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The geology of northeastern Oman is dominated by the Batain nappes, which comprise an allochthonous sequence of Permian to uppermost Cretaceous marine sedimentary and volcanic rocks (Map below). At the Cretaceous-Paleogene transition (~65 Ma), oblique convergence between India and Afro-Arabia caused fragments of the early Indian Ocean to be thrust onto the Batain Basin, eastern Oman. The Lower Permian to Maastrichtian sediments and volcanic rocks of the Batain basin and fragments of the Indian Ocean floor (eastern ophiolite of Oman “Masirah ophiolite”) were obducted northwestward onto the northeastern margin of Oman.

Evolved carbonatitic kimberlites from the Batain Nappes, eastern Oman continental margin