鄂南三叠系延长组自生成岩矿物成因及期次
|
摘要
为弄清鄂尔多斯盆地南部三叠系延长组关键成岩矿物形成的时间与过程,通过对自生矿物之间的产状及其与其他矿物互生关系的镜下观察,并利用流体包裹体、碳酸盐碳氧同位素记录的成岩流体信息,深入讨论了盆地南部自生成岩矿物成因及期次。研究认为,泥—微晶方解石、菱铁矿和白云石(旬邑地区)为成岩早期沉淀的矿物,其中,菱铁矿的形成时间早于自生绿泥石包膜;泥—微晶方解石沉淀时间与菱铁矿大致同期;旬邑地区白云石胶结物与北部物源区的泥—微晶方解石和菱铁矿胶结物的形成同期;中—晚期亮晶方解石和铁方解石等的形成时间整体早于白云石和铁白云石。石英次生加大边的两个世代分别对应90.0～100.0℃和110.0-120.0℃;自生微晶石英生长的时间略早于或同时于自生绿泥石的形成时间。自生绿泥石包膜主要形成于成岩早期,一般呈两个世代生长,第一世代自生绿泥石形成于20.0～50.0℃,以颗粒绿泥石环边赋存状态为主;第二世代形成于部分机械压实作用以后,只生长于孔隙接触的颗粒表面或第一世代绿泥石形成的微晶石英晶体表面,形成温度约为50.0～70.0℃。研究区延长组自生伊利石的分布较为广泛,其形成具有多源性的特点。
In order to understand the time and process of diagenetic mineral formation in the Triassic Yanchang Formation in the southern Ordos Basin,the occurrence of authigenic minerals and their alternative relationship with other types of minerals are examined.Furthermore,the liquid information of diagenetic minerals is recorded using fluid inclusion and the oxygen isotope data of carbonates.Based on these findings,the genesis and period of authigenic diagenetic minerals in the southern part of the Ordos Basin is discussed in detail.The study shows that mud-microcrystalline calcite,siderite,and dolomite(Xunyi Area)are diagenetic minerals precipitated at the early stages.Among these minerals,siderite is formed earlier than the authigenic chlorite coating,while the mud-microcrystalline calcite is formed at approximately the same time with siderite.The dolomite cement found in the Xunyi Area is formed at the same time with the mud-microcrystal line calcite and siderite found in the north source areas.The mid-late stage sparry calcite and ferroan calcite are both formed earlier than the dolomite and ferroan dolomite.The two generations associated with quartz secondary enlargement corresponds to 90.0～100.0 ℃ and 110.0～120.0 ℃,respectively.The growth period of authigenic microcrystalline quartz is slightly earlier than or the same as the formation time of authigenic chlorite.The authigenic chlorite coating is formed during early diagenesis,which often grows in two generations.The authigenic chlorite in the first generation is formed at 20.0～50.0 ℃ and mainly exists in the form of ring-edge occurrence of chlorite particles.The second generation authigenic chlorite,formed by compaction,is found to only grow on the particle surface in contact with the pore,or the surface of microcrystalline quartz crystals formed from the first-generation chlorite.The formation temperature of the second generation authigenic chlorite is around 50.0～70.0 ℃.The authigenic illite is found to be widely distributed in the Yanchang Formation in the research region.The authigenic illite is formed from multiple sources.
In order to understand the time and process of diagenetic mineral formation in the Triassic Yanchang Formation in the southern Ordos Basin,the occurrence of authigenic minerals and their alternative relationship with other types of minerals are examined.Furthermore,the liquid information of diagenetic minerals is recorded using fluid inclusion and the oxygen isotope data of carbonates.Based on these findings,the genesis and period of authigenic diagenetic minerals in the southern part of the Ordos Basin is discussed in detail.The study shows that mud-microcrystalline calcite,siderite,and dolomite(Xunyi Area)are diagenetic minerals precipitated at the early stages.Among these minerals,siderite is formed earlier than the authigenic chlorite coating,while the mud-microcrystalline calcite is formed at approximately the same time with siderite.The dolomite cement found in the Xunyi Area is formed at the same time with the mud-microcrystal line calcite and siderite found in the north source areas.The mid-late stage sparry calcite and ferroan calcite are both formed earlier than the dolomite and ferroan dolomite.The two generations associated with quartz secondary enlargement corresponds to 90.0～100.0 ℃ and 110.0～120.0 ℃,respectively.The growth period of authigenic microcrystalline quartz is slightly earlier than or the same as the formation time of authigenic chlorite.The authigenic chlorite coating is formed during early diagenesis,which often grows in two generations.The authigenic chlorite in the first generation is formed at 20.0～50.0 ℃ and mainly exists in the form of ring-edge occurrence of chlorite particles.The second generation authigenic chlorite,formed by compaction,is found to only grow on the particle surface in contact with the pore,or the surface of microcrystalline quartz crystals formed from the first-generation chlorite.The formation temperature of the second generation authigenic chlorite is around 50.0～70.0 ℃.The authigenic illite is found to be widely distributed in the Yanchang Formation in the research region.The authigenic illite is formed from multiple sources.
