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) |
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Pages (from-to) | 589-594 |
Number of pages | 6 |
Journal | Nature |
Volume | 300 |
Issue number | 5893 |
DOIs | |
State | Published - 1982 |
Externally published | Yes |
ASJC Scopus subject areas
- General