1. 自然资源部构造成矿成藏重点实验室(成都理工大学),四川,成都,610059
2. 成都理工大学地球与行星科学学院,四川,成都,610059
3. 大庆油田有限责任公司勘探开发研究院,黑龙江,大庆,163712
网络出版:2025-05-10,
纸质出版:2025
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赵波, 尹淑敏, 李忠权, 孙国昕, 刘筝, 李晶. 松辽盆地北部中央隆起带岩浆岩潜山优质储层特征及控制因素[J]. 石油学报, 2025, 46(4): 692-707.
Zhao Bo, Yin Shumin, Li Zhongquan, et al. Characteristics and controlling factors of high-quality reservoirs in magmatic rock buried-hill of the central uplift zone,northern Songliao Basin[J]. ACTA PETROLEI SINICA, 2025, 46(4): 692-707.
赵波, 尹淑敏, 李忠权, 孙国昕, 刘筝, 李晶. 松辽盆地北部中央隆起带岩浆岩潜山优质储层特征及控制因素[J]. 石油学报, 2025, 46(4): 692-707. DOI: 10.7623/syxb202504003.
Zhao Bo, Yin Shumin, Li Zhongquan, et al. Characteristics and controlling factors of high-quality reservoirs in magmatic rock buried-hill of the central uplift zone,northern Songliao Basin[J]. ACTA PETROLEI SINICA, 2025, 46(4): 692-707. DOI: 10.7623/syxb202504003.
中央隆起带岩浆岩潜山气藏是松辽盆地北部深层天然气风险勘探的重要领域之一
但其优质储层特征及控制因素尚不清晰
严重制约了气藏的勘探进程。利用钻井、测井、地震资料以及分析化验数据详细分析了中央隆起带岩浆岩潜山的储层特征及优质储层的控制因素。研究结果表明:中央隆起带岩浆岩潜山在垂向上分为风化堆积层、风化淋滤层、裂缝层和岩浆岩致密层;储层属于低孔、超低渗储层;储层的储集空间类型为粒间溶蚀孔、粒内溶蚀孔、石英原生晶间孔以及构造裂缝和微裂缝
与微裂缝沟通的微米—纳米级孔隙可为天然气的聚集提供储集空间;裂缝走向主要为NNW向、NNE向、NE向和NW向
裂缝倾角以中—高角度为主;花岗岩和碎裂花岗岩储层的物性相对较好、其裂缝发育、裂缝开启程度好
是中央隆起带岩浆岩潜山成储的优势岩性;多期构造叠加作用、风化淋滤作用和有机酸溶蚀作用
以及构造高部位等因素
控制了松辽盆地北部中央隆起带岩浆岩潜山优质储层的发育。研究为推进岩浆岩潜山的天然气勘探开发提供了依据。
The magmatic rock buried-hill gas reservoir in the central uplift zone of northern Songliao Basin is one of the important areas for risk exploration of deep natural gas
and the characteristics and controlling factors of high-quality reservoirs are still unclear
thus severely restricting the gas reservoir exploration process. Based on the drilling
logging
seismic data and analytical test data
this paper analyzes in detail the reservoir characteristics of magmatic rock buried-hill and the controlling factors of high-quality reservoirs in the central uplift zone. The research results show that the magmatic rock buried-hill in the central uplift zone can be vertically divided into weathered accumulation layer
weathering-leaching layer
fracture layer and tight magmatic rock layer
showing the characteristics of reservoirs with low-porosity and ultra-low permeability. The reservoir spaces include the intergranular dissolution pores
intragranular dissolution pores
quartz primary intergranular pores
structural fractures and micro-fractures. The micron and nanoscale pores communicating with micro-fractures can provide storage space for natural gas. The NNW-
NNE-
NE- and NW-trending fractures are mainly developed in the study area
with the medium to high dip angles. Granite and cataclastic granite reservoirs have relatively good physical properties
well-developed fractures
and high degree of fracture opening
and are the dominant lithologies of magmatic rock buried-hill reservoir in the central uplift zone. The controlling factors such as multi-stage structural superposition
weathering leaching
organic acid dissolution
and structural high locations have controlling effects on the development of high-quality reservoirs in magmatic rock buried-hill of the central uplift zone of northern Songliao Basin. The research results provide a reference for promoting the natural gas exploration and development in magmatic rock buried-hills.
