The hydrogen-absorbing ability of a mantle mineral in its structure determines the capacity of the water reservoirs hosted by the mineral. Water reservoirs at the base of Earth’s mantle directly influence the fate of...
详细信息
The hydrogen-absorbing ability of a mantle mineral in its structure determines the capacity of the water reservoirs hosted by the mineral. Water reservoirs at the base of Earth’s mantle directly influence the fate of water brought down by slab subduction and the seismic heterogeneity such as ultralow-velocity zones(ULVZs)at the core-mantle boundary. Pyrite-Fe O2 Hx(0≤x ≤1) presents a possibility of such reservoirs in the deep mantle [1–3].
暂无评论