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Oasis is a meteorite crater in Libya. The crater is exposed at the surface, and has been significantly eroded. The prominent topographic ring is only the central uplift, which is about Template:Convert in diameter, while the original crater rim is estimated to have been Template:Convert in diameter. The age is estimated to be less than 120 million years (Lower Cretaceous).<ref>Template:Cite Earth Impact DB</ref>

The Oasis crater was photographed from space during the Apollo-Soyuz Test Project, and was recognized as a "possible astrobleme" at the time.<ref>Apollo-Soyuz Test Project Preliminary Science Report. NASA TM X- 58173. Feb. 1976.</ref> The crater had been recognized prior to this in 1969 by A. J. Martin.<ref>Martin, A. Possible Impact Structure in Southern Cyrenaica, Libya. Nature 223, 940–941 (1969). https://doi.org/10.1038/223940a0</ref> French et al. state that Oasis crater and the smaller BP Structure, about Template:Cvt to the north, were probably simultaneous impacts.<ref>BEVAN M. FRENCH, JAMES R. UNDERWOOD, EDWARD P. FISK; Shock-Metamorphic Features in Two Meteorite Impact Structures, Southeastern Libya. GSA Bulletin 1974;; 85 (9): 1425–1428. doi: https://doi.org/10.1130/0016-7606(1974)85<1425:SFITMI>2.0.CO;2</ref> Both impacts deform the Nubian Sandstone of early Cretaceous age.

About Template:Cvt to the southeast in Egypt is the much younger Kamil Crater.

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