P’AN C H.Petroleum in basement rocks[J].AAPG Bulletin,1982,66(10):1597-1643.
WALTER B,GÉRAUD Y,BARTIER D,et al.Petrophysical and mineralogical evolution of weathered crystalline basement in western Uganda:implications for fluid transfer and storage[J].AAPG Bulletin,2018,102(6):1035-1065.
张功成,杨东升,郭帅,等.基岩潜山三元主导油气成藏模式——兼论南海北部深水区勘探新领域[J].天然气地球科学,2023,34(12): 2045-2061.
窦立荣,温志新,王兆明,等.全球古老油气成藏组合资源潜力、重大发现及启示[J].石油学报,2024,45(8):1163-1173.
叶涛,牛成民,王清斌,等.渤海湾盆地大型基岩潜山储层特征及其控制因素——以渤中19-6凝析气田为例[J].地质学报,2021,95(6):1889-1902.
徐长贵,杜晓峰,刘晓健,等.渤海海域太古界深埋变质岩潜山优质储集层形成机制与油气勘探意义[J].石油与天然气地质,2020,41(2):235-247.
李娟,卫平生,石兰亭,等.海拉尔盆地贝尔凹陷基岩储集层流体作用机制与成岩改造[J].石油勘探与开发,2020,47(1):45-56.
杜晓峰,刘晓健,张新涛,等.渤海海域太古界变质岩储层特征与形成控制因素[J].中国海上油气,2021,33(3):15-27.
王德英,刘晓健,邓辉,等.渤海湾盆地渤中19-6区中—新生代构造转换特征及其对太古宇潜山大规模储层形成的控制作用[J].石油与天然气地质,2022,43(6):1334-1346.
杜金虎.松辽盆地中央古隆起带(北部)天然气成藏条件分析及勘探前景[J].中国石油勘探,2017,22(5):1-14.
王春燕,史鹏宇,李晶,等.松辽盆地古中央隆起带基底浅变质岩岩性测井解释及其应用[J].大庆石油地质与开发,2020,39(2):125-132.
张帆,冉清昌,吴玉明,等.松辽盆地北部古中央隆起带天然气地球化学特征及成藏条件[J].天然气地球科学,2019,30(1):126-132.
易士威,李明鹏,徐淑娟,等.松辽盆地中央隆起潜山成藏条件及模式[J].天然气地球科学,2020,31(12):1663-1676.
孙立东,孙国庆,杨步增,等.松辽盆地北部中央古隆起带古潜山天然气成藏条件[J].天然气工业,2020,40(3):23-29.
孙立东,陆加敏,杨步增,等.松辽盆地北部中央古隆起带天然气成藏条件与勘探方向[J].石油学报,2020,41(10):1163-1173.
张顺,王丽静,张博远,等.松辽盆地安达古隆起风化壳特征及控藏机制[J].大庆石油地质与开发,2019,38(1):9-16.
ZENG Z Q,SHAN X L,HAO G L,et al.Semiquantitative microscopic pore characterizations of the metamorphic rock reservoir in the central paleo-uplift belt,Songliao Basin[J].Scientific Reports,2022,12:2606.
赵波,丁寒生,尹淑敏,等.松辽盆地北部中央隆起带基岩潜山天然气成藏主控因素与成藏模式[J].石油学报,2024,45(12):1783-1799.
余和中,李玉文,韩守华,等.松辽盆地古生代构造演化[J].大地构造与成矿学,2001,25(4):389-396.
LIU Y J,LI W M,FENG Z Q,et al.A review of the Paleozoic tectonics in the eastern part of Central Asian orogenic belt[J].Gondwana Research,2017,43:123-148.
