oa Evidence of Glacio-eustacy during the Late Berriasian to Late Valanginian: Record in the Lekhwair/Habshan/Salil Prograding Geometries, Rayda Basin, Sultanate of Oman

The Lekhwair/Habshan/Salil (or LHS) system is a carbonate succession that prograded by 300 km toward the northeast across the eastern part of the Arabian Plate (Rayda Basin) from Berriasian to Early Barremian. The system is organized as a series of large prograding clinoforms with amplitudes ranging from 200 to 350 m.