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This article analyzes the prospects of petroleum potential in Kurgan region. The relevance of the work is due to the high degree of development of the traditional oil and gas recovery areas of Western Siberia, which leads to the need to organize search activities in areas with a low density of hydrocarbon resources. We have analyzed the results of exploratory drilling in the area of the Alabuga river in Kurgan region, and have studied the history of detections of onshore oil occurrences there. Based on the results of the retrospective analysis, the research area was determined, field work was performed to determine the state of search wells in the area, and a collection of geochemical soil and liquid samples was selected. The analysis of the samples revealed that all of them contain methane and its homologues up to and including pentane. The genesis of light methane homologs is related to the processes of catagenesis; their detection on the surface indicates active processes of generation and migration of petroleum hydrocarbons. Based on the analysis of archival materials and estimated ground-based geochemical studies, a conclusion is made about petroleum potential in Kurgan region.
This article analyzes the prospects of petroleum potential in Kurgan region. The relevance of the work is due to the high degree of development of the traditional oil and gas recovery areas of Western Siberia, which leads to the need to organize search activities in areas with a low density of hydrocarbon resources. We have analyzed the results of exploratory drilling in the area of the Alabuga river in Kurgan region, and have studied the history of detections of onshore oil occurrences there. Based on the results of the retrospective analysis, the research area was determined, field work was performed to determine the state of search wells in the area, and a collection of geochemical soil and liquid samples was selected. The analysis of the samples revealed that all of them contain methane and its homologues up to and including pentane. The genesis of light methane homologs is related to the processes of catagenesis; their detection on the surface indicates active processes of generation and migration of petroleum hydrocarbons. Based on the analysis of archival materials and estimated ground-based geochemical studies, a conclusion is made about petroleum potential in Kurgan region.
The article presents the facts of possible gas field discovery in Petukhovo district of Kurgan region. In 1962, a structural prospecting well 4-G was drilled to a depth of 928 m in the area of Petukhovo state farm in Kurgan region. When drilling the well in the process of trial pumping from a depth of 900.85-923.4 m, a gas release occurred with a rapid release of combustible methane gas. The first signs of weak carbonation were observed from a depth of 227 m, gas indicators didn't exceed 7%.Subsequent seismic surveys established a calm occurrence of sediments of Mesocainozoic age and revealed a weak dislocation of rocks of the Paleozoic complex. The study of the surface of the lower reference reflecting horizon, which is linked to the bottoms of Mesozoic sediments or the roof of the Paleozoic foundation, made it possible to identify three local positive structures: Medvedevskoe, in the area of Lake Medvezhye, measuring 4×13 km, contoured with an isohypse of -700 m, with an amplitude of 50 m; the west of the village of Kazantsevskoye, measuring 1×2.5 km, contoured with an isohypse of -650 m; the north of the village of Kazantsevskoye, measuring 2×3.5 km, contoured with an isohypse of -700 m, with an amplitude of 50 m. The selected structures at that time were recommended for testing oil and gas prospects by drilling. In case of positive results, it was recommended to continue areal seismic studies in order to delineate the selected uplifts the north of the village of Pashkovo and the northwest of the village of Grenadiers, followed by their verification by drilling.The authors of the article carried out an expedition to Petukhovo district. As a result, they found liquidated wells in the north of Lake Domozhirovo (presumably, wells 4-G and 2-PR), the conditions of mouths of these wells were established. The authors give recommendations for conducting geological exploration in the territory of Petukhovo district.
This article presents the results of drilling a 1-k core well in Zverinogolovskoye district of Kurgan region and the study of core material. A number of researchers have doubts about the fact that the reason of periodic appearance of an oil film on the Alabuga River was the migration of oil from the depths. Some people assumed that it could get to the river in a small amount by accident, for example, farmers spilled it during fieldwork. In 1959, 1-k and 2-k wells were drilled in order to check and study oil occurrences along the Alabuga River. Core wells 1-k and 2-k have traversed the cover deposits of the Meso-Cenozoic and have exposed the basement rocks represented by red flowers of presumably Permian-Triassic age. This made it possible to study the lithology and stratigraphy of the sediments, which were involved in the structure of the area. The angles of inclination of red-colored rocks measured by the core of the 1-k well give an idea of the degree of their disturbance. The facies-lithological features of these rocks, the absence of fauna and flora in them, and other signs indicate that the formation of red-colored deposits occurred under continental conditions. The signs of Permian-Triassic oil found in the 1-k well are of fundamental importance. These oil occurrences are also of interest in the fact that they were detected in the area, where oil was observed to the surface.
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