DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crust

DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crust

Hole 504B provides a reference section for correlation of in situ petrological and geophysical studies with regional crustal models based on dredged samples and remote surveys; and, at least for the medium-spreading-rate Costa Rica Rift, Hole 504B confirms that the main features of the upper part of...

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Veröffentlicht in:Nature (London) 1982-12, Vol.300 (5893), p.589-594
Hauptverfasser: Anderson, R. N., Honnorez, J., Becker, K., Adamson, A. C., Alt, J. C., Emmermann, R., Kempton, P. D., Kinoshita, H., Laverne, C., Mottl, M. J., Newmark, R. L.
Format: Artikel
Sprache:eng
Schlagworte:
Humanities and Social Sciences
Marine
multidisciplinary
Science
Science (multidisciplinary)
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Beschreibung
Zusammenfassung:Hole 504B provides a reference section for correlation of in situ petrological and geophysical studies with regional crustal models based on dredged samples and remote surveys; and, at least for the medium-spreading-rate Costa Rica Rift, Hole 504B confirms that the main features of the upper part of an idealized ophiolite sequence occurs in the oceanic crust.
ISSN:0028-0836
1476-4687
DOI:10.1038/300589a0