王成文,金巍,张兴洲,等.东北及邻区晚古生代大地构造属性新认识[J].地层学杂志,2008,32(2):119-136.
黄清华,朱国同,王辉,等.松辽盆地古中央隆起带基岩锆石U-Pb年龄及其地质意义[J].大庆石油地质与开发,2019,38(3):1-7.
冯志强,董立,童英,等.蒙古-鄂霍茨克洋东段关闭对松辽盆地形成与演化的影响[J].石油与天然气地质,2021,42(2):251-264.
曲希玉,张满利,刘立,等.中国东北地区晚二叠世岩相古地理特征[J].古地理学报,2013,15(5):679-692.
李宁,王成文.东北及邻区晚古生代地层接触关系与佳-蒙地块的形成和演 化[J].吉林大学学报(地球科学版),2017,47(5):1331-1340.
李锦轶,刘建峰,曲军峰,等.中国东北地区古生代构造单元:地块还是造山带?[J].地球科学,2019,44(10):3157-3177.
邢大全,刘永江,唐振兴,等.松辽盆地上古生界构造格局及演化探究[J].世界地质,2015,34(2):396-407.
王璞珺,赵然磊,蒙启安,等.白垩纪松辽盆地:从火山裂谷到陆内拗陷的动力学环境[J].地学前缘,2015,22(3):99-117.
田有,马锦程,刘财,等.西太平洋俯冲板块对中国东北构造演化的影响及其动力学意义[J].地球物理学报,2019,62(3):1071-1082.
单玄龙,秦树洪,张艳,等.松辽盆地北部浅部基底推覆伸展作用的地震学证据与地质意义[J].地球物理学报,2009,52(8):2044-2049.
葛荣峰,张庆龙,王良书,等.松辽盆地构造演化与中国东部构造体制转换[J].地质论评,2010,56(2):180-195.
万双双.松辽盆地北部构造演化研究[D].成都:成都理工大学,2012:1-74.
WU F Y,SUN D Y,LI H M,et al.The nature of basement beneath the Songliao Basin in NE China:geochemical and isotopic constraints[J].Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,2001,26(9/10):793-803.
史鹏宇.古中央隆起带基岩测井解释方法研究[D].大庆:东北石油大学,2020:1-123.
CHALMERS G R,BUSTIN R M,POWER I M.Characterization of gas shale pore systems by porosimetry,pycnometry,surface area,and field emission scanning electron microscopy/transmission electron microscopy image analyses:examples from the Barnett,Woodford,Haynesville,Marcellus,and Doig units[J].AAPG Bulletin,2012,96(6):1099-1119.
许文良,孙晨阳,唐杰,等.兴蒙造山带的基底属性与构造演化过程[J].地球科学,2019,44(5):1620-1646.
许文良,王旖旎,王枫,等.西太平洋俯冲带的演变:来自东北亚陆缘增生杂岩的制约[J].地质论评,2022,68(1):1-17.
唐杰,许文良,王枫,等.古太平洋板块在欧亚大陆下的俯冲历史:东北亚陆缘中生代-古近纪岩浆记录[J].中国科学:地球科学,2018,48(5):549-583.
黄云飞,张昌民,朱锐,等.准噶尔盆地玛湖凹陷晚二叠世至中三叠世古气候、物源及构造背景[J].地球科学,2017,42(10):1736-1749.
NESBITT H W,YOUNG G M.Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J].Nature,1982,299(5885):715-717.
王昕,周心怀,徐国胜,等.渤海海域蓬莱9-1花岗岩潜山大型油气田储层发育特征与主控因素[J].石油与天然气地质,2015,36(2): 262-270.
余朝华,杜业波,肖坤叶,等.乍得Bongor盆地基岩潜山储层特征与影响因素研究[J].岩石学报,2019,35(4):1279-1290.
孔垂显,陈轩,秦军,等.中-基性火山岩孔缝储集体形成控制因素——以准噶尔盆地金龙区块石炭系为例[J].石油与天然气地质,2018,39(3):558-566.
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