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- W2384961608 abstract "The Songliao Basin is composed of two basin filling episodes.The lower part,generally being buried more than 3 000 m beneath the surface,consists of Late Jurassic and Early Cretaceous volcanogenic successions including Huoshiling Formation(J_(3)h),Shahezi Formation(K_(1)sh) and Yingcheng Formation( K_(1)y) which were formed in the block-faulting stage.The upper part is made up of normal sedimentary sequence of Albian to Maastrichtian stages,which was formed in the sagging episode of the basin evolution.The volcanic rocks of Yingcheng Formation contribute 87% of the reservoirs for the deep basin gases. Porosity and permeability of the reservoir volcanic rocks are facies-controlled.The best volcanic reservoirs are commonly found among those subfacies including diatreme(Ⅰ_(1)),crypto-explosive breccia(Ⅰ_(3)),pyroclastic bearing lava flow(Ⅱ_(3)),upper effusive(Ⅲ_(3)) and inner extrusive ones(Ⅳ_(1)),with the latter two ones being the best.Commercial gases found in the volcanic reservoirs there include hydrocarbon,CO_(2),N_(2),H_(2)S and some noble gases.Multi-sources for those gases are concluded,i.e.a mixture of gases from coal,mudstone,and abiogenic origin gases which may be mantle/magma-derived,based on composition of the natural gases trapped,the C/H isotopes of the hydrocarbon and CO_(2)." @default.
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- W2384961608 date "2007-01-01" @default.
- W2384961608 modified "2023-09-26" @default.
- W2384961608 title "Characteristics of volcanic facies and genesis of natural gases in deep Songliao Basin,NE China" @default.
- W2384961608 hasPublicationYear "2007" @default.
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