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The clay mineral assemblage within the marine rocks of the synclinal basins of the Syrian arc deformation belt in the northwest of Israel is dominated by smectitic IS (interstratified illite/smectite rich in smectite layers) accompanied by palygorskite and occasional sepiolite. Based on the observation that the smectitic IS originated by conversion of the smectite transported to the synclinal basins...
The marine sedimentation along the margin of the southeastern Neo-Tethys during the oceanic convergence stage between the Senonian and the Eocene took place on sea-bottom topography formed by the folding of the Syrian arc deformation belt. The clay mineral assemblage within the marine rocks of the synclinal basins of the Syrian arc deformation belt in the southeast of Israel is dominated by smectitic...
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