Mantle geochemistry: the message from oceanic volcanism
Abstract
Basaltic volcanism 'samples' the Earth's mantle to great depths, because solid-state convection transports deep material into the (shallow) melting region. The isotopic and trace-element chemistry of these basalts shows that the mantle contains several isotopically and chemically distinct components, which reflect its global evolution. This evolution is characterized by upper-mantle depletion of many trace elements, possible replenishment from...
Paper Details
Title
Mantle geochemistry: the message from oceanic volcanism
Published Date
Jan 1, 1997
Journal
Volume
385
Issue
6613
Pages
219 - 229
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