Scapolite pegmatite from the Nordøyane ultra-high pressure domain, Western Gneiss Region, Norway: Partial melting driven by infiltration of mantle-derived fluid-Reference-Cited by-同舟云学术

Scapolite pegmatite from the Nordøyane ultra-high pressure domain, Western Gneiss Region, Norway: Partial melting driven by infiltration of mantle-derived fluid

Published:2020-07 Issue: Volume:364-365 Page:105546
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Bryden C.D.,Jamieson R.A.

Funder

Natural Sciences and Engineering Council of Canada

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference76 articles.

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5. Stable Isotope Chemistry and Geochronology of Scapolite-Bearing Pegmatites in Nordøyane, Western Gneiss Region, Norway: A Monitor for the Role of Fluids in (Ultra)-High Pressure Partial Melting;Bryden,2017

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