ЕПІПЛАТФОРМНИЙ РИФТОГЕНЕЗ, ФОРМУВАННЯ ЛЕПТИТОВОЇ ТА АНДЕЗИТО-БАЗАЛЬТОВОЇ ФОРМАЦІЇ ОСНИЦЬКО-МІКАШЕВИЦЬКОГО ВУЛКАНО-ПЛУТОНІЧНОГО ПОЯСУ
The Osnytsk-Mikashevitsky volcano-plutonic belt may be considered as a representative of special intracraton type of volcano-plutonic belts of Early Precambrian in conditions of epiplatform rifting, which was the beginning of the basic restructuring of cratonic crust at the end of the early Proteroz...
Збережено в:
| Дата: | 2013 |
|---|---|
| Автор: | |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Institute of Geological Sciences of the Ukrainian National Academy of Sciences
2013
|
| Теми: | |
| Онлайн доступ: | http://ts.igs-nas.org.ua/article/view/93710 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Tectonics and stratigraphy |
Репозитарії
Tectonics and stratigraphy| Резюме: | The Osnytsk-Mikashevitsky volcano-plutonic belt may be considered as a representative of special intracraton type of volcano-plutonic belts of Early Precambrian in conditions of epiplatform rifting, which was the beginning of the basic restructuring of cratonic crust at the end of the early Proterozoic in central East-European platform. This is evidenced by duration of the belt formation, the inheritance of magmatism, the formation of structure and the variation of paleotectonic conditions from Early Proterozoic till Vend (Mesoproterozoic). |
|---|