Sedimentary rocks

Sedimentary rocks – are still called the sloping rocks. After the manner of occurrence, four groups are allocated: vulcanillic, clastic, chemical and organogeneous sedimentary rocks. Sedimentary rocks arise on the Earth’s surface and the process of their occurrence covers several stages: surface decomposition, transport, sedimentation and diagenerate. In the group of vulcanillic sedimentary rocks are: the lipbratch, volcanic brececes, volcanic agglomerates, tufovitic sedimentary rocks include: the brethren, conglomerates, sandstones, classes, the leset, pelitolites and gules. The group of chemically sedimentary rocks include: the lines, the dolomites, lapsees, the cliner, marble onyx, travertine, writing for writing, as well as the silician sediments. In the organogenic sedimentary rocks include: the diatomainic country, the silicles and loses. Lit.: Blazo Buev, Risto Stojanov, Petrography, RGF, Shtip, 1994. BL. B.


Original article in Macedonian language Cyrillic alphabet
Кириличен напис СЕДИМЕНТНИ КАРПИ

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