混合沉积研究现状及其与油气富集的关系
|
摘要
混合沉积广泛发育于海洋与湖泊沉积环境中,通过对混合沉积的成因机理、组合类型、沉积模式与层序地层、控制因素、储集层发育与油气聚集等方面的系统分析,阐述了混合沉积研究的现状及其与油气富集的关系。结合大量资料,对准噶尔盆地吉木萨尔凹陷二叠系芦草沟组混合沉积的成因机理、形成条件与控制因素、沉积模式及油气富集关系等方面进行了阐述。混合沉积受构造背景、沉积环境、物源、海(湖)平面变化、构造升降、水动力与气候变化等多种因素的控制,但碳酸盐是其形成的基本条件。已有的关于混合沉积的研究成果具有明显的区域性,缺乏对各种不同沉积环境的混合沉积的岩性及其组合类型、控制因素的差异性对比分析,以后应加强混合沉积与沉积体系、层序地层之间的关系及其反映的古地理、古沉积环境、古物源条件等信息的研究。混合沉积与油气富集的关系极为密切,由于其不同岩性既不同程度地含原始有机质,又发育多种类型的孔隙,所以,其有机质富集特征与不同孔隙类型发育之间有内在成因关系,是今后进行油气地质研究的重要内容,对非常规油气的富集有重要意义。
The mixed sediments are widely developed in marine and lacustrine sedimentary environments.This paper overviews the research status and its relationship with oil and gas enrichment based on the systematic analysis of the genesis mechanism,type of assemblage,sedimentary model and sequence stratigraphy,controlling factors,reservoir development and hydrocarbon accumulation in mixed sediments.Based on a large amount of data,the paper describes the genetic mechanism,formation conditions,controlling factors,sedimentary model and the relationship between oil and gas accumulation in the Permian Lucaogou Formation in the Jimsar Sag,Junggar Basin.The mixed deposition is controlled by many factors such as tectonic setting,sedimentary environment,provenance,sea/lake level change,tectonic movements,hydrodynamic and climate change,but carbonate is the basic condition for its formation.The existing research results about the mixed sediments are obviously regional with no comparative analysis on the lithology,mixed types and control factors of mixed deposition in different sedimentary environments.Future research should focus on the mixed sedimentary and sedimentary systems,the relationship between sequence stratigraphy and its reflections on paleogeography,paleo-sediment environment and antiquities.The relationship between mixed sedimentation and hydrocarbon enrichment is very close,and because of their different lithologies,they contain not only the original organic matter,but also a variety of types of pores.Therefore,there is an inherent genetic relationship between the organic matter enrichment characteristics and the development of different pore types,which is an important part of oil and gas geology research in the future and is of great significance to the enrichment of unconventional oil and gas.
The mixed sediments are widely developed in marine and lacustrine sedimentary environments.This paper overviews the research status and its relationship with oil and gas enrichment based on the systematic analysis of the genesis mechanism,type of assemblage,sedimentary model and sequence stratigraphy,controlling factors,reservoir development and hydrocarbon accumulation in mixed sediments.Based on a large amount of data,the paper describes the genetic mechanism,formation conditions,controlling factors,sedimentary model and the relationship between oil and gas accumulation in the Permian Lucaogou Formation in the Jimsar Sag,Junggar Basin.The mixed deposition is controlled by many factors such as tectonic setting,sedimentary environment,provenance,sea/lake level change,tectonic movements,hydrodynamic and climate change,but carbonate is the basic condition for its formation.The existing research results about the mixed sediments are obviously regional with no comparative analysis on the lithology,mixed types and control factors of mixed deposition in different sedimentary environments.Future research should focus on the mixed sedimentary and sedimentary systems,the relationship between sequence stratigraphy and its reflections on paleogeography,paleo-sediment environment and antiquities.The relationship between mixed sedimentation and hydrocarbon enrichment is very close,and because of their different lithologies,they contain not only the original organic matter,but also a variety of types of pores.Therefore,there is an inherent genetic relationship between the organic matter enrichment characteristics and the development of different pore types,which is an important part of oil and gas geology research in the future and is of great significance to the enrichment of unconventional oil and gas.
