Diorites from the Mid-Atlantic Ridge at 45° N

Diorites, associated with basalts, basalt breccias, and serpentinized peridotites, occur in situ on the faulted scarps of two seamounts from the western High Fractured Plateau of the Mid-Atlantic Ridge at 45° N.

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1969-09, Vol.165 (3898), p.1112-1113
1. Verfasser: Aumento, F.
Format: Artikel
Sprache:eng
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Zusammenfassung:Diorites, associated with basalts, basalt breccias, and serpentinized peridotites, occur in situ on the faulted scarps of two seamounts from the western High Fractured Plateau of the Mid-Atlantic Ridge at 45° N.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.165.3898.1112