Evidence for Low‐Pressure Crustal Anatexis During the Northeast Atlantic Break‐Up

Evidence for Low‐Pressure Crustal Anatexis During the Northeast Atlantic Break‐Up

Abstract While basaltic volcanism is dominant during rifting and continental breakup, felsic magmatism may be a significant component of some rift margins. During International Ocean Discovery Program (IODP) Expedition 396 on the continental margin of Norway, a graphite‐garnet‐cordierite bearing dac...

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Main Authors: A. M. Morris, S. Lambart, M. A. Stearns, J. R. Bowman, M. T. Jones, G. Mohn, G. Andrews, J. Millett, C. Tegner, S. Chatterjee, J. Frieling, P. Guo, D. W. Jolley, E. H. Cunningham, C. Berndt, S. Planke, C. A. Alvarez Zarikian, P. Betlem, H. Brinkhuis, M. Christopoulou, E. Ferré, I. Y. Filina, D. T. Harper, J. Longman, R. P. Scherer, N. Varela, W. Xu, S. L. Yager, A. Agarwal, V. J. Clementi
Format: Article
Language:English
Published: Wiley 2024-07-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
crustal anatexis
Mimir High
IODP Site U1570
continental break‐up
NAIP
Online Access:https://doi.org/10.1029/2023GC011413
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https://doi.org/10.1029/2023GC011413

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