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During the late Sakmarian (Early Permian), the Haushi limestone was deposited in a shallow embayment of the Neotethys Ocean covering what is now north Oman and parts of southeast Saudi Arabia. The sea persisted through the late Sakmarian, but by the time of the deposition of the ?Artinskian Middle Gharif Member, limestone deposition had ceased and generally arid fluvial and minor lacustrine palaeonvironments...
We investigated the structural and electrical behavior of Fe implanted and annealed MOVPE grown GalnP layers lattice matched to GaAs substrates, demonstrating that high temperature Fe implantation can give rise to stable semi-insulating layers
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