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Published in 2020 at "Contributions to Mineralogy and Petrology"
DOI: 10.1007/s00410-020-01689-x
Abstract: Observations in the S-type granites (s.l.) of the Wilson’s Promontory batholith demonstrate that one type of schlieren in granitic rocks represent accumulations of mainly mafic magmatic minerals, with internal layering formed through pulsed magma flow.…
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Keywords:
mafic schlieren;
case;
dissolution reprecipitation;
granitic magmas ... See more keywords