Plastic Deformation of Plagioclase in Oceanic Gabbro Accreted at a Slow‐Spreading Ridge (Hole U1473A, Atlantis Bank, Southwest Indian Ridge)

Crustal architecture at slow‐spreading oceanic ridges results from complex interactions between magmatism, hydrothermalism, and tectonics. IODP Hole U1473A was drilled during Expeditions 360 and 362T at the summit of the Atlantis Bank, a gabbroic massif exhumed at the Southwest Indian Ridge. In this...

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Veröffentlicht in:Journal of geophysical research. Solid earth 2021-10, Vol.126 (10), p.n/a
Hauptverfasser: Allard, Maël, Ildefonse, Benoît, Oliot, Émilien, Barou, Fabrice
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Sprache:eng
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