松辽盆地南部红岗阶地和华字井阶地含片钠铝石砂岩中的黏土矿物特征
|
摘要
松辽盆地南部中央坳陷红岗阶地和华字井阶地含片钠铝石砂岩中黏土矿物主要由伊/蒙混层、伊利石和高岭石组成。采用比较岩石学和数值模拟方法,比较红岗阶地青山口组和华字井阶地泉头组含片钠铝石砂岩与对照组砂岩的岩石学特征。研究结果表明:含片钠铝石砂岩中绿泥石缺失,高岭石和伊利石质量分数显著增加;绿泥石溶解和高岭石沉淀作用发生在深大断裂附近,深大断裂是幔源CO2运移的主要通道;CO2充注引起注入点附近砂岩储层中绿泥石溶解和自生高岭石沉淀以及长石的高岭石化;长石等可溶性矿物的溶解,为伊/蒙混层向伊利石转化提供必需的K+,促进伊/蒙混层向伊利石的转化。
Clay minerals consist of illite/smectite,illite and kaolinite in dawsonite-bearing sandstones in Honggang terrace and Huazijing terrace in south of Songliao Basin.The petrology of dawsonite-bearing sandstone and control group from Honggang terrace and Huazijing terrace was investigated by the method of comparative petrology and numerical simulation.The results show that chlorite in dawsonite bearing sandstone is lack,and the mass fraction of kaolinite and illite significantly increases.Dissolution of chlorite and precipition of kaolinite occur in deep fault,which is the main channel of mantel-genetic CO2 influx.Chlorite dissolution,authigenic kaolinite precipition and kaolinization of feldspar are impacted by CO2 injection.CO2 inject leads to dissolubility feldspar dissolution.K-feldspar dissolution mainly provides K+,which is necessary for illitization of smectite.
Clay minerals consist of illite/smectite,illite and kaolinite in dawsonite-bearing sandstones in Honggang terrace and Huazijing terrace in south of Songliao Basin.The petrology of dawsonite-bearing sandstone and control group from Honggang terrace and Huazijing terrace was investigated by the method of comparative petrology and numerical simulation.The results show that chlorite in dawsonite bearing sandstone is lack,and the mass fraction of kaolinite and illite significantly increases.Dissolution of chlorite and precipition of kaolinite occur in deep fault,which is the main channel of mantel-genetic CO2 influx.Chlorite dissolution,authigenic kaolinite precipition and kaolinization of feldspar are impacted by CO2 injection.CO2 inject leads to dissolubility feldspar dissolution.K-feldspar dissolution mainly provides K+,which is necessary for illitization of smectite.
引文
[1]Pearce J M,Holloway S,Wacker H,et al.Natural occurrences asanalogues for the geological disposal of carbon dioxide[J].Energy Conversion and Management,1996,37:1123-1128.
[2]Watson M N,Zwingmann N,Lemon N M.The LadbrokeGrove-Katnook carbon dioxide natural laboratory:A recent CO2accumulation in a lithic sandstone reservoir[J].Energy,2004,29:1457-1466.
[3]XU Tianfu,Apps J A,Pruess K.Mineral sequestration of carbondioxide in a sandstone-shale system[J].Chemical Geology,2005,217:295-318.
[4]Lu J M,Wilkinson M,Haszeldine R,et al.Carbonate cements inMiller field of the UK North Sea:A natural analog for mineraltrapping in CO2-geological storage[J].Environmental EarthSciences.2011,62:507-517.
[5]ZHANG Wei,LI Yilian,XU Tianfu,et al.Long-term variationsof CO2-trapped in different mechanisms in deep salineformations:A case study of the Songliao Basin,China[J].International Journal of Greenhouse Gas Control,2009,3:161-180.
[6]Okuyama Y,Sasaki M,Nakanishi S,et al.Geochemical CO2trapping in open aquifer storage-the Tokyo Bay model[J].EnergyProcedia,2009(1):3253-3258.
[7]Credoz A,Bildstein O,Jullien M,et al.Mixed-layerillite-smectite reactivity in acidified solutions:Implications forclayey caprock stability in CO2-geological storage[J].AppliedClay Science,2011,53:402-408.
