Differentiation of Hawaiian basalts; Trends of Mauna Loa and Kilauea historic magma
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ID: 297976
1961
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Abstract
New analyses strengthen the conclusion that the historic lavas of Mauna Loa and Kilauea are derived from different magmatic batches. The presence or absence of hypersthene in the lavas seems to be related to the silica and lime contents.
| Reference Key |
openalex_W2330184473
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|---|---|
| Authors | C. E. Tilley, J. H. Scoon |
| Journal | american journal of science |
| Year | 1961 |
| DOI |
10.2475/ajs.259.1.60
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| URL | |
| Keywords | Keywords not found |
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