Petrogenesis of ultramafic-mafic clasts in the Dos Hermanos Mélange, Ilocos Norte: Insights to the evolution of western Luzon, Philippines

Journal of Asian Earth Sciences(2019)

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摘要
•Ophiolitic clasts (e.g. peridotites, gabbros) comprise the Dos Hermanos Mélange.•The ultramafic-mafic clasts are formed in an island arc and mid-ocean ridge.•The clasts resemble the crust-mantle section of the Zambales Ophiolite Complex.•Strike-slip faulting modified the emplaced lithosphere to form the mélange.
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关键词
Luzon,Mélange,Peridotite,Gabbro,Petrology
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