引文
[1] Mount J F.Mixing of silicilastics and carbonate sediments in shallow shelf environments[J].Geology,1984,12(7):432-435.
[2]郭福生.浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义[J].沉积学报,2004,22(1):136-141.
[3]董桂玉,陈洪德,何幼斌,等.陆源碎屑与碳酸盐混合沉积研究中的几点思考[J].地球科学进展,2007,22(9):931-940.
[4]杨朝青,沙庆安.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积[J].沉积学报,1990,8(2):59-66.
[5] Tirsga A H.Cyclic sedimentation of carbonate and siliciclastic deposits on a Late Precambrian ramp:The Elisabeth Bjerg Formation(Eleonore Bay Supergroup)East Greenland[J].Journal of Sedimentary Research,1996,66(4):699-712.
[6]沙庆安.混合沉积和混积岩的讨论[J].古地理学报,2001,3(3):63-66.
[7] Brooks G R,Doyle L J,Suthard B C,et al.Facies architecture of the mixed carbonate/siliciclastic inner continental shelf of west-central Florida:Implications for Holocene barrier development[J].Marine Geology,2003,200(1/4):325-349.
[8] Garcia-Hidalgo J F,Gil J,Segura M,et al.Internal anatomy of a mixed siliciclastic-carbonate platform:The Late CenomanianMid Turonian at the southern margin of the Spanish Central System[J].Sedimentology,2007,54(6):1245-1271.
[9]廖群山,胡华,林建平,等.四川盆地川中侏罗系致密储层石油勘探前景[J].石油与天然气地质,2011,32(54):815-822.
[10]赵贤正,姜在兴,张锐锋,等.陆相断陷盆地特殊岩性致密油藏地质特征与勘探实践:以束鹿凹陷沙河街组致密油藏为例[J].石油学报,2015,36(增刊1):1-9.
[11]查明,苏阳,高长海,等.致密储层储集空间特征及影响因素:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].中国矿业大学学报,2017,46(1):85-95.
[12]Bruckner W D.Cyclic calcareous sedimentation as an index of climatic variation in the past[J].Journal of Sedimentary Petrology,1953,23(4):235-237.
[13]Carozzi A.Some remarks on cyclic calcareous sedimentation as an index of climatic variations[J].Journal of Sedimentary Petrology,1955,25(1):78-79.
[14]Maxwell W G,Swinchatt J P.Great barrier reef:Regional variation in a Terrigenous-Carbonate province[J].Geological Society of American Bulletin,1970,81(3):691-724.
[15]Butto N A,Vos R G.Subtidal and intertidal clastic and carbonate sedimentation in amacrotidal environment:An example from the Lower Proterozoic of South Africa[J].Sedimentary Geology,1977,18(1/3):175-200.
[16]Price I.Deposition and derivation of clastic carbonate on a Mesozoic continental margin,Orthis,Greece[J].Sedimentology,1977,24(4):529-546.
[17]Markello J R,Read J F.Carbonate ramp-to-deeper shale shelf transitions of an Upper Cambrian intrashelf basin:Nolichucky Formation,southwest Virginia,Appalachians[J].Sedimentology,1981,28(4):573-597.
[18]Tucker M.Storm-surge sandstones and the deposition of interbedded limestone:Late Precambrian,southern Norway[M]∥Einsele G,Seilacher A.Cyclic and event stratification.Berlin:Springer-Verlag,1982:363-370.
[19]刘宝珺,余光明,王成善,等.珠穆朗玛峰地区侏罗纪沉积环境[J].沉积学报,1983,1(2):1-16.
[20]Cawthope R I.Sedimentation during carbonate ramp-to-slope evolution in a technically active area:Bavland basin(Dinantian),Norlhern England[J].Sedimentology,2010,33(2):185-206.
