Abstract
The event of catagenesisi in stratisfere is plays main role in alteration and formation of sedimentary rocks and sedimentary useful minerals. The first of all under subsidence sedimentary fasins and sedimentary rocks lost petrophysics puculdrity under oction of thermobar-ic factors. Rockformation minerals as quartz feldshpats an carbonate take plays is erosive and distructive and in same time in contrary direction is condacts transformation terrigenous and carbonate minerals to new minerals. Under catagenesis in the intensive catagenic processes determine role plays primery composition of sedimentary rocks and duration stay it’s in the zone of catagenesis. Authors of the article in order proves action to time of staying sedimentary rocks to catagenetic processes conducted in concrete factice materials specially investigation, which disclosed scole alterations of sedimentary rocks in stratisfere. For standing task has been used comparative analysis of catagenesis the example of permo-triassic rocks of Southn Manqishlak and fraqmental lastern precaucasus and Pliocene deposits of western boart of South Caspian...
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