[8]徐同台,王行信,张有瑜,等.中国含油气盆地黏土矿物[M].北京:石油工业出版社.2003:87121.XU Tongtai,WANG Xingxin,ZHANG Youyu,et al.Claymineral in petroleum basin,China[M].Beijing:PetroleumIndustry Press.2003:87-121.
[9]侯启军,赵志魁,王立武.火山岩气藏:松辽盆地南部大型火山岩气藏勘探理论与实践[M].北京:科学出版社,2009:259-317.HOU Qijun,ZHAO ZHIkui,WANG Liwu.Volcanic gasreservoir:Theory and practice of exploration volcanic rock gasreservoir in south of Songliao Basin[M].Beijing:Science Press,2009:259-317.
[10]熊福生,史謌,孙永梅.松辽盆地两井孤店地区泉头组四段沉积微相研究[J].北京大学学报:自然科学版,2008,44(2):185-192.XIONG Fusheng,SHE Ge,SUN Yongmei,et al,Research onsedimentary Microfacies of Fourth Section of QuantouFormation in Liangjing Gudian Area of Songliao Basin[J].ActaScientiarum Naturalium Universitatis Pekinensis,2008,44(2):185-192.
[11]张庆国,鲍志东,那未红,等.松辽盆地中央坳陷南部下白垩统泉头组四段沉积相[J].古地理学报,2007,9(3):267-276.ZHANG Qingguo,BAO Zhidong,NA Weihong,et al.Sedimentary facies of the member 4-of Quantou Formation oflower cretaceous in Southern Central Depression of SongliaoBasin[J].Journal of Palaeogeography,2007,9(3):267-276.
[12]任战利,萧德铭,迟元林.松辽盆地古地温恢复[J].大庆石油地质与开发,2001,20(1):1314,55.REN Zhanli,XIAO Deming,CHI Yuanlin.Restoration of thePalaeogeotherm in songliao Basin[J].Petroleum Geology andOilfield Development in Daqing,2001,20(1):13-14,55.
[13]张英魁,刘斌,古武,等.利用多元回归方法确定岩石压缩系数[J].油气井测试,2001,10(1/2):79.ZHANG Yingkui,LIU Bin,GU Wu.Determine the rockcompressibility by the multiple regression analysis method[J].Well Testing,2001,10(1/2):7-9.
[14]Allard P.A CO2-rich gas trigger of explosive paroxysms atStromboli basaltic volcano,Italy[J].Journal of Volcanology andGeothermal Research,2010,189(3/4):363-374.
[15]刘立,刘娜,周冰,等.松辽盆地南部红岗背斜幔源-岩浆成因CO2大规模泄露的岩石学记录[J].吉林大学学报:地球科学版,2011,41(2):411420.LIU Li,LIU Na,ZHOU Bing,et al.Petrological Recording ofMantle-Magmatic CO2-Leakage on a Large-Scale in HonggangAnticline,Southern Songliao Basin[J].Journal of JilinUniversity:Earth Science Edition,2011,41(2):411-420.
[16]Felix B,Dirk B,Evelyn K B,et al.Chlorite dissolution in theacid pH-range:A combined microscopic and macroscopicapproach[J].Geochimica et Cosmochimica Acta,2003,67(8):1451-1461.
[17]楼章华,姚炎明,金爱民.松辽盆地地下流体地球化学特征研究[J].矿物学报.2002,22(4):343349.LOU Zhanghua,YAO Yanming,JIN Aimin,et al.Geochemicalproperties of underground fluids in Songliao Basin,China[J].Acta Mineralogica Sinica.2002,22(4):343-349.
[18]闫建萍,刘池阳,马艳萍.成岩作用与油气侵位对松辽盆地齐家—古龙凹陷扶杨油层物性的影响[J].沉积学报,2009,27(2):213-220.YAN Jianping,LIU Chiyang,MA Yanping.Influence ofdiagenesis and hydrocarbon emplacement on the quality of theFuyang Reservoir in Songliao Basin[J].Acta SedimentologicaSinica,2009,27(2):213-220.
[19]LIU Na,LIU Li,QU Xiyu,et al.Genesis of authigene carbonateminerals in the Upper Cretaceous Reservoir,Honggang Anticline,Songliao Basin:A natural analog for mineral trapping of naturalCO2storage[J].Sedimentary Geology,2011,237:166-178.
