凝灰岩气藏成藏期次及成藏模式——以松辽盆地德惠断陷火石岭组为例

Accumulation stages and model of tuff gas reservoir: a case study of Huoshiling Formation in Dehui Fault Depression, Songliao Basin

  • 摘要: 松辽盆地德惠断陷上侏罗统火石岭组凝灰岩气藏有望成为中国第一个有工业开发价值的凝灰岩气藏。由于德惠断陷多期构造活动与多期生排烃相互叠加,凝灰岩气藏成藏过程复杂,又因开发时间较短,因此目前还缺乏对气藏成藏规律的认识。运用流体包裹体、三维地震、岩心、铸体薄片等资料,通过对凝灰岩流体包裹体进行岩相学分析、均一温度及盐度测定,结合德惠断陷埋藏史—热演化史模拟,厘定了火石岭组凝灰岩气藏成藏期次、时间,建立了气藏成藏模式。研究结果表明:火石岭组凝灰岩储层中主要发育含烃类盐水包裹体,其大多赋存于石英颗粒微裂缝及孔隙内,呈群状、带状分布,无明显荧光特性;包裹体均一温度呈现双峰式特征,峰值在100~110 ℃和115~125 ℃,凝灰岩储层发生过2期天然气充注,分别为早白垩世中期(127~133 Ma)和早白垩世晚期(106~114 Ma),主成藏期为早白垩世晚期;烃源岩、储—盖组合、断裂共同控制着凝灰岩气藏富集,气藏基本分布在凝灰岩上部;建立了松辽盆地德惠断陷火石岭组凝灰岩气藏“多源供烃、断裂输导、高位富集”的成藏模式。

     

    Abstract: The tuff gas reservoir in the Upper Jurassic Huoshiling Formation of the Dehui Fault Depression, Songliao Basin is expected to become the first tuff gas reservoir with industrial development value in China. However, due to the combined effects of multi-stage tectonic activities and multi-stage hydrocarbon generation and expulsion in Dehui Fault Depression, the accumulation process of the tuff gas reservoir is complex. Furthermore, the development history is relatively short, resulting in a current lack of understanding of the gas reservoir accumulation patterns. Using data including fluid inclusions, three-dimensional earthquake, cores, and cast thin sections, through petrographic analysis of tuff fluid inclusions and determination of homogenization temperature and salinity, combined with burial history and thermal evolution history simulation of the Dehui Fault Depression, the accumulation stage and time of tuff gas reservoir in the Huoshiling Formation were determined. A gas reservoir accumulation model was subsequently established. The results showed that the tuff reservoir of the Huoshiling Formation was mainly dominated by hydrocarbon-bearing saline inclusions. These inclusions were mostly found in micro-fractures and pores of quartz particles, showing clustered and banded distribution without distinct fluorescence characteristics. The homogenization temperatures of the inclusions showed bimodal characteristics, with peaks at 100 to 110 ℃ and 115 to 125 ℃. The tuff reservoir experienced two stages of natural gas injection in the middle Early Cretaceous (127 to 133 Ma) and late Early Cretaceous (106 to 114 Ma), with the main accumulation period in the late Early Cretaceous. Source rocks, reservoir and caprock combinations, and faults jointly controlled the enrichment of the tuff gas reservoir, with the gas reservoir mainly distributed in the upper part of the tuff. An accumulation model of "multi-source hydrocarbon supply, fault migration, and high-position enrichment" for the tuff gas reservoir in Huoshiling Formation of Dehui Fault Depression, Songliao Basin was established.

     

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