Not exact matches
Now a recent study, led by Arizona State University's School of Earth and Space Exploration Associate Professor Dan Shim, has re-created in the laboratory the
conditions found
deep in the Earth, and used this to discover an important property of the dominant mineral in Earth's
mantle, a region lying far below our feet.
In a lab at Ohio State, the researchers compress different minerals that are common to the
mantle and subject them to high pressures and temperatures using a diamond anvil cell — a device that squeezes a tiny sample of material between two diamonds and heats it with a laser — to simulate
conditions in the
deep Earth.
«Interactions between oxygen and iron dictate Earth's formation, differentiation — or the separation of the core and
mantle — and the evolution of our atmosphere, so naturally we were curious to probe how such reactions would change under the high - pressure
conditions of the
deep Earth,» said Mao.
«Because the diamond windows are transparent, we can look into the high - pressure device and watch reactions occurring at
conditions of the
deep mantle,» he said.