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The Miocene syn-rift mixed carbonate-siliciclastic sediments of_ Sidri-Feiran area provide a good example_ for the co-effect of the rift tectonics and eustatic sea level changes on carbonate siliciclastic _sedimentation_ These syn-rift Miocene sediments had been affected by four major tectonic events during Miocene time. These are the early-clysmic, post-Nukhul, mid-clysmic and post Karem tectonic events. Facies variations, tectonic events and ...
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