| Abstract: | Interpretation of abundant seismic data suggest that Kilauea‘s primary conduit within the upper mantle is concentrically zoned to about 34-km depth. This zoned structure is inferred to contain a central core region of relatively higher permeability, surrounded by numerous dikes that are in intermittent hydraulic communication with each other and with the central core. During periods of relatively high magma transport, the entire cross section of the conduit is utilized. During periods of relatively low to moderate transport, however, only the central core is active.-from Author |
| Genre: | Article |
| ProdID: | 70014817 |
| Citation Author: | Ryan, M. P. |
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| Citation End Page: | 4248 |
| Citation Issue: | B5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Geophysical Research |
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| Citation Number Of Pages: | 36 |
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| Citation Search Results Text: | The mechanics and three-dimensional internal structure of active magmatic systems: Kilauea volcano, Hawaii.; 1988; Article; Journal; Journal of Geophysical Research; Ryan, M. P. |
| Citation Start Page: | 4213 |
| Citation Volume: | 93 |
| Citation Year: | 1988 |
| Type: | citation/reference |
| Text: | The mechanics and three-dimensional internal structure of active magmatic systems: Kilauea volcano, Hawaii.; 1988; Article; Journal; Journal of Geophysical Research; Ryan, M. P. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Fri, 1 Jan 1988 00:00 -0600 |
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