引文
[1]MANSURBEG H,CAJA M A,MARPIL R,et al.Diagenetic evolution and porosity destruction of turbiditic hybrid arenites and siliciclastic sandstones of foreland basins:Evidence from the Eocene Hecho Group,Pyrenees,Spain[J].Journal of Sedimentary Research,2009,79(9):711-735.doi:10.2110/j sr.2009.060
[2]DUTTON S P,LOUCKS R G.Diagenetic controls on evolution of porosity and permeability in lower Tertiary Wilcox sandstones from shallow toultra deep(200~6 700 m)burial,Gulfof Mexico Basin,USA[J].Marineand Petroleum Geology,2010,27:69-81.doi:10.1016/j.-marpetgeo.2009.08.008
[3]徐黎明,牛小兵,梁晓伟,等.华庆地区长6致密油储层微观孔喉结构特征[J].西南石油大学学报(自然科学版),2017,39(4):36-46.doi:10.11885/j.issn.1674-5086.2016.03.28.03XU Liming,NIU Xiaobing,LIANG Xiaowei,et al.Microscopic characteristics of pore-throat structures of the Chang 6 Member tight oil layer in the Huaqing Region[J].Journal of South we st Petroleum University(Science&Technology Edition),2017,39(4):36-46.doi:10.11885/j.-issn.1674-5086.2016.03.28.03
[4]张忠义,陈世加,姚泾利,等.鄂尔多斯盆地长7段致密储层微观特征研究[J].西南石油大学学报(自然科学版),2016,38(6):70-80.doi:10.11885/j.issn.1674-5086.2015.05.01.02ZHANG Zhongyi,CHEN Shijia,YAO Jingli,et al.A study on microscopic pore characteristics of tight reservoir of Chang 7 sedimentation section of Yanchang Formation,Ordos Basin[J].Journal of Southwest Petroleum University(Science&Technology Edition),2016,38(6):70-80.doi:10.11885/j.issn.1674-5086.2015.05.01.02
[5]潘仁芳,李笑天,金吉能,等.渝东南盆缘转换带常压页岩气储层非均质性特征及主控因素[J].天然气工业,2018,38(12):26-36.doi:10.3787/j.issn.1000-0976.2018.12.003PAN Renfang,LI Xiaotian,JIN Jineng,et al.Heterogeneity characteristics and controlling factors of normalpressure shale gas reservoirs in the basin-margin transition zone of SE Chongqing[J].Natural Gas Industry,2018,38(12):26-36.doi:10.3787/j.issn.1000-0976.2018.12.-003
[6]韩京,陈波,赵幸滨,等.下扬子地区二叠系页岩有机质孔隙发育特征及其影响因素[J].天然气工业,2017,37(10):17-26.doi:10.3787/j.issn.1000-0976.2017.10.-003HAN Jing,CHEN Bo,ZHAO Xingbin,et al.Development characteristics and influential factors of organic pores in the Permian shale in the Lower Yangtze Region[J].Natural Gas Industry,2017,37(10):17-26.doi:10.3787/j.issn.-1000-0976.2017.10.003
[7]闫林,冉启全,高阳,等.陆相致密油藏差异化含油特征与控制因素[J].西南石油大学学报(自然科学版),2017,39(6):45-54.doi:10.11885j.issn.1674-5086.2016.06.21.04YAN Lin,RAN Qiquan,GAO Yang,et al.The differentitation oil-beanring characteristic and control factors ofcontinental tight oil[J].Journal of Southwest Petroleum University(Science and Technology Edition),2017,39(6)45-54.doi:10.11885/j.issn.1674-5086.2016.06.21.04
[8]姚泾利,王琪,张瑞,等.鄂尔多斯盆地中部延长组砂岩中碳酸盐胶结物成因与分布规律研究[J].天然气地球科学,2011,22(6):943-950.doi:10.11764/j.issn.1672-1926.2011.06.943YAO Jingli,WANG Qi,ZHANG Rui,et al.Origin and spatial distribution of carbonate cements in Yanchang Fm(Triassic)sandstones within the lacustrine center of Ordos Basin,NW China[J].Natural Gas Geoscience,201122(6):943-950.doi:10.11764/j.issn.1672-1926.2011.06.-943
[9]罗春艳.鄂尔多斯盆地中部长8低孔低渗储层成岩作用与成岩烃类充注过程研究[D].西安:西北大学,2015.LUO Chunyan.Research on diagenesis and diagenetichydrocarbon filling process of Chang 8 group in the central Ordos Basin[D].Xi'an:Northwe st University,2015.
