Collaborative Research: Hydrous melting of a lithologically-heterogeneous mantle: A combined experimental and computational approach
Description preview
The Earth’s mantle melts as it rises beneath mid-ocean ridges and hotspot volcanoes. This process generates ocean crust and is responsible for most of the volcanic eruptions on Earth. The presence of even small amounts of water in the mantle is known to have large effects on the amount of magma produced. Likewise, small changes in chemical…
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