tailieunhanh - Origin of the pleonaste-bearing mafic–ultramafic rocks from the Armutlu peninsula, NW Turkey

Al-rich spinels were rarely reported compared to Cr-spinels, which were mostly observed in ophiolitic rocks. Pleonaste [(Mg, Fe2+)Al2 O4 ], which is an Al-rich spinel, was observed in the ophiolitic mafic–ultramafic rocks tectonically located in the Early Cretaceous accretionary complex, at the eastern part of the Armutlu peninsula, NW Turkey. | Origin of the pleonaste-bearing mafic–ultramafic rocks from the Armutlu peninsula, NW Turkey

TỪ KHÓA LIÊN QUAN