Relaxation Processes in a Quantum Wire with Parabolic Confinement

Hasanov, Kh. A.; Huseynov, J. I.; Mamedov, Fikret; Abbasov, I. I.; Hasanov, A. A.

doi:10.15407/ujpe63.10.930

Cited by 1 publication

(7 citation statements)

References 9 publications

(11 reference statements)

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“…Cretaceous deposits are widespread in the region (Khuduzade et al, 2015;Geology of Azerbaijan, 2005) and are represented by volcanic (Turonian-Lower Coniacian) in the lower part, volcanic-sedimentary (Upper Coniacian-Lower Santonian) in the middle part, and carbonate lithofacies in the upper parts (Upper Santonian-Maastrichtian). Volcanogenic rocks are mainly composed of porphyries, basalts, andesites and their derivatives and are classified as vuggy-porous reservoirs due to their capacity and permeability (Hasanov, et al, 2017). Table 1 shows data covering the lower, upper and middle limits of the physical properties of rocks of different ages taken from different depths (the number of samples studied is indicated in brackets).…”

Section: Resultsmentioning

confidence: 99%

“…Paleogene limestones are practically non-magnetic, their density is 2.56 g/ cm 3 , porosity is 5.1%, and the propagation velocity of longitudinal elastic waves reaches 3000 m/s. Based on the results of laboratory studies of rock samples, the following assessments of the physical properties of Eocene rocks were made (Hasanov, et al, 2017). The density siltstones is 2.45 g/cm 3 , porosity is 5.0%, ultrasonic wave velocity is 1300 m/s, the density of limestone is 2.65 g/cm 3 , porosity is 5.24%, ultrasonic wave velocity is 2950 m/s, the magnetosensitivity is missing.…”

Section: Resultsmentioning

confidence: 99%

“…However, it should be noted that the geological structure and oil and gas bearing of the Mesozoic complex have not yet been sufficiently clarified by exploration drilling, so hydrocarbon resources have not yet been fully exploited. In particular, according to the authors (Aliyarov, et al, 2018;Hasanov, et al, 2017;Gurbanov, et al, 2020;Guliyev, et al, 2014), Cretaceous and Jurassic terrigenous-carbonate reservoirs in the complex are characterized by more favorable conditions for the search for new oil and gas fields in the northwestern part of the country. Thus, according to (Hasanov, et al, 2017;Hasanov, Ganbarova, 2019), the maximum thickness of deposits (1117 m) in the territory of the Kura-Gabirri oil and gas region was identified in the areas of Mammadtapa(1037 m) and Tarsdallar.…”

Section: Introductionmentioning

confidence: 99%

“…In particular, according to the authors (Aliyarov, et al, 2018;Hasanov, et al, 2017;Gurbanov, et al, 2020;Guliyev, et al, 2014), Cretaceous and Jurassic terrigenous-carbonate reservoirs in the complex are characterized by more favorable conditions for the search for new oil and gas fields in the northwestern part of the country. Thus, according to (Hasanov, et al, 2017;Hasanov, Ganbarova, 2019), the maximum thickness of deposits (1117 m) in the territory of the Kura-Gabirri oil and gas region was identified in the areas of Mammadtapa(1037 m) and Tarsdallar. Here, the Eocene deposits are divided into three series (lower, middle, and upper), differing from each other in lithological properties.…”

Section: Introductionmentioning

confidence: 99%

“…From 1976 to 1993, the area of the field was almost completely covered by regional and detailed seismic surveys to depths of 5-6 km using various seismic survey methods (CDP, MCDP). Accurate gravimetric measurements were made in 1975, 1981, 1987. Based on these studies, it was possible to identify and maping the regional tectonic elements of the region (Akhundov and Ganiyev, 2016;Hasanov, et al, 2017).…”

Section: Introductionmentioning

confidence: 99%

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Assessment of the deep oil and gas bearing potential onshore in the west of Azerbaijan (Tarsdallar area)

Hasanov¹,

Paşayev²,

Kаrimov³

et al. 2023

Journ. Geol., Geogr., and Geoec..

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The Tarsdeller oil and gas field, which has a brachyoanthicline structure, is the most promising area of the oil-gas region (OGR) in the Kura-Gabirri interfluve. Goal: Based on the reservoir characteristics of rock samples obtained from exploration wells drilled in the area adjacent to the field, petrophysical models have been compiled, reflecting the spatial variation in porosity and permeability of oil-containing reservoirs. Objects: Consideration of the petrophysical properties of core samples taken in the study area made it possible to confirm the oil and gas potential of deep-seated reservoirs. Methods: This analyzed the values and variation of petrophysical properties by depth, age and various physical factors. The observed wide range of changes in the reservoir properties of rocks in the study area is mainly due to tectonic changes, lithological heterogeneity of the sedimentary complex, differences in the depth of bedrocks, as well as the complexity of tectonic conditions. As a result, to predict the oil and gas content in deep reservoirs of the same structures, it is advisable to use the methods of exploration geophysics, as well as the results of changes inthe reservoir characteristics of rocks, determined by petrophysical data. At the same time, it is most expedient to focus on the study of Paleogene-Cretaceous tectonics for the search for oil and gas objects using prospecting and exploration (preferably aerial-photo-space) works at the field. Results: Models made in 3D format illustrate the predicted oil and gas potential and patterns of distribution of productive horizons involved in the geological structure of oil and gas deposits, along the depths and stratigraphic units. It is shown that although the permeability of the rocks in the area is low, the porosity values are favorable for the industrial accumulation of hydro-carbons. Fractured carbonate reservoirs of the Upper Cretaceous are the most promising among the Mesozoic sediments in the OGRbetween the Kura and Gabirri rivers. Deep-seated structural uplifts complicated by large-amplitude fractures are recommended as the priority targets for further geological exploration. However, the real potential of the Eocene deposits, which are widespread in the NGR between the Kura and Gabirri rivers, remains unexplored by deep drilling. This is due, on the one hand, to the incomplete opening of the Eocene section in the structures prepared for deep drilling, structural-tectonic and lithofacies features, as well as insufficient knowledge of drilling for oil and gas, and on the other hand, poor development of promising intervals of the section.

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Section: Resultsmentioning

confidence: 99%

Section: Resultsmentioning

confidence: 99%