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- W2377574810 abstract "The combustible gas and burned tunnels founded in the Dabie orogenic belt are concentrated to the North Dabie complex zone south of the Mozitan-Xiaotian fault and the Early Carboniferous metamorphosed quartz schist close to the Xinyang-Shucheng fault.The two faults have provided gas source pathways which are connected to deeper reservoir rocks.The Lower Cambrian Fengtai Formation below thrust nappes and the North Huaiyang Carboniferous strata,both of which occur as the marine source rocks,are considered as the main gas source of the tunnel combustible gas.The Lower Cambrian Fengtai Formation consists of the continental marginal deposits,in which the marine muddy source have been in an oversaturation stage of thermal evolution characterized by high carbon,high Ro,high Tmax and lower chloroform-bitumen A.The North Huaiyan Carboniferous source have high abundances of organic matter with the III-type kerogen and high thermal maturation,resulting in the generation of abundant hydrocarbons.The discovery of the tunnel combustible gas indicates that the deep-seated marine strata in the Hefei Basin may be highly prospective for oil and gas resources.The future exploration should be carried out from the Mesozoic and Cenozoic basin systems to the deep-seated marine strata,with the emphasis on the source and Palaeozoic reservoir rocks or source and Cenozoic reservoir rocks." @default.
- W2377574810 created "2016-06-24" @default.
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- W2377574810 date "2009-01-01" @default.
- W2377574810 modified "2023-09-23" @default.
- W2377574810 title "Evolution and hydrocarbon potential of the marine strata on the southeastern margin of the North China plate" @default.
- W2377574810 hasPublicationYear "2009" @default.
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