[10]刘怀波,吴智勇.俄克拉荷马州南哈桑气田斯普罗砂岩的成岩作用和孔隙演化[J].江汉石油学院学报,1995,17(2):1-9.LIU Huaibo,WU Zhiyong.Diagenesis and porosity evolution of the spiro sandstone in south Hartshorne Gas Field of Oklahoma,USA[J].Journal of Jianghan Petroleum institute,1995,17(2):1-9.
[11]AMTHOR J E,OKKERMAN J.Influence of early diagenesis on reservoir quality of Rotliegende sandstones northern Netherlands[J].American Association of Petroleum Geologists Bulletin,1998,82(12):2246-2265.doi10.1306/00AA7F04-1730-11D7-8645000102C1865D
[12]TAYLOR J,IACONO W G,McGue M.Evidence for a geneticetiology of early-onset delinquency[J].Journal of Abnormal Psychology,2000,109(4):634-643.doi:10.1037/0021-843X.109.4.634
[13]黄思静,石和,张萌,等.锶同位素地层学在碎屑岩成岩研究中的应用[J].沉积学报,2002,20(3):359-366doi:10.3969/j.issn.1000-0550.2002.03.001HUANG Sijing,SHI He,ZHANG Meng,et al.Application of Strontium Isotope Strtigraphy to diagenesis research[J].Acta Sedimentologica Sinica,2002,20(3):359-366doi:10.3969/j.issn.1000-0550.2002.03.001
[14]孙致学,孙治雷,鲁洪江,等.砂岩储集层中碳酸盐胶结物特征——以鄂尔多斯盆地中南部延长组为例[J].石油勘探与开发,2010,37(5):543-551.SUN Zhixue,SUN Zhilei,LU Hongjiang,et al.Characteristics of carbonate cements in sandstone reservoirs:Acase from Yangchang Formation,middle and southern Ordos Basin,China[J].Petroleum Exploration and Develop ment,2010,37(5):543-551.
[15]钟金银,何苗,周韬,等.鄂尔多斯盆地东南缘长8油层组碳酸盐胶结物成因分析[J].岩性油气藏,2011,23(4):65-69.doi:10.3969/j.issn.1673-8926.2011.04.012ZHONG Jinyin,HE Miao,ZHOU Tao,et al.Origin analy sis of carbonate in Chang 8 reservoir in southeastern margin of Ordos Basin[J].Lithologic Reservoirs,2011,23(4):65-69.doi:10.3969/j.issn.1673-8926.2011.04.012
[16]田亚铭,施泽进,李庭艳,等.姬塬地区长8油层组碳酸盐胶结物特征与成因[J].西安石油大学学报(自然科学版),2011,26(3):26-31.doi:10.3969/j.issn.1673064X.2011.03.005TIAN Yaming,SHI Zejin,LI Tingyan,et al.Characteris tics and origin of the carbonate cements of Chang 8 Mem ber in Jiyuan Area,Ordos Basin[J].Journal of Xi'an Shi you University(Natural Science),2011,26(3):26-31.doi10.3969/j.issn.1673-064X.2011.03.005
[17]MCBRIDE.Social research:An international quarterly[J].1989,56(4):849-875.
