Abstract
Above, in defining this type of deep-seated tectonic region, we noted that its significant differences are a somewhat greater depth of earthquake foci, as compared with extrageosynclinal regions, and a well-defined linearity of the zones.
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© 1971 Consultants Bureau, New York
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Sheinmann, Y.M. (1971). Magmatic Features of Midocean Ridges. In: Tectonics and the Formation of Magmas. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-1584-1_9
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DOI: https://doi.org/10.1007/978-1-4684-1584-1_9
Publisher Name: Springer, Boston, MA
Print ISBN: 978-1-4684-1586-5
Online ISBN: 978-1-4684-1584-1
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