matt de paoli | geologist
 
THERMOCALC
Pseudosections represent the mineral assemblages that will form over a P-T range for a given chemical bulk rock. From the pseudosections, omphacite granulite and entrained eclogite within the Breaksea Orthogneiss have very similar P-T histories despite there being large differences in chemical (bulk rock) composition. Peak metamorphic assemblages reside within high-P granulite to eclogite fields. More to come!!! Once the paper gets out.

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