[18]WORDEN R H,FRENCH M W,MARLANL E.Amorphous silica Nano films result in growth of misorlented mi crocrystalline quartz maintaining poro sity in deeply burled sandstones[J].Geology,2012,40(2):179-182.doi:10.1130/G32661.1
[19]EHRENBERG S N,AAGAARD P,WILSON M J,et al.Depth-dependent transformation oof kaolinite to dickite i sandstones of the Orwegian continental shelf[J].Clay Min erals,1993,28(3):325-352.doi:10.1180/claymin.1993.028.3.01
[20]GRIGSBY J D.Origin and growth mechanism of authi genic chlorite in sandstones of the lower Vicksburg Formation,South Tesas[J].Journal of Sedimentary Research,2001,71(1):27-36.doi:10.1306/060100710027
[21]DOWEY P J,HODGSON D M,WORDEN R H.Pre re qulsites,processes,and prediction of chlorite grain coatings in petroleum reservoirs:A review of sub-surface examples[J].Marine and Petroleum Geology,2012,32:63-75.doi:10.1016/j.marpetgeo.2011.11.007
[22]BAUER A,VELDE B,GAUPP R.Experi mental con straints onillite crystal morphology[J].Clay Minerals2000,35(3):587-597.doi:10.1180/000985500546909
[23]STORVOLL V,BJORLYKKE K,KARLSEN D,et al.Porosity preservation inreservoir sandstones due to Graincoating illite:A study of the Jurassic Garn Formation fromthe Kristin and Lavrans fields,offshore Mid-Norway[J].Marine and Petroleum Geology,2002,19(6):767-781.doi:10.1016/S0264-8172(02)00035-1
[24]LANDER R H,BONNELL L M.A model for fibrous illite nucleationand growth in sandstones[J].American Association of Petroleum Geologists Bulletin,2010,94(8):1161-1187.doi:10.1306/042 1 1009121
[25]FRANKS,STEPHEN G,ZWINGMANN H.Origin and timing of late diagenetic illite in the permiancarboniferous unayzah sandstone reservoirs of Saudi Arabia[J].American Association of Petroleum Geologists Bulletin,2010(94(8):1133-1159.doi:10.1306/04211009142
[26]CLAUER N, LIEWIG N, ZWINGMANN H.Timeconstrained illitization in gas-bearing Rotliegende(Permian)sandstones from northern Germany by illite potassiumargon dating[J].American Association of Petroleum Geologists Bulletin,2012,96(3):519-543.doi:10.1306/07131111003
[27]STROKER T M,HARRIS N B,ELLIOTT W,et al.Diagenesis of a tight gas sand reservoir:Upper Cretaceous Mesaverde Group,Piceance Basin,Colorado[J].Marine and Petroleum Geology,2013,40(1):48-68.doi:10.-1016./j.marpetgeo.2012.08.003
[28]黄思静,黄可可,冯文立,等.成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成——来自鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J].地球化学,2009,38(5):498-506.doi:10.3321/j.issn:0379-1726.2009.05.009HUANG Sijing,HUANG Keke,FENG Wenli,et al.Mass exchanges among feldspar,kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis:A case study on the Upper Paleozoic,Ordos Basin and Xujiahe Formation,Western Sichuan Depression[J],Geoclimica,2009,38(5):498-506.doi:10.3321/j.issn:-0379-1726.2009.05.009
[2]DUTTON S P,LOUCKS R G.Diagenetic controls on evolution of porosity and permeability in lower Tertiary Wilcox sandstones from shallow toultra deep(200~6 700 m)burial,Gulfof Mexico Basin,USA[J].Marineand Petroleum Geology,2010,27:69-81.doi:10.1016/j.-marpetgeo.2009.08.008
[3]徐黎明,牛小兵,梁晓伟,等.华庆地区长6致密油储层微观孔喉结构特征[J].西南石油大学学报(自然科学版),2017,39(4):36-46.doi:10.11885/j.issn.1674-5086.2016.03.28.03XU Liming,NIU Xiaobing,LIANG Xiaowei,et al.Microscopic characteristics of pore-throat structures of the Chang 6 Member tight oil layer in the Huaqing Region[J].Journal of South we st Petroleum University(Science&Technology Edition),2017,39(4):36-46.doi:10.11885/j.-issn.1674-5086.2016.03.28.03
