No mafic layer in 80 km thick Tibetan crust
Crustal doubling in Tibet and the Himalayas by underthrusting of the Indian plate is thought to require the presence of a mafic layer above the Moho. Here, the authors present seismic data which shows that the middle Lhasa Terrane has very low velocity (V p < 6.7 km/s) throughout the 80 km thick...
Enregistré dans:
| Auteurs principaux: | , , |
|---|---|
| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2021
|
| Sujets: | |
| Accès en ligne: | https://doaj.org/article/407344e26f1e4ae1a8d81fdced375f40 |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|