Name
Elzaev Aslambek Sipaevich
Scholastic degree
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Academic rank
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Honorary rank
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Organization, job position
Grozny State Petrol Technical University in the name of academician M. D. Millionshchikov
Web site url
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Articles count: 1
Within the Terek-Sunzha oil and gas region of the
Eastern Caucasus a productive sediments are clearly
expressed by the classical diapir due to the increase in
power in the arched part of the strata of the Maikop
clays. In accordance with the theory of I. M. Gubkin,
developed based on the analysis of the structure of the
oil and gas structures of mud volcanoes of Azerbaijan,
diapirism of the structure is an important prerequisite for
the formation of a mud volcano. The article provides a
comparative analysis of diapir structures of the TerekSunzha
oil and gas region of the Eastern Caucasus,
which is quasi-mud unripe volcanoes, and structures of
mud volcanoes in the South-Eastern end of the Caucasus
range (the Apsheron Peninsula and other territories of
Azerbaijan) and the North-Western end of the Caucasus
range (the Kerch and Taman Peninsula). It is shown that
the formation of diapir structure, when, in the context of
high power clay strata, is not a sufficient condition for its
transformation into a mud volcano. In such geological
conditions, it is essential to determine the capacity of
clay strata, but also the degree of its water-filled
porosity, visco-plastic and fluid-forming properties,
contributing to the transition of the breed in a phase of
active current and the coming to the surface