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 |
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Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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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. |
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ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.165.3898.1112 |