[20]杨光大.松辽盆地南部中央坳陷区高精度三维地震勘探方法研究[D].中国地质大学(北京):地球物理与信息技术学院,2006:3-23.YANG Guangda.Research on Method of high Accuracy 3DSeismic Exploration at Central Depressions in the South ofSongliao Basin[D].China University of China(Beijing):Schoolof Geophysics and Information Technology,2006:3-23.
[21]Luquot L,Andreani M,Gouze P,et al.CO2-percolationexperiment through chlorite/zeolite-rich sandstone(Pretty HillFormation-Otway Basin-Australia)[J].Chemical geology,2012,294/295:75-88.
[22]Gaus I,Azaroual M,Czernichowski L I.Reactive transportmodelling of the impact of CO2-injection on the clayey cap rockat Sleipner(North Sea)[J].Chemical Geology,2005,217:319-337.
[23]曲希玉,刘立,马瑞,等.CO2流体对岩屑长石砂岩改造作用的实验[J].吉林大学学报:地球科学版,2008,38(6):959-964.QU Xiyu,LIU Li,MA Rui,et al.Experiment on Debris-ArkosicSandstone Reformation by CO2-Fluid[J].Journal of JilinUniversity:Earth Science Edition,2008.38(6):959-964.
[2]Watson M N,Zwingmann N,Lemon N M.The LadbrokeGrove-Katnook carbon dioxide natural laboratory:A recent CO2accumulation in a lithic sandstone reservoir[J].Energy,2004,29:1457-1466.
[3]XU Tianfu,Apps J A,Pruess K.Mineral sequestration of carbondioxide in a sandstone-shale system[J].Chemical Geology,2005,217:295-318.
[4]Lu J M,Wilkinson M,Haszeldine R,et al.Carbonate cements inMiller field of the UK North Sea:A natural analog for mineraltrapping in CO2-geological storage[J].Environmental EarthSciences.2011,62:507-517.
[5]ZHANG Wei,LI Yilian,XU Tianfu,et al.Long-term variationsof CO2-trapped in different mechanisms in deep salineformations:A case study of the Songliao Basin,China[J].International Journal of Greenhouse Gas Control,2009,3:161-180.
[6]Okuyama Y,Sasaki M,Nakanishi S,et al.Geochemical CO2trapping in open aquifer storage-the Tokyo Bay model[J].EnergyProcedia,2009(1):3253-3258.
[7]Credoz A,Bildstein O,Jullien M,et al.Mixed-layerillite-smectite reactivity in acidified solutions:Implications forclayey caprock stability in CO2-geological storage[J].AppliedClay Science,2011,53:402-408.
[8]徐同台,王行信,张有瑜,等.中国含油气盆地黏土矿物[M].北京:石油工业出版社.2003:87121.XU Tongtai,WANG Xingxin,ZHANG Youyu,et al.Claymineral in petroleum basin,China[M].Beijing:PetroleumIndustry Press.2003:87-121.
[9]侯启军,赵志魁,王立武.火山岩气藏:松辽盆地南部大型火山岩气藏勘探理论与实践[M].北京:科学出版社,2009:259-317.HOU Qijun,ZHAO ZHIkui,WANG Liwu.Volcanic gasreservoir:Theory and practice of exploration volcanic rock gasreservoir in south of Songliao Basin[M].Beijing:Science Press,2009:259-317.
[10]熊福生,史謌,孙永梅.松辽盆地两井孤店地区泉头组四段沉积微相研究[J].北京大学学报:自然科学版,2008,44(2):185-192.XIONG Fusheng,SHE Ge,SUN Yongmei,et al,Research onsedimentary Microfacies of Fourth Section of QuantouFormation in Liangjing Gudian Area of Songliao Basin[J].ActaScientiarum Naturalium Universitatis Pekinensis,2008,44(2):185-192.
[11]张庆国,鲍志东,那未红,等.松辽盆地中央坳陷南部下白垩统泉头组四段沉积相[J].古地理学报,2007,9(3):267-276.ZHANG Qingguo,BAO Zhidong,NA Weihong,et al.Sedimentary facies of the member 4-of Quantou Formation oflower cretaceous in Southern Central Depression of SongliaoBasin[J].Journal of Palaeogeography,2007,9(3):267-276.