[21]Roberts H H.Modern caibonate-siliciclastic transitions:Humid and arid tropical examples[J].Sedimentary Geology,1987,50(1/3):25-65.
[22]Dolyle L J,Roberts H H.Carbonate-clastic transitions[M].New York:Elsevier,1988:142.
[23]Dolan J F.Eustatic and tectonic controls on deposition of hybrid siliciclastic/carbonate basinal cycles:Discussion with examples[J].AAPG Bulletin,1989,73(10):1233-1246.
[24]Yose L A,Heller P L.Sea level controls of mixed carbonate-siliciclastic gravity flow deposition,lower part of the Keeler Canyon Formation(Pennsylvanian),Southeastern California[J].Geological Society of America Bulletin,1989,101(3):422-439.
[25]Lomando A I,Harris P M.Mixed carbonate-siliciclastic sequences[M].[S.l.]:SEPM(Society for Sedimentary Geology),1991:568.
[26]张廷山,兰光志,陈晓慧.川西北早志留世陆缘碎屑-碳酸盐混积缓坡[J].沉积学报,1995,13(4):27-35.
[27]张雄华.混积岩的分类和成因[J].地质科技情报,2000,19(4):31-34.
[28]Lubesedera S,Redferna J,Boutibb L.Mixed siliciclastic carbonate shelf sedimentation Lower Devonian sequences of the SW Anti-Atlas,Morocco[J].Sedimentary Geology,2008,215(1/4):13-32.
[29]宋章强,陈延芳,杜晓峰,等.渤海海域A构造区沙二段混合沉积特征及储层研究[J].海洋石油,2013,33(4):13-18.
[30]Toshifumi K,Hajime N,Yasunari S,et al.Lower Triassic mixed carbonate and siliciclastic setting with Smithian-Spathian anoxic to dysoxic facies,A Chau Basin,northeastern Vietnam[J].Sedimentary Geology,2014,300:28-48.
[31]马艳萍,刘立.大港滩海区第三系湖相混积岩的成因与成岩作用特征[J].沉积学报,2003,21(4):607-613.
[32]Halfar J,Lngle J C.Modern non-tropical mixed carbonate-siliciclastic sediments and environments of the southwestern Gulf of California,Mexico[J].Sedimentary Geology,2004,165(1/2):93-115.
[33]Alex C B,Valeria S Q,Mariana B M,et al.Shelf morphology as an indicator of sedimentary,regimes:A synthesis from a mixed siliciclastic-carbonate shelf on the eastern Brazilian margin[J].Journal of South American Earth Sciences,2015,63:125-136.
[34]冯增昭.中国沉积学[M].北京:石油工业出版社,1994:623-631.
[35]Garcia-Mondejar J,Fernández-Mediola P A.Sequence stratigraphy and systems tracts of a mixed carbonate and siliciclastic platform-basin setting:the Albian of Lunada and Soba,northern Spain[J].AAPG Bulletin,1993,77(2):245-275.
[36]Steven G,Driese R H,Dott J.Model for sandstone-carbonate“cyclothems”based on upper member of Morgan Formation(Middle Pennsylvanian)of Northern Utah and Colorado[J].AAPG Bulletin,1984,68(5):574-597.
[37]Bechstǎdt T,Schweizer T.The carbonate-clastic cycles of the East-Alpine Raibl Group:Result of third-order sea-level fluctuations in the Carnian[J].Sedimentary Geology,1991,70(2/4):241-270.
[38]蔡进功,李从先.内蒙西南部石炭系碎屑岩-碳酸盐岩混合沉积特征[J].石油与天然气地质,1994,15(1):80-87.
[39]李祥辉.层序地层中的混合沉积作用及其控制因素[J].高校地质学报,2008,14(3):395-404.
[40]冯进来,胡凯,曹剑,等.陆源碎屑与碳酸盐混积岩及其油气地质意义[J].高校地质学报,2011,17(2):297-307.
