STUDIES OF VOLCANIC RESERVOIR FORMING CHARACTERISTICS OF CHANGLING FAULTED-DEPRESSION, THE SONGLIAO BASIN
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摘要: 松辽盆地长岭断陷营城组火山岩厚度大,岩石类型多,相态类型齐全。对火山岩储层微观特征进行系统观察分析,初步研究其形成机理。将火山岩储层形成划分为2个阶段:初始成岩作用阶段和成岩后生作用阶段。初始成岩作用形成原生孔隙;成岩后生作用形成次生孔隙;构造作用贯穿成岩的全过程,形成原生和次生各类各级别的裂缝;深部热液及生排烃作用对储层的改造作用明显。多期大规模构造运动是火山岩地层成为优质储层的主要动因。深部大量发育的优质火山岩储层具有巨大的勘探潜力。Abstract: The volcanic rock of Yingcheng Formation in the Changling Faulted-Depression of the Songliao Basin is thick with various types and facies.Microscopic characteristics and formation mechanism of volcanic rock reservoirs have been systematically observed.Formation of volcanic rock reservoirs is divided into 2 stages,the initial diagenesis stage and the later diagenesis stage.During the initial diagenesis stage,primary pores are formed.And in the later diagenesis stage,secondary pores are formed.Tectonic effects take place through out both the 2 stages,forming various primary and secondary cracks.Deep hydrothermal flow and hydrocarbon-generating effects have obviously transformed reservoir.Many large-scale tectonic movements are the main reasons that volcanic rocks turn to high quality reservoirs.Substantially developed high quality volcanic reservoirs in deep formation have enormous exploration potential.
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Key words:
- diagenesis /
- later diagenesis /
- reservoir /
- volcanic rock /
- Changling Faulted-Depression /
- Songliao Basin
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[1] 吴聿元,周荔青.松辽盆地主要断陷大中型油气田形成分布特征[J].石油实验地质,2007,29(3):231～237 [2] 吴群,周荔青.松辽盆地长岭断陷东部大中型火山岩(油)气田形成分布特征[J].石油实验地质,2009,31(1):40～45 [3] 周荔青,吴聿元,张淮.松辽盆地断陷层系油气成藏的分区特征[J].石油实验地质,2007,29(1):7～12 [4] 蒙启安,门广田,赵洪文等.松辽盆地中生界火山岩储层特征及对气藏的控制作用[J].石油与天然气地质,2002,23(3):285～292 [5] 秦伟军,刘超英.松辽盆地长岭断陷火山岩相与天然气成藏关系[J].石油实验地质,2008,30(4):328～332,339 [6] Wu C Z,Gu L X,Zhang Z Z,et al.Formation mechanisms of hydrocarbon reservoirs associated with volcanic and subvolcanic intrusive rocks:Examples in Mesozoic-Cenozoic basins of eastern China[J].AAPG Bulletin,2006,90(1):137～147 [7] Rohrman M.Prospectivity of volcanic basins:Trap delineation and acreage de-risking[J].AAPG Bulletin,2007,91(6):915～939 [8] 高有峰,刘万洙,纪学雁等.松辽盆地营城组火山岩成岩作用类型、特征及其对储层物性的影响[J].吉林大学学报(地球科学版),2007,37(6):1251～1257 [9] 张德会,张文淮,许国建.岩浆热液出溶和演化对斑岩成矿系统金属成矿的制约[J].地学前缘,2001,8(3):193～201 [10] Dobson F,Kneafsey T,Hulen J,et al.Porosity,permeability and fluid flow in the Yellowstone geothermal system,Wyoming[J].Journal of Volcanology and Geothermal Research,2003,123:313～324 [11] 高波,陶明信,王万春等.深部热流体对油气成藏的影响[J].矿物岩石地球化学通报,2001,20(1):30～34 [12] Navon O,Hutcheon I D,Rossman G R,et al.Mantle-derived fluids in diamond micro-inclusions[J].Nature,1988,335:784～789 [13] 刘宝珺.沉积成岩作用[M].北京:科学出版社,1989.21～22 -
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