| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8907004 | Earth and Planetary Science Letters | 2018 | 10 Pages |
Abstract
- Havre magma entered the ocean before fragmenting.
- Clasts were produced by quenching buoyant magma in the ocean.
- Buoyant >1 m diameter pumice blocks floated to the ocean surface.
- Clasts with enough isolated porosity and trapped gas floated in a raft while the rest sank.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Michael Manga, Kristen E. Fauria, Christina Lin, Samuel J. Mitchell, Meghan Jones, Chris E. Conway, Wim Degruyter, Behnaz Hosseini, Rebecca Carey, Ryan Cahalan, Bruce F. Houghton, James D.L. White, Martin Jutzeler, S. Adam Soule, Kenichiro Tani,