“…Seeping brines fill local seafloor depressions (green diamonds in frame a). The thickness of Miocene evaporites varies significantly due to salt mobilization (circles: Ahmed, 1972;Almalki et al, 2015;Azab et al, 2020;A. L. Evans, 1988;Hughes and Johnson, 2005;Miller and Barakat, 1988;Purser and Bosence, 1998;Whitmarsh et al, 1974).…”