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Relict fluvial and lacustrine deposits in the interior of Oman near Saiwan consist of waterlain breccias with pebble imbrications and current ripples, covered by algal laminites containing calcified reeds and charcoal pieces. Geomorphological evidence suggests that the palaeolake covered a maximum surface of 1400 km 2 and had a maximum depth of about 25 m. Optically stimulated luminescence (OSL) and thermally transferred OSL d...
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