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• W3119987855 abstract "PreviousNext No AccessSEG Technical Program Expanded Abstracts 2013Time-frequency domain electromagnetic sounding to map deep targets in M depressionAuthors: Gang YuZhanxiang HeXiaodong SuoWeibing DongHaizhen WanGang YuBGP, CNPCSearch for more papers by this author, Zhanxiang HeBGP, CNPCSearch for more papers by this author, Xiaodong SuoBGP, CNPCSearch for more papers by this author, Weibing DongBGP, CNPCSearch for more papers by this author, and Haizhen WanBGP, CNPCSearch for more papers by this authorhttps://doi.org/10.1190/segam2013-0367.1 SectionsSupplemental MaterialAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail Abstract This study discussed the application of time-frequency domain electromagnetic (TFEM) sounding technique to map and characterize the deep basement structure. It has enhanced our understanding of the deep basement structure of the Permian and Carboniferous formation in the M depression of the SH Basin in western China. The electrical structure from the 2 TFEM sounding inversion sections and residual gravity anomalies reflect the development of the east and west Carboniferous residues subsags within the M depression. In the east residues subsag, the Upper Carboniferous basement has the depth of 4,500 m ~ 5,000 m with a maximum depth up to 5,500 m. The Upper Carboniferous formation thickness is about 2,000 m ~ 2,500 m. In the west subsag, the Carboniferous basement depth is similar to the east subsag, but its thickness is smaller, usually about 1,500 m ~ 2,000 m. The M depression developed 2 Carboniferous residues subsags in the east and west direction. The TFEM inversion section shows a 1,000 m ~ 1,500 m thick low resistivity layer on the top of the east subsag but not on the top of the west subsag, and this low resistivity layer is thicker in the east and south direction but thinner in the west and north side. Therefore, we believe the east subsag located on the east-south side of M depression is the major residual hydrocarbon generation subsag, and it extends to the northeast side. This study has also identified local volcanic rock bodies with hydrocarbon potential in the Carboniferous residual hydrocarbon generation subsag on the southeast side of the M depression. Permalink: https://doi.org/10.1190/segam2013-0367.1FiguresReferencesRelatedDetails SEG Technical Program Expanded Abstracts 2013ISSN (print):1052-3812 ISSN (online):1949-4645Copyright: 2013 Pages: 5258 Publisher:Society of Exploration Geophysicists HistoryPublished: 19 Aug 2013 CITATION INFORMATION Gang Yu, Zhanxiang He, Xiaodong Suo, Weibing Dong, and Haizhen Wan, (2013), Time-frequency domain electromagnetic sounding to map deep targets in M depression, SEG Technical Program Expanded Abstracts : 785-789. https://doi.org/10.1190/segam2013-0367.1 Plain-Language Summary PDF DownloadLoading ..." @default.
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• W3119987855 date "2013-08-19" @default.
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• W3119987855 title "Time-frequency domain electromagnetic sounding to map deep targets in M depression" @default.
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