PYROXENITE VEINS WITHIN SSZ PERIDOTITES – EVIDENCE OF MELT-ROCK INTERACTION (EGIINGOL MASSIF), MAJOR AND TRACE ELEMENT COMPOSITION OF MINERALS
Evidence of melt-rock reaction between suprasubduction zone (SSZ) peridotites and island arc boninititc and tholeiitic melts are identified. This process is the cause of replacive dunites and pyroxenite veins forming, which are represent the ways of island-arc melts migration. The peridotite-melt in...
שמור ב:
| Principais autores: | , , |
|---|---|
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2017-09-01
|
| סדרה: | Геодинамика и тектонофизика |
| גישה מקוונת: | https://www.gt-crust.ru/jour/article/view/410 |
| תגים: |
אין תגיות, היה/י הראשונ/ה לתייג את הרשומה!
|