Not exact matches
The 5 - millimeter - long diamond — and its water -
carrying ringwoodite (not visible)-- formed
deep within Earth's
mantle.
Led by Carnegie's Ho - kwang «Dave» Mao, the research team believes that as much as 300 million tons of water could be
carried down into Earth's interior every year and generate
deep, massive reservoirs of iron dioxide, which could be the source of the ultralow velocity zones that slow down seismic waves at the core -
mantle boundary.
Hydration reactions along the subducting plate are thought to
carry water
deep into the Earth, and dehydration reactions at greater depths release fluids into the overlying
mantle that promote melting and volcanism.
Led by Geophysical Laboratory's Ho - kwang «Dave» Mao, the research team believes that as much as 300 million tons of water could be
carried down into Earth's interior every year and generate
deep, massive reservoirs of iron dioxide, which could be the source of the ultralow velocity zones that slow down seismic waves at the core -
mantle boundary.