Description of silicified geodes within Slunfeh formation and determination of their minerals and crystal habits


Abstract in English

Cauliflower silicified geodes within Slunfeh Formation of upper cretaceous were described. Mid-range infrared spectroscopy FTIR was used for determination of mineral composition of these geodes. Polarized light microscope was used for the study of thin sections taken from inner parts of geodes in order to determine their crystal habits. The results showed that geodes of studied formation consists of silicon in form of amorphous to cryptocrystalline opal, chalcedony of micro-crystalline fibrous radial structure, hexagonal prismatic quartz, radial quartz, zoned quartz and mosaic quartz.

References used

Makhlouf, M., Recognition of quartz geodes in the Upper Cretaceous Wadi Umm Ghudran Formation, Ras En Naqab, South Jordan. Arab J Geosci, 2015, 1535-1547
Chowns, T.M., Elkins, J.E., The origin of quartz geodes and cauliflower cherts through the silicification of anhydrite nodules. Sediment Petrol, 1974, 885-903
Maliva, R.G., Quartz geodes: early diageneticchertifiedanhydritenodules related to dolomitization. J Sed Petrol, 1987, 1054-1059

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