Subduction zone polarity in the Oman Mountains: Implications for ophiolite emplacement
Two end-member models have been proposed to account for the structure and metamorphism of rocks beneath the Semail ophiolite in the Oman mountains. Model A involves a single, continuous NE-directed subduction away from the continental margin during the late Cretaceous. The ophiolite and underlying t...
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| Định dạng: | Conference item |
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2003
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