Discussion Overview
The discussion revolves around the nature of seismic ultralow-velocity zones in the Earth's mantle and their potential relationship to mantle plumes. Participants explore whether these zones could be liquid or partially molten, while also addressing the solid-state characteristics of the mantle.
Discussion Character
- Debate/contested
- Technical explanation
- Conceptual clarification
Main Points Raised
- Some participants suggest that seismic ultralow-velocity zones may be liquid and could underlie rising mantle plumes.
- Others argue that the mantle is solid, capable of transmitting shear waves, but deforms visco-plastically.
- A participant mentions that the interpretation of the seismic data regarding the base of the Iceland plume is complex, suggesting it could be partially molten material or a solid with an iron-rich composition.
- There is a concern about misconceptions regarding the mantle's state, with participants emphasizing that it is not entirely liquid.
Areas of Agreement / Disagreement
Participants express disagreement regarding the state of the mantle, with some asserting it is solid while others propose the possibility of liquid or partially molten regions. The discussion remains unresolved with multiple competing views present.
Contextual Notes
Participants highlight the complexity of interpreting seismic data and the potential for different models to explain the observations, indicating that assumptions about the mantle's composition and behavior are critical to the discussion.