Subduction zone polarity in the Oman Mountains: Implications for ophiolite emplacement

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...

Полное описание

Библиографические подробности
Главные авторы:	Searle, M, Warren, C, Waters, D, Parrish, R
Формат:	Conference item
Опубликовано:	2003

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