Encapsulating Earth's deep water filter
Small
inclusions in diamonds brought up from the mantle provide valuable
clues to the mineralogy and chemistry of parts of Earth that we cannot
otherwise sample. Tschauner et al. found inclusions of the
high-pressure form of water called ice-VII in diamonds sourced from
between 410 and 660 km depth, the part of the mantle known as the
transition zone. The transition zone is a region where the stable
minerals have high water storage capacity. The inclusions suggest that
local aqueous pockets form at the transition zone boundary owing to the
release of chemically bound water as rock cycles in and out of this
region.
Source: sciencemag
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