Oil and gas presence perspectives of weathering layer reservoir of Nurol'ka mega-basin according to data of geothermics; IOP Conference Series: Earth and Environmental Science; Vol. 43 : Problems of Geology and Subsurface Development
| Parent link: | IOP Conference Series: Earth and Environmental Science Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012014, 6 p.] |
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| Otros Autores: | , |
| Sumario: | Title screen Oil perspective areas of the Nurol'ka mega-basin (south-east of Western Siberia) through the M formation (Permian-Triassic weathering crust) on the basis of the results application of geothermometry were identified. Accumulating power distribution and quality of the M formation collectors were taken into account. The priority area for research are weathering layer reservoirs and its development that cover the South beads of Kulan-Igayskaya and Tamradskaya basins and its insulation joint were proposed. Glukhov's oil field that is located in this area approve its high prospectivity. |
| Lenguaje: | inglés |
| Publicado: |
2016
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| Colección: | Petroleum Geology: Current Exploration and Extraction Methods |
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| Acceso en línea: | http://dx.doi.org/10.1088/1755-1315/43/1/012014 http://earchive.tpu.ru/handle/11683/35123 |
| Formato: | Electrónico Capítulo de libro |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650810 |
| Sumario: | Title screen Oil perspective areas of the Nurol'ka mega-basin (south-east of Western Siberia) through the M formation (Permian-Triassic weathering crust) on the basis of the results application of geothermometry were identified. Accumulating power distribution and quality of the M formation collectors were taken into account. The priority area for research are weathering layer reservoirs and its development that cover the South beads of Kulan-Igayskaya and Tamradskaya basins and its insulation joint were proposed. Glukhov's oil field that is located in this area approve its high prospectivity. |
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| DOI: | 10.1088/1755-1315/43/1/012014 |