The hidden role of Mg–Si–COH fluids on mantle wedge metasomatism
Key Points
Metasomatism is significantly influenced by magnesium, silicon, and carbon fluids in the mantle wedge, enhancing geochemical processes.
Key evidence shows that these fluids can alter the composition of mantle materials, influencing magma formation.
Observational analysis of mantle samples reveals chemical interactions between fluids and mantle rocks, leading to significant changes in mineral composition.
This work highlights the need for further studies on mantle metasomatism to understand its broader geological implications.