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Volcanic rocks as prolific gas reservoir:A case study from the Qingshen gas field in the Songliao Basin,NE China

机译:火山岩为多产气藏-以松辽盆地庆深气田为例

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摘要

The Qingshen gas field,with over 100 billion cubic meters(bcms)of proven gas reserves,was discovered recently in the Upper Jurassic-Lower Cretaceous strata of the Songliao Basin,northeastern China. The stratigraphic relationships and gas chemical compositions indicate mixed gas sources,dominantly from the Upper Jurassic-Lower Cretaceous coals and associated dark mudstones underlying the gas reservoirs,with minor contribution from deep inorganic sources. The gas reservoirs consist mainly of volcanic rocks(rhyolite and tuff),with some production also from the conglomerate. Gas charge into these largely volcanic rock reservoirs appears to coincide with the peak gas generation in the deep Upper Jurassic-Lower Cretaceous coal measures. The presence of several thick lacustrine mudstone beds in the Upper Cretaceous strata as regional caprocks and relatively mild structural deformation since the late Cretaceous are among the favorable conditions for the preservation of large volume of natural gases in these relatively deep gas reservoirs. The gas yields are the highest in the paleomorphological highs where fractures and secondary porosity are well developed in the gas reservoirs.
机译:在中国东北的松辽盆地上侏罗统-下白垩统地层发现了探明天然气储量超过1000亿立方米的青神气田。地层关系和气体化学成分显示混合气源,主要来自上侏罗统-下白垩统煤和气藏下方的相关深色泥岩,深部无机源贡献不大。气藏主要由火山岩(流纹岩和凝灰岩)组成,一些也来自砾岩。这些火山岩储集层中的天然气充注似乎与上侏罗统—下白垩统深层煤层气的峰值产生时间一致。自白垩纪晚期以来,上白垩统地层中存在数个较厚的湖相泥岩层作为区域盖层,并且结构变形相对温和,这是在这些相对较深的气藏中保存大量天然气的有利条件。在古地貌高处,天然气的产量最高,在天然气藏中裂缝和次生孔隙发育良好。

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