Raman confirmation of microdiamond in the Svartberget Fe-Ti type garnet peridotite, Western Gneiss Region, Western Norway
Author:
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-3121.2008.00820.x/fullpdf
Reference47 articles.
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2. Paleozoic diamonds within a Precambrian peridotite lens in UHP gneisses of the Norwegian Caledonides;Brueckner;Earth Planet. Sci. Lett.,2002
3. Introduction with review of the definition, distribution and geotectonic significance of ultrahigh pressure metamorphism
4. Ultrahigh pressure metamorphism in the Western Gneiss Region of Norway
5. On multi-phase mineral inclusions associated with microdiamond formation in mantle-derived peridotite lens at Bardane on Fjortoft, west Norway;Carswell;Eur. J. Mineral.,2005
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