The Structure of the Upper Mantle Transition Zone Beneath Northeast China Associated With Mantle Plume Migration
Abstract The stagnation and dehydration of the Pacific Plate slab in the mantle transition zone (MTZ) are widely accepted to have resulted in Mesozoic and Cenozoic volcanic activities and the formation of the Songliao Basin in NE China. However, this notion has been challenged by recent seismic stud...
Sábháilte in:
| Príomhchruthaitheoir: | |
|---|---|
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe / Cruthaithe: |
American Geophysical Union (AGU)
2021-09-01
|
| Sraith: | Earth and Space Science |
| Ábhair: | |
| Rochtain ar líne: | https://doi.org/10.1029/2021EA001874 |
| Clibeanna: |
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
|