Abstract
Mineral and melt inclusions in olivines from the most Mg-rich magma from the southern West Sulawesi Volcanic Province indicate that two distinct melts contributed to its petrogenesis. The contribution that dominates the whole-rock composition comes from a liquid with high CaO (up to 16 wt %) and low Al
Original language | English |
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Pages (from-to) | 2433-2462 |
Journal | Journal of Petrology |
Volume | 47 |
DOIs | |
Publication status | Published - 2006 |