[4]张忠义,陈世加,姚泾利,等.鄂尔多斯盆地长7段致密储层微观特征研究[J].西南石油大学学报(自然科学版),2016,38(6):70-80.doi:10.11885/j.issn.1674-5086.2015.05.01.02ZHANG Zhongyi,CHEN Shijia,YAO Jingli,et al.A study on microscopic pore characteristics of tight reservoir of Chang 7 sedimentation section of Yanchang Formation,Ordos Basin[J].Journal of Southwest Petroleum University(Science&Technology Edition),2016,38(6):70-80.doi:10.11885/j.issn.1674-5086.2015.05.01.02
[5]潘仁芳,李笑天,金吉能,等.渝东南盆缘转换带常压页岩气储层非均质性特征及主控因素[J].天然气工业,2018,38(12):26-36.doi:10.3787/j.issn.1000-0976.2018.12.003PAN Renfang,LI Xiaotian,JIN Jineng,et al.Heterogeneity characteristics and controlling factors of normalpressure shale gas reservoirs in the basin-margin transition zone of SE Chongqing[J].Natural Gas Industry,2018,38(12):26-36.doi:10.3787/j.issn.1000-0976.2018.12.-003
[6]韩京,陈波,赵幸滨,等.下扬子地区二叠系页岩有机质孔隙发育特征及其影响因素[J].天然气工业,2017,37(10):17-26.doi:10.3787/j.issn.1000-0976.2017.10.-003HAN Jing,CHEN Bo,ZHAO Xingbin,et al.Development characteristics and influential factors of organic pores in the Permian shale in the Lower Yangtze Region[J].Natural Gas Industry,2017,37(10):17-26.doi:10.3787/j.issn.-1000-0976.2017.10.003
[7]闫林,冉启全,高阳,等.陆相致密油藏差异化含油特征与控制因素[J].西南石油大学学报(自然科学版),2017,39(6):45-54.doi:10.11885j.issn.1674-5086.2016.06.21.04YAN Lin,RAN Qiquan,GAO Yang,et al.The differentitation oil-beanring characteristic and control factors ofcontinental tight oil[J].Journal of Southwest Petroleum University(Science and Technology Edition),2017,39(6)45-54.doi:10.11885/j.issn.1674-5086.2016.06.21.04
[8]姚泾利,王琪,张瑞,等.鄂尔多斯盆地中部延长组砂岩中碳酸盐胶结物成因与分布规律研究[J].天然气地球科学,2011,22(6):943-950.doi:10.11764/j.issn.1672-1926.2011.06.943YAO Jingli,WANG Qi,ZHANG Rui,et al.Origin and spatial distribution of carbonate cements in Yanchang Fm(Triassic)sandstones within the lacustrine center of Ordos Basin,NW China[J].Natural Gas Geoscience,201122(6):943-950.doi:10.11764/j.issn.1672-1926.2011.06.-943
[9]罗春艳.鄂尔多斯盆地中部长8低孔低渗储层成岩作用与成岩烃类充注过程研究[D].西安:西北大学,2015.LUO Chunyan.Research on diagenesis and diagenetichydrocarbon filling process of Chang 8 group in the central Ordos Basin[D].Xi'an:Northwe st University,2015.
[10]刘怀波,吴智勇.俄克拉荷马州南哈桑气田斯普罗砂岩的成岩作用和孔隙演化[J].江汉石油学院学报,1995,17(2):1-9.LIU Huaibo,WU Zhiyong.Diagenesis and porosity evolution of the spiro sandstone in south Hartshorne Gas Field of Oklahoma,USA[J].Journal of Jianghan Petroleum institute,1995,17(2):1-9.
[11]AMTHOR J E,OKKERMAN J.Influence of early diagenesis on reservoir quality of Rotliegende sandstones northern Netherlands[J].American Association of Petroleum Geologists Bulletin,1998,82(12):2246-2265.doi10.1306/00AA7F04-1730-11D7-8645000102C1865D
[12]TAYLOR J,IACONO W G,McGue M.Evidence for a geneticetiology of early-onset delinquency[J].Journal of Abnormal Psychology,2000,109(4):634-643.doi:10.1037/0021-843X.109.4.634
[13]黄思静,石和,张萌,等.锶同位素地层学在碎屑岩成岩研究中的应用[J].沉积学报,2002,20(3):359-366doi:10.3969/j.issn.1000-0550.2002.03.001HUANG Sijing,SHI He,ZHANG Meng,et al.Application of Strontium Isotope Strtigraphy to diagenesis research[J].Acta Sedimentologica Sinica,2002,20(3):359-366doi:10.3969/j.issn.1000-0550.2002.03.001
[14]孙致学,孙治雷,鲁洪江,等.砂岩储集层中碳酸盐胶结物特征——以鄂尔多斯盆地中南部延长组为例[J].石油勘探与开发,2010,37(5):543-551.SUN Zhixue,SUN Zhilei,LU Hongjiang,et al.Characteristics of carbonate cements in sandstone reservoirs:Acase from Yangchang Formation,middle and southern Ordos Basin,China[J].Petroleum Exploration and Develop ment,2010,37(5):543-551.
