| Abstract: | Compared with prior eruptions, lavas following the magnitude 7.5 (Richter scale) earthquake contained distinctly less Ti, K, P, Sr, Zr and Nb with a halved lava-production rate. These data suggest either that part of the system linking a shallow reservoir with the surface remains out of balance or that supply from a mantle source decreased as the volcano moved away from a fixed-source hot spot.-K.F. |
| Genre: | Article |
| ProdID: | 70015242 |
| Citation Author: | Tilling, R. I.; Rhodes, J. M.; Sparks, J. W.; Lockwood, J. P.; Lipman, P. W. |
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| Citation End Page: | 199 |
| Citation Issue: | 4785 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Disruption of the Mauna Loa magma system by the 1868 Hawaiian earthquake: geochemical evidence.; 1987; Article; Journal; Science; Tilling, R. I.; Rhodes, J. M.; Sparks, J. W.; Lockwood, J. P.; Lipman, P. W. |
| Citation Start Page: | 196 |
| Citation Volume: | 235 |
| Citation Year: | 1987 |
| Type: | citation/reference |
| Text: | Disruption of the Mauna Loa magma system by the 1868 Hawaiian earthquake: geochemical evidence.; 1987; Article; Journal; Science; Tilling, R. I.; Rhodes, J. M.; Sparks, J. W.; Lockwood, J. P.; Lipman, P. W. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1987 00:00 -0600 |
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