E. Rzayeva, S. Mammadova, T. A. Askerov, T. Hamzayeva
{"title":"Gobustan含油气区Shaigler-Gaibler剖面萨尔马提亚沉积物微动物群与生物学","authors":"E. Rzayeva, S. Mammadova, T. A. Askerov, T. Hamzayeva","doi":"10.37474/0365-8554/2023-04-12-16","DOIUrl":null,"url":null,"abstract":"Biostratigraphic characteristics of Sarmatian sediments in South-eastern Gobustan is presented according to the data of Shaigler-Gaibler section; the systematic composition and characteristic complexes of microfossils – foraminifers, ostracods, otolites and the fish remnants are defined. As a result of the biostratigraphic division of the section carried out, it was revealed that the sediments of Sarmatian stage participate in the geological structure of Shaigler-Gaibler anticline; there are no Upper Sarmatian sediments in the section. The scheme of division of Sarmatian sediments in Shaigler-Gaibler sections which may be applied for the further geological surveys in the other areas of South-eastern Gobustan, has been developed. The results obtained may be used for the biostratigraphic research of deeply buried Miocene sediments of Western edge of South Caspian.","PeriodicalId":8668,"journal":{"name":"Azerbaijan Oil Industry","volume":"15 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2023-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Microfauna complex and bionomy of Sarmatian sediments of Shaigler-Gaibler section (Gobustan oil-gas bearing region)\",\"authors\":\"E. Rzayeva, S. Mammadova, T. A. Askerov, T. Hamzayeva\",\"doi\":\"10.37474/0365-8554/2023-04-12-16\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Biostratigraphic characteristics of Sarmatian sediments in South-eastern Gobustan is presented according to the data of Shaigler-Gaibler section; the systematic composition and characteristic complexes of microfossils – foraminifers, ostracods, otolites and the fish remnants are defined. As a result of the biostratigraphic division of the section carried out, it was revealed that the sediments of Sarmatian stage participate in the geological structure of Shaigler-Gaibler anticline; there are no Upper Sarmatian sediments in the section. The scheme of division of Sarmatian sediments in Shaigler-Gaibler sections which may be applied for the further geological surveys in the other areas of South-eastern Gobustan, has been developed. The results obtained may be used for the biostratigraphic research of deeply buried Miocene sediments of Western edge of South Caspian.\",\"PeriodicalId\":8668,\"journal\":{\"name\":\"Azerbaijan Oil Industry\",\"volume\":\"15 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-04-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Azerbaijan Oil Industry\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.37474/0365-8554/2023-04-12-16\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Azerbaijan Oil Industry","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.37474/0365-8554/2023-04-12-16","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Microfauna complex and bionomy of Sarmatian sediments of Shaigler-Gaibler section (Gobustan oil-gas bearing region)
Biostratigraphic characteristics of Sarmatian sediments in South-eastern Gobustan is presented according to the data of Shaigler-Gaibler section; the systematic composition and characteristic complexes of microfossils – foraminifers, ostracods, otolites and the fish remnants are defined. As a result of the biostratigraphic division of the section carried out, it was revealed that the sediments of Sarmatian stage participate in the geological structure of Shaigler-Gaibler anticline; there are no Upper Sarmatian sediments in the section. The scheme of division of Sarmatian sediments in Shaigler-Gaibler sections which may be applied for the further geological surveys in the other areas of South-eastern Gobustan, has been developed. The results obtained may be used for the biostratigraphic research of deeply buried Miocene sediments of Western edge of South Caspian.