| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8907129 | Earth and Planetary Science Letters | 2018 | 9 Pages |
Abstract
- Magmatic fluids under Daisen volcano affected large Tottori earthquakes.
- Upwelling flow occurs in the upper mantle above the old Pacific slab.
- The PHS slab is heated from below and side by the hot mantle upwelling.
- Daisen adakite magmas were affected by the PHS slab melting.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Dapeng Zhao, Xin Liu, Yuanyuan Hua,