Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway)

Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway)

Graphite formation in the deep crust during granulite facies metamorphism is documented in the Proterozoic gneisses of the Lofoten–Vesterålen Complex, northern Norway. Graphite schist is hosted in banded gneisses dominated by orthopyroxene-bearing quartzofeldspathic gneiss, including marble, calcsil...

Full description

Bibliographic Details
Main Authors: Ane K. Engvik, Håvard Gautneb, Pål Tore Mørkved, Janja Knežević Solberg, Muriel Erambert
Format: Article
Language:English
Published: MDPI AG 2023-09-01
Series:Minerals
Subjects:
C-isotope
fluid
granulite
graphite
Vesterålen
Online Access:https://www.mdpi.com/2075-163X/13/10/1279

Similar Items

Similar Items