[41]Davies H R.Shelf sandstones in the Mowry Shale:Evidence for deposition during Cretaceous sea level falls[J].Journal of Sedimentary Research,1989,59(4):548-560.
[42]王国忠.南海北部大陆架现代礁源碳酸盐与陆源碎屑的混合沉积作用[J].古地理学报,2001,3(2):47-54.
[43]Coffey B P,Read J F.Mixed carbonate-siliciclastic sequence stratigraphy of a Paleogene transition zone continental shelf,southeastern USA[J].Sedimentary Geology,2004,166(1/2):21-57.
[44]司马立强,杨毅,吴丰,等.柴西北小梁山地区狮子沟组混积岩储层评价[J].现代地质,2005,28(1):173-180.
[45]张金亮,司学强.断陷湖盆碳酸盐与陆源碎屑混合沉积:以东营凹陷金家地区古近系沙河街组第四段上亚段为例[J].地质论评,2007,53(4):448-454.
[46]张娣,侯中健,王亚辉,等.板桥-北大港地区沙河街组沙一段湖相碳酸盐岩沉积特征[J].岩性油气藏,2008,20(4):92-97.
[47]孙娇鹏,陈世悦,胡忠亚,等.柴东北缘古生代碎屑岩-碳酸盐岩混积相发育特征及组合模式研究[J].天然气地球科学,2014,25(10):1586-1694.
[48]Campbell A E.Shelf-geometry response to changesin relative sea level on a mixed carbonate-siliciclastic shelf in the Guyana Basin[J].Sedimentary Geology,2005,175(1/4):259-275.
[49]Garcia-Garcia F,Soria J M,Viseras C,et al.High-frequency rhythmicity in a mixed siliciclastic-carbonate shelf(Late Miocene,Guadix basin,Spain):A model of interplay between climatic oscillations,subsidence,and sediment dispersal[J].Journal of Sedimentary Research,2009,79(5/6):302-315.
[50]Miller R P,Hiller P L.Depositional framework and controls on mixed carbonate-siliciclastic gravity flows:Pennsylvanian-Permian shelf to basin transect,south-western Great Basin,USA[J].Sedimentology,1994,41(1):1-20.
[51]李祥辉,曾允孚.扬子西缘泥盆纪碳酸盐与陆源碎屑的混合沉积层序和层序混合沉积模式[J].沉积学报,1999,17(3):339-344.
[52]El-Azabi M H,El-Araby A.Depositional framework and sequence stratigraphic aspects of the Coniacian-Santonian mixed siliciclastic/carbonate Matulla sediments in Nezzazat and Ekma blocks,Gulf of Suez,Egypt[J].Journal of African Earth Sciences,2007,47(4/5):179-202.
[53]Korngreen D,Bialik O M.The characteristics of carbonate system recovery during a relatively dry event in a mixed carbonate/siliciclastic environment in the Pelsonian(Middle Triassic)proximal marginal marine basins:A case study from the tropical Tethyan northwest Gondwana margins[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2015,440:793-812.
[54]Hersi O S,Abbasib I A,Al-Harthy A.Sedimentology,rhythmicity and basin-fill architecture of a carbonate ramp depositional system with intermittent terrigenous influx:The Albian Kharfot Formation of the Jeza-Qamar Basin,Dhofar,Southern Oman[J].Sedimentary Geology,2016,331:114-131.
[55]Zahra S,Annette D G,Maurice E T.Sequence development of a latest Devonian-Tournaisian distally-steepened mixed carbonate-siliciclastic ramp,Canning Basin,Australia[J].Sedimentary Geology,2016,333:164-183.
[56]张少敏,操应长,朱如凯,等.湖相细粒混合沉积岩岩石类型划分:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].地学前缘,2018,25(4):198-209.
[57]张亚奇,马世忠,高阳,等.吉木萨尔凹陷芦草沟组致密油储层沉积相分析[J].沉积学报,2017,35(2):358-370.
