The two major progradational cycles can be identified in nearby subsurface well penetrations such as Masirah-1 (SMP-1).The tidal sandstones of the Masirah Bay Formation were deposited as regressive-transgressive pulses in a longer term transgressive stratigraphic trend associated with both the demise of continental glaciation and the end of active extensional tectonics. If you’re not in the mood for online dating at the moment, don't put up with it.Find thousands of fun-loving and flirty singles to flirt with.The Huqf Supergroup of Oman contains an excellently exposed succession from the presumed Marinoan-age Fiq glaciation (ca.635 Ma) to the Precambrian–Cambrian boundary (542 Ma).
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