Sedimentation features of reservoir formation and leakage assessment of the Galmaz underground gas storage

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Název: Sedimentation features of reservoir formation and leakage assessment of the Galmaz underground gas storage
Autoři: Yusubov, N.P., Rajabli, J.B., Quliyeva, U.M.
Zdroj: Геофизический журнал, Vol 42, Iss 6 (2020)
Geofizicheskiy Zhurnal; Vol. 42 No. 6 (2020); 222-229
Геофизический журнал; Том 42 № 6 (2020); 222-229
Геофізичний журнал; Том 42 № 6 (2020); 222-229
Informace o vydavateli: Institute of Geophysics of the National Academy of Sciences of Ukraine by S.I. Subbotin name, 2020.
Rok vydání: 2020
Témata: Geography (General), QE1-996.5, 3D сейсмічний куб, lithology cube, длина сейсмического сигнала, роздільна здатність сейсморозвідки, 3D сейсмический куб, seismic signal length, Geology, reservoirs, пласты-коллекторы, seismic resolution, 6. Clean water, разрешающая способность сейсморазведки, пласти-колектори, куб литологии, 13. Climate action, 3D seismic cube, G1-922, довжина сейсмічного сигналу, куб літології
Popis: The performed complex interpretation of the data of three-dimensional seismic exploration and geophysical study of wells (GIS) using the results obtained from the analysis of core material by laboratory and experimental methods, making it possible to identify paleo conditions for the formation of objects with collector and screening properties on the Galmaz area. The results of the study, which revealed the lithological features of the structure of natural reservoirs, served as the basis for assessing the reservoir properties of the reservoirs and the tightness of the shielding horizons, to which the Galmaz underground gas storage is confined. According to the authors, in the formation, which was in operation for a long time (1960—2006), the Galmaz gas field was mainly played by the eruptive channels of the mud volcano of the same name. At the same time, the maternal strata of the Oligocene—Miocene were the gas-generating source. The results of a comprehensive interpretation of seismic data and well logging showed that confined deposits to reservoirs of the productive stratum (PT-I), Akchagyl and Apsheron are communicated through eruptive channel of a mud volcano. Tire layers, represented by transgressive clays accumulated in shelf conditions, are reliable enough for storage of gas by covers.
Druh dokumentu: Article
Other literature type
Popis souboru: application/pdf
ISSN: 2524-1052
0203-3100
DOI: 10.24028/gzh.0203-3100.v42i6.2020.222301
Přístupová URL adresa: http://journals.uran.ua/geofizicheskiy/article/download/222301/223431
https://doaj.org/article/61ff9f553c15439681f833ca61897c96
http://journals.uran.ua/geofizicheskiy/article/view/222301
Rights: CC BY
Přístupové číslo: edsair.doi.dedup.....8a84e2dc19f98dfa7df051b84c5dc41c
Databáze: OpenAIRE
Popis
Abstrakt:The performed complex interpretation of the data of three-dimensional seismic exploration and geophysical study of wells (GIS) using the results obtained from the analysis of core material by laboratory and experimental methods, making it possible to identify paleo conditions for the formation of objects with collector and screening properties on the Galmaz area. The results of the study, which revealed the lithological features of the structure of natural reservoirs, served as the basis for assessing the reservoir properties of the reservoirs and the tightness of the shielding horizons, to which the Galmaz underground gas storage is confined. According to the authors, in the formation, which was in operation for a long time (1960—2006), the Galmaz gas field was mainly played by the eruptive channels of the mud volcano of the same name. At the same time, the maternal strata of the Oligocene—Miocene were the gas-generating source. The results of a comprehensive interpretation of seismic data and well logging showed that confined deposits to reservoirs of the productive stratum (PT-I), Akchagyl and Apsheron are communicated through eruptive channel of a mud volcano. Tire layers, represented by transgressive clays accumulated in shelf conditions, are reliable enough for storage of gas by covers.
ISSN:25241052
02033100
DOI:10.24028/gzh.0203-3100.v42i6.2020.222301