Behaviour of platinum-group elements in the subcontinental mantle of eastern Australia during variable metasomatism and melt depletion
Increasing recognition of complexities in the Platinum-group element (PGE) and Re concentration patterns in mantle samples are challenging the view of chondritic relative abundances in the upper mantle. To investigate the possible causes of PGE abundance
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|Source:||Geochimica et Cosmochimica Acta|
|01_Handler_Behaviour_of_platinum-group_1999.pdf||1.09 MB||Adobe PDF||Request a copy|
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