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

R. N. Anderson; J. Honnorez; K. Becker; A. C. Adamson; J. C. Alt; R. Emmermann; P. D. Kempton; H. Kinoshita; C. Laverne; M. J. Mottl; R. L. Newmark

doi:10.1038/300589a0

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

R. N. Anderson, J. Honnorez, K. Becker, A. C. Adamson, J. C. Alt, R. Emmermann, P. D. Kempton, H. Kinoshita, C. Laverne, M. J. Mottl, R. L. Newmark

Research output: Contribution to journal › Article › peer-review

103 Scopus citations

Abstract

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 CRI Rift, Hole 504B confirms that the main features of the upper part of an idealized ophiolite sequence occurs in the oceanic crust.

Original language	English (US)
Pages (from-to)	589-594
Number of pages	6
Journal	Nature
Volume	300
Issue number	5893
DOIs	https://doi.org/10.1038/300589a0
State	Published - 1982
Externally published	Yes

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

In: Nature, Vol. 300, No. 5893, 1982, p. 589-594.

Research output: Contribution to journal › Article › peer-review

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AU - Anderson, R. N.

AU - Honnorez, J.

AU - Becker, K.

AU - Adamson, A. C.

AU - Alt, J. C.

AU - Emmermann, R.

AU - Kempton, P. D.

AU - Kinoshita, H.

AU - Laverne, C.

AU - Mottl, M. J.

AU - Newmark, R. L.

PY - 1982

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AB - 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 CRI Rift, Hole 504B confirms that the main features of the upper part of an idealized ophiolite sequence occurs in the oceanic crust.

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