Origin and implications of a thrust-bound gypsiferous unit along the western edge of Jabal Sumeini, northern Oman Mountains
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DOI: 10.1016/j.jseaes.2017.12.018
Abstract: Abstract The Oman Mountains comprise a series of thrust sheets of Neo-Tethyan oceanic rocks that were emplaced onto the Arabian continental margin during obduction of the Semail Ophiolite during the Late Cretaceous. Three separate groups… read more here.
Keywords: jabal sumeini; ediacaran early; oman mountains;