[12]任战利,萧德铭,迟元林.松辽盆地古地温恢复[J].大庆石油地质与开发,2001,20(1):1314,55.REN Zhanli,XIAO Deming,CHI Yuanlin.Restoration of thePalaeogeotherm in songliao Basin[J].Petroleum Geology andOilfield Development in Daqing,2001,20(1):13-14,55.
[13]张英魁,刘斌,古武,等.利用多元回归方法确定岩石压缩系数[J].油气井测试,2001,10(1/2):79.ZHANG Yingkui,LIU Bin,GU Wu.Determine the rockcompressibility by the multiple regression analysis method[J].Well Testing,2001,10(1/2):7-9.
[14]Allard P.A CO2-rich gas trigger of explosive paroxysms atStromboli basaltic volcano,Italy[J].Journal of Volcanology andGeothermal Research,2010,189(3/4):363-374.
[15]刘立,刘娜,周冰,等.松辽盆地南部红岗背斜幔源-岩浆成因CO2大规模泄露的岩石学记录[J].吉林大学学报:地球科学版,2011,41(2):411420.LIU Li,LIU Na,ZHOU Bing,et al.Petrological Recording ofMantle-Magmatic CO2-Leakage on a Large-Scale in HonggangAnticline,Southern Songliao Basin[J].Journal of JilinUniversity:Earth Science Edition,2011,41(2):411-420.
[16]Felix B,Dirk B,Evelyn K B,et al.Chlorite dissolution in theacid pH-range:A combined microscopic and macroscopicapproach[J].Geochimica et Cosmochimica Acta,2003,67(8):1451-1461.
[17]楼章华,姚炎明,金爱民.松辽盆地地下流体地球化学特征研究[J].矿物学报.2002,22(4):343349.LOU Zhanghua,YAO Yanming,JIN Aimin,et al.Geochemicalproperties of underground fluids in Songliao Basin,China[J].Acta Mineralogica Sinica.2002,22(4):343-349.
[18]闫建萍,刘池阳,马艳萍.成岩作用与油气侵位对松辽盆地齐家—古龙凹陷扶杨油层物性的影响[J].沉积学报,2009,27(2):213-220.YAN Jianping,LIU Chiyang,MA Yanping.Influence ofdiagenesis and hydrocarbon emplacement on the quality of theFuyang Reservoir in Songliao Basin[J].Acta SedimentologicaSinica,2009,27(2):213-220.
[19]LIU Na,LIU Li,QU Xiyu,et al.Genesis of authigene carbonateminerals in the Upper Cretaceous Reservoir,Honggang Anticline,Songliao Basin:A natural analog for mineral trapping of naturalCO2storage[J].Sedimentary Geology,2011,237:166-178.
[20]杨光大.松辽盆地南部中央坳陷区高精度三维地震勘探方法研究[D].中国地质大学(北京):地球物理与信息技术学院,2006:3-23.YANG Guangda.Research on Method of high Accuracy 3DSeismic Exploration at Central Depressions in the South ofSongliao Basin[D].China University of China(Beijing):Schoolof Geophysics and Information Technology,2006:3-23.
[21]Luquot L,Andreani M,Gouze P,et al.CO2-percolationexperiment through chlorite/zeolite-rich sandstone(Pretty HillFormation-Otway Basin-Australia)[J].Chemical geology,2012,294/295:75-88.
[22]Gaus I,Azaroual M,Czernichowski L I.Reactive transportmodelling of the impact of CO2-injection on the clayey cap rockat Sleipner(North Sea)[J].Chemical Geology,2005,217:319-337.
[23]曲希玉,刘立,马瑞,等.CO2流体对岩屑长石砂岩改造作用的实验[J].吉林大学学报:地球科学版,2008,38(6):959-964.QU Xiyu,LIU Li,MA Rui,et al.Experiment on Debris-ArkosicSandstone Reformation by CO2-Fluid[J].Journal of JilinUniversity:Earth Science Edition,2008.38(6):959-964.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |