A New Magma Type in the Continental Collision Zone. The Case of Capraia Island (Tuscany, Italy)
The Tuscany Magmatic Province consists of a Miocene to Pleistocene association of a wide variety of rock types, including peraluminous crustal anatectic granites and rhyolites, calcalkaline and shoshonitic suites and ultrapotassic lamproites. In addition to the magma types already recognised, the oc...
Main Author: | Alba Patrizia Santo |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2021-02-01
|
Series: | Geosciences |
Subjects: | |
Online Access: | https://www.mdpi.com/2076-3263/11/2/104 |
Similar Items
-
Composition and evolution of the continental crust: Retrospect and prospect
by: J.L.R. Touret, et al.
Published: (2022-09-01) -
Origin and evolution of the deep continental crust /
by: Karmalkar, N. R.
Published: (c201) -
Late Mesozoic adakite granites of the southern frame of the eastern flank of the Mongol-Okhotsk orogenic belt: material composition and geodynamic conditions of formation
by: I. M. Derbeko, et al.
Published: (2020-09-01) -
Andesites and evolution of the continental crust: Perspectives from the Central Volcanic Zone of the Andes
by: Dale H. Burns, et al.
Published: (2023-01-01) -
Mobilization of Cu in the continental lower crust: A perspective from Cu isotopes
by: Chen-Hao Luo, et al.
Published: (2023-09-01)