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Moore 1965
Moore, J.G. (1965). Petrology of deep sea basalt near Hawaii. American Journal of Science 263(1): 40-52.
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.
Keywords
basalts; Cenozoic; changes of level; East Pacific Ocean Islands;, Hawaii; igneous rocks; Oceania; petrology; Polynesia; seamounts;, seamounts off Hawaii Island; submarine; submarine pillow lava cf., subaerial lava; United States; volcanic rocks; weathering, 05, Igneous and metamorphic petrology
Journal
American Journal of Science
http://plate.geology.yale.edu/level5/Ajs.html
Publisher
The American Journal of Science, Yale University
P.O. Box 208109
New Haven, CT 06520-8109
USA
203-432-3131
203-432-5668
ajs@yale.edu
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