| Abstract: | The deposits of mafic hydromagmatic eruptions are more fine grained and variable in vesicularity than dry magmatic deposits. Blocky, equant shapes of many hydromagmatic clasts also contrast with droplet, thread, and bubble wall morphology of dry magmatic fragments. Small (
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| Genre: | Article |
| ProdID: | 70033157 |
| Citation Author: | Mastin, L. G. |
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| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Geophysical Research B: Solid Earth |
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| Citation Search Results Text: | Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds; 2007; Article; Journal; Journal of Geophysical Research B: Solid Earth; Mastin, L. G. |
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| Citation Volume: | 112 |
| Citation Year: | 2007 |
| Type: | citation/reference |
| Text: | Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds; 2007; Article; Journal; Journal of Geophysical Research B: Solid Earth; Mastin, L. G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1029/2005JB003883 |
| Date Other: | Mon, 1 Jan 2007 00:00 -0600 |
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