з північного заходу на південний схід, підпорядковуючись сегментації структури. У Чорноморській мегазападині і прилеглих структурах переважає базальтоїдний тип кори. Вперше виділено тип кори, який не збігається з відомими і характеризується наявністю в розрізі «базальтового» і «гранітного» шарів (за нульової або дуже малої потужності «діоритового» шару). Подібний тип кори існує в Інгульському мегаблоці щита, у північній бортовій зоні Дніпровсько-Донецької западини, а також у Чорно- морській мегазападині.

Посилання

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