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This study utilizes high-resolution LA-ICP-MS trace-element mapping to investigate biotite from 22 felsic intrusions in New Brunswick, focusing on its magmatic zoning patterns. The findings reveal that while major elements in biotite are homogeneous, two-thirds of the grains exhibit trace-element zoning, particularly in larger grains, which may indicate rapid cooling post-crystallization. The research highlights the potential of biotite zoning to provide insights into syn- to post-magmatic processes and the

Author
july.quiceno
Language
EN

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