[58]马克,侯加根,刘钰铭,等.吉木萨尔凹陷二叠系芦草沟组咸化湖混合沉积模式[J].石油学报,2017,38(6):636-648.
[59]邵雨,杨勇强,万敏,等.吉木萨尔凹陷二叠系芦草沟组沉积特征及沉积相演化[J].新疆石油地质,2015,36(6):635-641.
[60]张锦泉,叶红专.论碳酸盐与陆源碎屑的混合沉积[J].成都地质学院学报,1989,16(2):87-92.
[61]Dorsey R J,Kidwell S M.Mixed carbonate-siliciclastic sedimentation on a tectonically active margin:Example from the Pliocene Baja California Sur,Mexico[J].Geology,1999,27(10):935-938.
[62]Harrowfield M,Keep M.Tectonic modification of the Australian North-West Shelf:Episodic rejuvenation of long-lived basin divisions[J].Basin Research,2005,17(2):225-239.
[63]陈怀龙,王兆峰,汪文,等.阿富汗喀什喀里油田下白垩统阿普第阶地层混合沉积特征研究[J].石油天然气学报,2013,35(11):11-15.
[64]赵灿,李旭兵,郇金来,等.碳酸盐与硅质碎屑的混合沉积机理和控制因素探讨[J].地质论评,2013,59(4):615-626.
[65]江茂生,沙庆安.碳酸盐与陆源碎屑的混合沉积体系研究进展[J].地球科学进展,1995,10(6):551-554.
[66]匡立春,唐勇,雷德文,等.准噶尔盆地二叠系咸化湖相云质岩致密油形成条件与勘探潜力[J].石油勘探与开发,2012,39(6):657-668.
[67]孟元林,祝恒东,李新宁.白云岩溶蚀的热力学分析与次生孔隙带预测:以三塘湖盆地二叠系芦草沟组二段致密凝灰质白云岩为例[J].石油勘探与开发,2014,41(6):690-696.
[68]李婷婷,朱如凯,白斌,等.混积岩储层特征:以酒泉盆地青西凹陷下白垩统混积岩为例[J].沉积学报,2015,33(2):376-384.
[69]高岗,向宝力,王轩,等.准噶尔盆地吉木萨尔凹陷芦草沟组湖相混合沉积中缝合线发育与有机质富集研究[J].天然气地球科学,2016,27(11):1963-1969.
[70]Poeppelreiter M,Aigner T.Unconventional pattern of reservoir facies distribution in epeiric successions:Lessons from an outcrop analogy(Lower Keuper,Germany)[J].AAPG Bulletin,2003,87(1):39-70.
[71]Palermol D,Aignerl T,Geluk M.Reservoir potential of a lacustrine mixed carbonate/siliciclastic gas reservoir the lower Triassic Rogenstein in the Netherlands[J].Journal of Petroleum Geology,2008,31(1):61-96.
[72]李新宁,马强,梁辉,等.三塘湖盆地二叠系芦草沟组二段混积岩致密油地质特征及勘探潜力[J].石油勘探与开发,2015,42(6):763-772.
[73]闫伟鹏,杨涛,李欣,等.中国陆上湖相碳酸盐岩地质特征及勘探潜力[J].中国石油勘探,2014,19(4):11-17.
[74]张新顺,王红军,马锋,等.致密油资源富集区与“甜点区”分布关系研究:以美国威利斯顿盆地为例[J].石油实验地质,2015,37(5):619-626.
[75]杨跃明,杨家静,杨光,等.四川盆地中部地区侏罗系致密油研究新进展[J].石油勘探与开发,2016,43(6):873-882.
[76]徐伟,陈开远,曹正林,等.咸化湖盆混积岩成因机理研究[J].岩石学报,2014,30(6):1804-1809.
[77]赵贤正,陈子料,陈洪德.柴达木盆地西部地区第二系湖相藻(蓝细菌)灰岩储层成因类型[J].沉积学报,2004,22(2):216-224.
