Stable isotopes (O, H) and quartz geochemistry provide insight to melt source and subsolidus fluid:rock interaction in the Cretaceous Little Nahanni LCT Pegmatites (NWT, Canada)

Author:

Pfister Jérémie D.,Kontak Daniel J.,Groat Lee A.,Fayek Mostafa

Publisher

Elsevier BV

Reference138 articles.

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3. Selwyn plutonic suite and its relationship to tungsten skarn mineralization, southeastern Yukon and District of Mackenzie;Anderson,1983

4. Mineralised Pegmatites of the Damara Belt, Namibia: Fluid Inclusion and Geochemical Characteristics with Implications for Post- Collisional Mineralisation;Ashworth,2014

5. Origin of rare-element-mineralized Damara Belt pegmatites: a geochemical and light stable isotope study;Ashworth;Lithos,2020

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