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Petrology of deep sea basalt near Hawaii

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Moore, J. G.·1965·American Journal of Science

Abstract

Dredge samples collected from the submarine part of the east rift zone of Kilauea Volcano consist of glassy, tholeiitic pillow basalts containing vesicles whose volume and size decrease systematically with depth. Basalt dredged from seamounts near the Island of Hawaii is weathered, and the large volume of vesicles indicates that the seamounts have submerged as much as 1,700 m since their lava was extruded. Close chemical similarity between the glassy crust of submarine pillows and subaerial lava of the same rift zone indicates that exchange does not take place between sea water and deep sea basalt at the time of eruption. There is no evidence that spilite forms at the time of eruption.

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Metadata

Authors
Moore, J. G.
Venue
American Journal of Science
Published
1965-01-01
Volume
263
Issue
1
Pages
40-52
ISSN
0002-9599 (ISSN-L)
OpenAlex
W2328806222
Cited by
282
References
0
FWCI
8.18
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Petrology of deep sea basalt near Hawaii. https://app.cochat.ai/papers/10.2475/ajs.263.1.40
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Moore, J. G. (1965). Petrology of deep sea basalt near Hawaii. American Journal of Science. https://doi.org/10.2475/ajs.263.1.40

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.