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...
Gespeichert in:
| Datum: | 2013 |
|---|---|
| 1. Verfasser: | |
| Format: | Artikel |
| Sprache: | Ukrainisch |
| Veröffentlicht: |
Institute of Geological Sciences of the Ukrainian National Academy of Sciences
2013
|
| Schlagworte: | |
| Online Zugang: | http://ts.igs-nas.org.ua/article/view/93710 |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| Назва журналу: | Tectonics and stratigraphy |
Institution
Tectonics and stratigraphy| Zusammenfassung: | 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). |
|---|