Quantification of Alpine Metamorphism in the Edolo Diabase, Central Southern Alps
The Southern Alps are the retro-vergent belt of the European Alps that developed from Late Cretaceous subduction to Neogene times. The most prominent Alpine thrusts and folds, nowadays sealed off by the Adamello intrusion, were already developed before the continental collision and clasts derived fr...
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| Автори: | , , , , , , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
MDPI AG
2022-08-01
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| Серія: | Geosciences |
| Предмети: | |
| Онлайн доступ: | https://www.mdpi.com/2076-3263/12/8/312 |
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