[78]伏美燕.混积背景下碳酸盐岩储层形成机理[D].成都:成都理工大学,2013.
[79]尹柯惟,刘颖,赵文婷,等.混合沉积研究进展及其油气地质意义[J].天然气技术与经济,2017,11(3):15-18.
[80]丁一,李智武,冯逢,等.川中龙岗地区下侏罗统自流井组大安寨段湖相混合沉积及其致密油勘探意义[J].地质论评,2013,59(2):389-400.
[81]王晓琦,孙亮,朱如凯,等.利用电子束荷电效应评价致密储集层储集空间:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].石油勘探与开发,2015,42(4):472-480.
[82]高岗,向宝力,李涛涛,等.吉木萨尔凹陷芦草沟组致密油系统的成藏特殊性[J].沉积学报,2017,35(4):824-833.
[83]邱振,施振生,董大忠,等.致密油源储特征与聚集机理:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].石油勘探与开发,2016,43(6):928-939.
[84]葸克来,操应长,朱如凯,等.吉木萨尔凹陷二叠系芦草沟组致密油储层岩石类型及特征[J].石油学报,2015,36(12):1495-1507.
[85]刘冬冬,张晨,罗群,等.准噶尔盆地吉木萨尔凹陷芦草沟组致密储层裂缝发育特征及控制因素[J].中国石油勘探,2017,22(4):36-47.
[86]刘效妤.新疆准噶尔盆地吉木萨尔凹陷致密储层裂缝发育程度与岩性的关系[J].石化技术,2017,24(10):119.
[2]郭福生.浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义[J].沉积学报,2004,22(1):136-141.
[3]董桂玉,陈洪德,何幼斌,等.陆源碎屑与碳酸盐混合沉积研究中的几点思考[J].地球科学进展,2007,22(9):931-940.
[4]杨朝青,沙庆安.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积[J].沉积学报,1990,8(2):59-66.
[5] Tirsga A H.Cyclic sedimentation of carbonate and siliciclastic deposits on a Late Precambrian ramp:The Elisabeth Bjerg Formation(Eleonore Bay Supergroup)East Greenland[J].Journal of Sedimentary Research,1996,66(4):699-712.
[6]沙庆安.混合沉积和混积岩的讨论[J].古地理学报,2001,3(3):63-66.
[7] Brooks G R,Doyle L J,Suthard B C,et al.Facies architecture of the mixed carbonate/siliciclastic inner continental shelf of west-central Florida:Implications for Holocene barrier development[J].Marine Geology,2003,200(1/4):325-349.
[8] Garcia-Hidalgo J F,Gil J,Segura M,et al.Internal anatomy of a mixed siliciclastic-carbonate platform:The Late CenomanianMid Turonian at the southern margin of the Spanish Central System[J].Sedimentology,2007,54(6):1245-1271.
[9]廖群山,胡华,林建平,等.四川盆地川中侏罗系致密储层石油勘探前景[J].石油与天然气地质,2011,32(54):815-822.
[10]赵贤正,姜在兴,张锐锋,等.陆相断陷盆地特殊岩性致密油藏地质特征与勘探实践:以束鹿凹陷沙河街组致密油藏为例[J].石油学报,2015,36(增刊1):1-9.
[11]查明,苏阳,高长海,等.致密储层储集空间特征及影响因素:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].中国矿业大学学报,2017,46(1):85-95.
[12]Bruckner W D.Cyclic calcareous sedimentation as an index of climatic variation in the past[J].Journal of Sedimentary Petrology,1953,23(4):235-237.
[13]Carozzi A.Some remarks on cyclic calcareous sedimentation as an index of climatic variations[J].Journal of Sedimentary Petrology,1955,25(1):78-79.
[14]Maxwell W G,Swinchatt J P.Great barrier reef:Regional variation in a Terrigenous-Carbonate province[J].Geological Society of American Bulletin,1970,81(3):691-724.