[15]钟金银,何苗,周韬,等.鄂尔多斯盆地东南缘长8油层组碳酸盐胶结物成因分析[J].岩性油气藏,2011,23(4):65-69.doi:10.3969/j.issn.1673-8926.2011.04.012ZHONG Jinyin,HE Miao,ZHOU Tao,et al.Origin analy sis of carbonate in Chang 8 reservoir in southeastern margin of Ordos Basin[J].Lithologic Reservoirs,2011,23(4):65-69.doi:10.3969/j.issn.1673-8926.2011.04.012
[16]田亚铭,施泽进,李庭艳,等.姬塬地区长8油层组碳酸盐胶结物特征与成因[J].西安石油大学学报(自然科学版),2011,26(3):26-31.doi:10.3969/j.issn.1673064X.2011.03.005TIAN Yaming,SHI Zejin,LI Tingyan,et al.Characteris tics and origin of the carbonate cements of Chang 8 Mem ber in Jiyuan Area,Ordos Basin[J].Journal of Xi'an Shi you University(Natural Science),2011,26(3):26-31.doi10.3969/j.issn.1673-064X.2011.03.005
[17]MCBRIDE.Social research:An international quarterly[J].1989,56(4):849-875.
[18]WORDEN R H,FRENCH M W,MARLANL E.Amorphous silica Nano films result in growth of misorlented mi crocrystalline quartz maintaining poro sity in deeply burled sandstones[J].Geology,2012,40(2):179-182.doi:10.1130/G32661.1
[19]EHRENBERG S N,AAGAARD P,WILSON M J,et al.Depth-dependent transformation oof kaolinite to dickite i sandstones of the Orwegian continental shelf[J].Clay Min erals,1993,28(3):325-352.doi:10.1180/claymin.1993.028.3.01
[20]GRIGSBY J D.Origin and growth mechanism of authi genic chlorite in sandstones of the lower Vicksburg Formation,South Tesas[J].Journal of Sedimentary Research,2001,71(1):27-36.doi:10.1306/060100710027
[21]DOWEY P J,HODGSON D M,WORDEN R H.Pre re qulsites,processes,and prediction of chlorite grain coatings in petroleum reservoirs:A review of sub-surface examples[J].Marine and Petroleum Geology,2012,32:63-75.doi:10.1016/j.marpetgeo.2011.11.007
[22]BAUER A,VELDE B,GAUPP R.Experi mental con straints onillite crystal morphology[J].Clay Minerals2000,35(3):587-597.doi:10.1180/000985500546909
[23]STORVOLL V,BJORLYKKE K,KARLSEN D,et al.Porosity preservation inreservoir sandstones due to Graincoating illite:A study of the Jurassic Garn Formation fromthe Kristin and Lavrans fields,offshore Mid-Norway[J].Marine and Petroleum Geology,2002,19(6):767-781.doi:10.1016/S0264-8172(02)00035-1
[24]LANDER R H,BONNELL L M.A model for fibrous illite nucleationand growth in sandstones[J].American Association of Petroleum Geologists Bulletin,2010,94(8):1161-1187.doi:10.1306/042 1 1009121
[25]FRANKS,STEPHEN G,ZWINGMANN H.Origin and timing of late diagenetic illite in the permiancarboniferous unayzah sandstone reservoirs of Saudi Arabia[J].American Association of Petroleum Geologists Bulletin,2010(94(8):1133-1159.doi:10.1306/04211009142
[26]CLAUER N, LIEWIG N, ZWINGMANN H.Timeconstrained illitization in gas-bearing Rotliegende(Permian)sandstones from northern Germany by illite potassiumargon dating[J].American Association of Petroleum Geologists Bulletin,2012,96(3):519-543.doi:10.1306/07131111003
[27]STROKER T M,HARRIS N B,ELLIOTT W,et al.Diagenesis of a tight gas sand reservoir:Upper Cretaceous Mesaverde Group,Piceance Basin,Colorado[J].Marine and Petroleum Geology,2013,40(1):48-68.doi:10.-1016./j.marpetgeo.2012.08.003
[28]黄思静,黄可可,冯文立,等.成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成——来自鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究[J].地球化学,2009,38(5):498-506.doi:10.3321/j.issn:0379-1726.2009.05.009HUANG Sijing,HUANG Keke,FENG Wenli,et al.Mass exchanges among feldspar,kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis:A case study on the Upper Paleozoic,Ordos Basin and Xujiahe Formation,Western Sichuan Depression[J],Geoclimica,2009,38(5):498-506.doi:10.3321/j.issn:-0379-1726.2009.05.009