High-pressure reactive melt stagnation recorded in abyssal pyroxenites from the ultraslow-spreading Lena Trough, Arctic Ocean
Pyroxenites are an essential component in petrological and geochemical models for melt formation at mid-ocean ridges and ocean islands. Despite their rarity, their origin has been widely discussed and various processes have been invoked for their formation. Here, we present a detailed study of the m...
Published in: | Journal of Petrology |
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Main Authors: | , , , , , |
Format: | Text |
Language: | unknown |
Published: |
LSU Digital Commons
2014
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Subjects: | |
Online Access: | https://digitalcommons.lsu.edu/geo_pubs/976 https://doi.org/10.1093/petrology/egt073 https://digitalcommons.lsu.edu/context/geo_pubs/article/1975/viewcontent/976.pdf |