Structural characteristics and Re–Os dating of quartz-pyrite veins in the Lewisian Gneiss Complex, NW Scotland: Evidence of an Early Paleoproterozoic hydrothermal regime during terrane amalgamation

Autor: Vernon, R., Holdsworth, R.E., Selby, D., Dempsey, E., Finlay, A.J., Fallick, A.E.
Zdroj: In Precambrian Research June 2014 246:256-267
Databáze: ScienceDirect