%T On the occurrence of primary dolomites in Qatrani Formation (Oligocene) in Fayoum Province, Western Desert, Egypt
%I University of Szeged, Department of Mineralogy, Geochemistry and Petrology
%C Szeged
%V 22
%N 1
%L acta24592
%P 119-131
%X This work represents a study of pÊtrographie properties, differential thermal analysis and Нг-ray diffraction study of carbonate rocks of the Qatrani formation of Oligocene age in Fayoum Province, Egypt. These carbonate rocks can be grouped into three major textural and compositional types. Microcrystalline dolostones or dolomicrite, gypsiferous dolomicrite and dolomitic sandstones.
%A  Abdel Rehim A. M.
%A  Abdel-Kireem M. R.
%O Bibliogr.: 131. p. ; ill. ; ĂśsszefoglalĂĄs angol nyelven
%K Kőzettan, Ásványtan, Földtan
%D 1975
%J Acta mineralogica-petrographica