Crustal Accretion in a Slow Spreading Back‐Arc Basin: Insights From the Mado Megamullion Oceanic Core Complex in the Shikoku Basin

Crustal Accretion in a Slow Spreading Back‐Arc Basin: Insights From the Mado Megamullion Oceanic Core Complex in the Shikoku Basin

Abstract Oceanic core complexes (OCCs) represent tectonic windows into the oceanic lower crust and mantle; they are key structures in understanding the tectono‐magmatic processes shaping the oceanic lithosphere. We present a petrological and geochemical study of gabbros collected at the Mado Megamul...

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Bibliographic Details
Main Authors: V. Basch, A. Sanfilippo, C. Sani, Y. Ohara, J. Snow, O. Ishizuka, Y. Harigane, K. Michibayashi, A. Sen, N. Akizawa, K. Okino, M. Fujii, H. Yamashita
Format: Article
Language:English
Published: Wiley 2020-11-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
oceanic core complex
back‐arc basin
Shikoku Basin
lower oceanic crust
mylonite
felsic veins
Online Access:https://doi.org/10.1029/2020GC009199

Internet

https://doi.org/10.1029/2020GC009199

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