Crustal origin for coupled ultra-depleted and plagioclase signatures in MORB olivine-josted melt inclusions: evidence from the Siqueiros Transform Fault, East Pacific Rise
Geochemical data from melt inclusions in olivine phenocrysts in a picritic basalt from the Siqueiros Transform Fault on the northern East Pacific Rise provide insights into the petrogenesis of mid-ocean ridge basalts (MORB). The fresh lava contains ∼ 10
|Collections||ANU Research Publications|
|Source:||Contributions to Mineralogy and Petrology|
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