Mass-balance modeling reveals Quaternary volcanism linked to a stagnant Neo-Tethyan oceanic slab in the mantle transition zone, highlighting deep slab dynamics.
Text S1 (analytical methods) and Text S2 (mass-balance modeling), Figures S1–S6, and Tables S1–S9.
No takes yet. Share an insight, caveat, or question.
Kang et al. (2024) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: