scholarly journals Structural features of the lower permian salt-bearing series and the character of salt-tectogenesis manifestations in the northern and northwestern margins of the Сaspian depression. Paper 1

Author(s):  
Yuri A. Pisarenko ◽  
◽  
Olga P. Goncharenko ◽  
Vladimir Yu. Pisarenko ◽  
◽  
...  

The detailed evaluation of the accumulated geological-geophysical data, particularly on the inner structure of the saltbearing series in the margins of the Caspian Depression, the mechanism of salt-tectogenesis manifestation, its reflection in the structure of the salt table and association with the structural inhomogeneities of the subsalt bed is presented. The authors attempt to acquire additional indirect criteria for predicting the structure of the subsalt bed by means of analyzing the structure of the salt-bearing series and the character of salt-tectogenesis manifestation. The problem solution is based on the complex analysis of the data from drilling and seismic prospecting.

Author(s):  
Yuri A. Pisarenko ◽  
◽  
Olga P. Goncharenko ◽  
Vladimir Yu. Pisarenko ◽  
◽  
...  

The article presents the analysis of the inner structure of the salt-bearing series within the Caspian Depression. Certain salt-bearing complexes of various ages, compositions and plastic properties are distinguished. Their structural relations and the features of salt-tectogenesis manifestation are evaluated. Up to the present no subsalt uplifts have been confirmed in the Russian sector of the Caspian Depression and no HC fields have been discovered. Therefore, any search for additional criteria for predicting the salt-bed structure from the character of salttectogenesis manifestation is conductive to predicting the zones of subsalt structure development over the Caspian Depression area.


1971 ◽  
Vol 13 (3) ◽  
pp. 419-421 ◽  
Author(s):  
M V. Gorfunkel' ◽  
G.L. Slepakova

1986 ◽  
Vol 123 (6) ◽  
pp. 673-681 ◽  
Author(s):  
J. G. M. Raven ◽  
Ben A. Van Der Pluijm

AbstractConodont colour alteration index (CAI) values from Upper Paleozoic rocks in the Cantabrian zone of northern Spain show that temperatures during Hercynian metamorphism locally exceeded 300 °C. Various temperature domains have been defined, which are generally separated by fundamental structures. These domains do not correspond with the tripartite subdivision based on stratigraphic analysis.The observed CAI values of conodonts are in general agreement with the mineral paragenesis. Areas with high CAI values display extensive alteration and mineralization, and where CAI values exceed 4–4.5 (>200 °C) slaty cleavage has developed.The Cantabrian zone is an area of very low grade metamorphism, where peak conditions were reached in Upper Carboniferous to Lower Permian times. The characteristics of the metamorphism and its spatial relationship with major faults suggest that fluids were the main source for regional heating and that fluid transport was focussed along crustal-scale structural features.The overall deformation regime in this part of the Variscan orogen of western Europe is interpreted to be large-scale transtension. This is in agreement with earlier proposed models for the formation of Upper Palaeozoic basins in this area.


2019 ◽  
Vol 16 (11) ◽  
pp. 4491-4501
Author(s):  
O. S. Obryadchikov ◽  
K. M. Taskinbaev

The features of the deep structure of the eastern part of the Caspian depression, the patterns of placement of large carbonate complexes, which are associated with the main accumulations of oil and gas, are considered. The discovery of industrial accumulation of oil in the Lower Permian terrigenous sediments on the Akzhar Eastern area showed the possibility of carbonaceous carbonate deposits of carbon to be the object of prospecting and exploration. Oil deposits in the supersalt complex of sediments on the structures of Karatube South and Saigak are assumed to be formed due to the vertical flow from subsalt clay-carbonate sediments, which also allows us to count on the expansion of prospecting works and to focus on the east of the Caspian depression a new direction geological exploration (DGE).


Author(s):  
Maryna Rudina ◽  
Anna Kopera

The paper explores the distinctive features of the study related to the specific representation of the emotion concepts. Several well-known approaches to the analysis of concepts based on the implementation of different research material are highlighted. The paper proposes a comprehensive methodology for the study and analysis of the linguacultural emotion concept of HAPPINESS, its artistic dynamics, based on the principles of integration of various scientific methods. The study enabled us to carry out a multifold description of the analyzed linguistic expression of the concept and to identify the specific features of the concepts in the English artistic discourse as well as in the Ukrainian translations. The complex and systematic approach to the study of an emotional concept is justified to serve as a characteristic feature of this methodology that attempts to identify textual functioning, structural features, emotive and valuable features of the concept. The study demonstrates that the effective use of provided methodology for the study of an artistic concept requires a special algorithm for the application of scientific methods in order to isolate and characterize the verbal expression of the content of the emotion concept. We consider the implementation of general scientific and empirical methods based on the principles of verbalization, objectification and interpretation of the linguacultural emotional concept for a systemic study of the conceptualization features of the concept. The methodology is represented by the example of a complex analysis of the specific features of the key components of the concept HAPPINESS, a verbal embodiment in a Fr. Sc. Fitzgerald’s piece of art ‒ “The Great Gatsby”. The proposed methodology contributed to the identification of 6 dominant conceptual structures in percentage terms and distinctive features of their artistic translation.


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