In the structural - tectonical plan formation of Low Kura lowland. It is possible to separate 3 stages. The first is Mezozoy and tectonical - structural plan created by formed soil complex in this stage. In this stage Kuryani lowland passed ocean stage of it is development and from this point is characterized relatively with slightly occurring of sediment accumulation process. But probably, the occurring of accretion in subduction zone available first in Tetis then in the north of Paratetis showed it is affection certainly for the formation of ocean sediment thickness. In the result of accretion the accumulated organic matter in the ocean sediment of this process is possible to say the reason for the accumulation in small site. From structural- tectonical aspect in the first stage the deep folds not and depth breakings were formed sharing and bordering to the blocks of the Kura lowland.


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