Chemical variation in magma caused by gas transport

Tuffisite veins are glass-filled fractures formed when magma fragments during degassing within the conduit. These veins form transient channels through which exsolved gases can escape from magma. The purpose of this study is to determine the extent to which chemical heterogeneity within the melt res...

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Bibliographic Details
Published in:Geochimica et Cosmochimica Acta
Main Authors: Berlo, Kim, Tuffen, Hugh, Smith, Vicki, Castro, Jonathan, Pyle, David, Geraki, Tina, Mather, Tamsin
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
Subjects:
Online Access:https://eprints.lancs.ac.uk/id/eprint/66065/
https://doi.org/10.1016/j.gca.2013.07.032