Abstract
Deep ocean floors are mostly covered by unconsolidated sediments, commonly a few to several hundred metres thick, which are underlain usually by basaltic rocks.
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© 1965 Akiho Miyashiro
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Miyashiro, A. (1965). Ocean-floor Metamorphism and its Significance. In: Metamorphism and Metamorphic Belts. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-6836-6_22
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DOI: https://doi.org/10.1007/978-94-011-6836-6_22
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-04-550026-0
Online ISBN: 978-94-011-6836-6
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