Origin of plagiogranites in oceanic complexes: A case study of the Nicoya and Santa Elena terranes, Costa Rica
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文摘

Plagiogranite zircons of Santa Elena and Nicoya yield SHRIMP 206Pb/238U ages of 125.3 ± 2.0 Ma and 90.9 ± 2.0 Ma to 88.5 ± 2.0 Ma, respectively.

Modeling suggests that Nicoya plagiogranites are ~ 10-15% residual liquids after fractional crystallization from its mafic parental source.

Plagiogranite chemistry is consistent with an oceanic arc and a MOR to oceanic plateau origin for Santa Elena and Nicoya, respectively.

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