Carbonatitic versus hydrothermal origin for fluorapatite REE-Th deposits: Experimental study of REE transport and crustal “antiskarn” metasomatism

Michael Anenburg; John A. Mavrogenes

doi:10.2475/03.2018.03

Loading [Contrib]/a11y/accessibility-menu.js

Anenburg, M., & Mavrogenes, J. A. (2018). Carbonatitic versus hydrothermal origin for fluorapatite REE-Th deposits: Experimental study of REE transport and crustal “antiskarn” metasomatism. American Journal of Science, 318(3), 335–366. https://doi.org/10.2475/03.2018.03

View more stats

Carbonatitic Versus Hydrothermal Origin for Fluorapatite REE-Th Deposits: Experimental Study of REE Transport and Crustal “Antiskarn” Metasomatism