| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4712897 | Journal of Volcanology and Geothermal Research | 2010 | 19 Pages |
Abstract
âºWe investigated syneruptive time and condition that changed eruption intensity. âºWe deduced magma decompression conditions from groundmass microlites of scoriae. âºDecompression rates in each eruptive unit have a positive correlation with intensity. âºDifferent rates had been generated before the start of microlite crystallization. âºMagmas erupted earliest and just after repose had been arrested in conduit.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Yuki Suzuki, Toshitsugu Fujii,