TRANSFORMATIONS OF HIGH-CHARGED SWELLING MINERALS DURING EARLY DIAGENESIS IN RECENT SEDIMENTS OF GDANSK BAY (BALTIC SEA)
The Vistula River and seafloor sediments were characterized by pH values 6.7-8.42. In studied cores below the seafloor pH decreased down to 2.5. Dioctahedral smectite (montmorillonite), mica, and kaolinite were main constituents of the clay fractions from Vistula loads. Traces of chlorite and hydroxyinterlayerd minerals (HIM) were also identified in the loads. The seafloor sediments also contained smectite, mica, and kaolinite. Clay fractions from the cores were significantly depleted in smectite and enriched in chlorite relative to the clays from the seafloor and the Vistula loads. Layer charges of swelling clays in all studied samples were from 0.46 to 0.56 per formula unit which indicated that the clay fractions were dominated by high-charged smectites. Clay fractions from the Vistula prodelta were enriched in K2O, MgO, and Fe2O3 relative to the clays separated from the loads.
Selective absorption of magnesium and/or iron and the hydroxylation are likely reactions leading to formation of chlorite at the expanse of smectite during early diagenesis in the Gdańsk Bay sediments. The process has to be taken into consideration in sedimentary basin studies.
Acknowledgments:
This study was financed by National Science Centre, Poland [grant number: UMO-2016/23/N/ST10/01388].
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