&. Frllcklewiez W., Bossowski
A. -
Wy-nikl wiercenia Gielczyce IG-l. Kwart. geol., 1970, nr 4.6. F r 11 c k i e Wf i c z W., B 0 s sow ski A. - Wy·· niki wiercenia 'l'wardawa IG-l. Ibidem, 1971, nr 3.
7. Ko 11n a us J., Gio go W'ski W. - Surowce
mineralne ceramiki budowlanej wojew6dztwa
opolskiego. Mat. i Stud. Opolskie, nr 30, 1974 .. SUMMARY
In the area stretching along the right bank of the Odra river, in the vicinities of Koonprachcice and Mechnice (Opole region), exposures of Upper Turonian marly clays not recorded so far were :liound. The deposits were previously described as marine Miocene sediments and used for production of red ceramics. On the basis of the micropaleon-tological studies the marly clays from Komprach-cice. /are interpreted as the youngest lithostratigra-phic link of the Pr6szk6w Beds; and in the local stratigraphic-deposits scheme they are interpreted as "series 7" of the Opole Cretaceous. Chemical . composition of the clays. indicates that they may be utilized in the cement industry as a raw mate-rial. with low
Cao
content. The older Turooian lithostratigraphic link - the so-called upper clay marls known from the areas of Folwark and Bier.-kowice - represent the same type of raw materialbut with a higher
Cao
content. The occurrence of sediments of such type in natural exposures offers a possibility to carry out geological-prospecting works aiming at the documentation of a new depo-sit of clay-marly raw materials.8. K
0 z low skiS. -
Podsiawowe probiemy bazysurowc6w mineralnych wojew6dztwa opolskiego.· Ibidem ..
9. Slusarczyk-Radwan D. - Surowce
mine-ralne przemysiu cementowego w wojew6dztwie opolskim. Ibidem.
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