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Development features of volcanic rocks of the Yingcheng Formation and their relationship with fault structure in the Xujiaweizi Fault Depression, Songliao Basin, China

机译:松辽盆地徐家围子断陷凹陷营城组火山岩发育特征及其与断层构造的关系

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The Xujiaweizi Fault Depression is located in the northern Songliao Basin, Northeast China. The exploration results show that the most favorable natural gas reservoirs are in the volcanic rocks of the Yingcheng Formation (K_(1)yc). Based on seismic interpretation, drill cores and the results of previous research, we analyzed the distribution of faults and the thickness of volcanic rocks in different periods of K_(1)yc, and studied the relationship of volcanic activities and main faults. Volcanic rocks were formed in the Yingcheng period when the magma erupted along pre-existing fault zones. The volcanic activities strongly eroded the faults during the eruption process, which resulted in the structural traces in the seismic section being diffuse and unclear. The tectonic activities weakened in the study area in the depression stage. The analysis of seismic interpretation, thin section microscopy and drill cores revealed that a large number of fractures generated in the volcanic rocks were affected by later continued weak tectonic activities, which greatly improved the physical properties of volcanic reservoirs, and made the volcanic rocks of K_(1)yc be favorable natural gas reservoirs. The above conclusions provide the basis to better understand the relationship of the volcanic rock distribution and faults, the mechanism of volcanic eruption and the formation of natural gas reservoirs in volcanic rocks.
机译:徐家围子断陷位于中国东北的松辽盆地北部。勘探结果表明,最有利的天然气藏在应城组(K_(1)yc)的火山岩中。基于地震解释,钻探岩心和以往的研究成果,分析了K_(1)yc不同时期断层的分布和火山岩厚度,研究了火山活动与主要断层的关系。火山岩在应城时期形成,当时岩浆沿着既有的断裂带爆发。火山活动在喷发过程中强烈侵蚀了断层,致使地震剖面中的构造痕迹分散且不清楚。洼地阶段研究区的构造活动减弱。对地震解释,薄片显微镜和钻芯的分析表明,火山岩中产生的大量裂缝受到后来持续的弱构造活动的影响,极大地改善了火山岩储集层的物理性质,使K_ (1)是有利的天然气藏。以上结论为更好地了解火山岩的分布与断层的关系,火山喷发的机理以及火山岩中天然气藏的形成提供了依据。

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