Microdiamonds in a megacrystic garnet websterite pod from Bardane on the island of Fjørtoft, western Norway: Evidence for diamond formation in mantle rocks during deep continental subduction-Reference-Cited by-同舟云学术

Microdiamonds in a megacrystic garnet websterite pod from Bardane on the island of Fjørtoft, western Norway: Evidence for diamond formation in mantle rocks during deep continental subduction

Published:2002 Issue:11 Volume:30 Page:959
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geol

Author:

van Roermund Herman L.M.,Anthony Carswell D.,Drury Martyn R.,Heijboer Tjerk C.

Publisher

Geological Society of America

Subject

Geology

Reference21 articles.

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2. Sinking intrusion model for the emplacement of garnet-bearing peridotites into continent collision orogens

3. A general model for the intrusion and evolution of ‘mantle’ garnet peridotites in high-pressure and ultra-high-pressure metamorphic terranes

4. TheP,Tphase and reaction diagram for elemental carbon, 1979

5. Raman microspectrometry of fluid inclusions

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