[15]Butto N A,Vos R G.Subtidal and intertidal clastic and carbonate sedimentation in amacrotidal environment:An example from the Lower Proterozoic of South Africa[J].Sedimentary Geology,1977,18(1/3):175-200.
[16]Price I.Deposition and derivation of clastic carbonate on a Mesozoic continental margin,Orthis,Greece[J].Sedimentology,1977,24(4):529-546.
[17]Markello J R,Read J F.Carbonate ramp-to-deeper shale shelf transitions of an Upper Cambrian intrashelf basin:Nolichucky Formation,southwest Virginia,Appalachians[J].Sedimentology,1981,28(4):573-597.
[18]Tucker M.Storm-surge sandstones and the deposition of interbedded limestone:Late Precambrian,southern Norway[M]∥Einsele G,Seilacher A.Cyclic and event stratification.Berlin:Springer-Verlag,1982:363-370.
[19]刘宝珺,余光明,王成善,等.珠穆朗玛峰地区侏罗纪沉积环境[J].沉积学报,1983,1(2):1-16.
[20]Cawthope R I.Sedimentation during carbonate ramp-to-slope evolution in a technically active area:Bavland basin(Dinantian),Norlhern England[J].Sedimentology,2010,33(2):185-206.
[21]Roberts H H.Modern caibonate-siliciclastic transitions:Humid and arid tropical examples[J].Sedimentary Geology,1987,50(1/3):25-65.
[22]Dolyle L J,Roberts H H.Carbonate-clastic transitions[M].New York:Elsevier,1988:142.
[23]Dolan J F.Eustatic and tectonic controls on deposition of hybrid siliciclastic/carbonate basinal cycles:Discussion with examples[J].AAPG Bulletin,1989,73(10):1233-1246.
[24]Yose L A,Heller P L.Sea level controls of mixed carbonate-siliciclastic gravity flow deposition,lower part of the Keeler Canyon Formation(Pennsylvanian),Southeastern California[J].Geological Society of America Bulletin,1989,101(3):422-439.
[25]Lomando A I,Harris P M.Mixed carbonate-siliciclastic sequences[M].[S.l.]:SEPM(Society for Sedimentary Geology),1991:568.
[26]张廷山,兰光志,陈晓慧.川西北早志留世陆缘碎屑-碳酸盐混积缓坡[J].沉积学报,1995,13(4):27-35.
[27]张雄华.混积岩的分类和成因[J].地质科技情报,2000,19(4):31-34.
[28]Lubesedera S,Redferna J,Boutibb L.Mixed siliciclastic carbonate shelf sedimentation Lower Devonian sequences of the SW Anti-Atlas,Morocco[J].Sedimentary Geology,2008,215(1/4):13-32.
[29]宋章强,陈延芳,杜晓峰,等.渤海海域A构造区沙二段混合沉积特征及储层研究[J].海洋石油,2013,33(4):13-18.
[30]Toshifumi K,Hajime N,Yasunari S,et al.Lower Triassic mixed carbonate and siliciclastic setting with Smithian-Spathian anoxic to dysoxic facies,A Chau Basin,northeastern Vietnam[J].Sedimentary Geology,2014,300:28-48.
[31]马艳萍,刘立.大港滩海区第三系湖相混积岩的成因与成岩作用特征[J].沉积学报,2003,21(4):607-613.
[32]Halfar J,Lngle J C.Modern non-tropical mixed carbonate-siliciclastic sediments and environments of the southwestern Gulf of California,Mexico[J].Sedimentary Geology,2004,165(1/2):93-115.
[33]Alex C B,Valeria S Q,Mariana B M,et al.Shelf morphology as an indicator of sedimentary,regimes:A synthesis from a mixed siliciclastic-carbonate shelf on the eastern Brazilian margin[J].Journal of South American Earth Sciences,2015,63:125-136.
[34]冯增昭.中国沉积学[M].北京:石油工业出版社,1994:623-631.
[35]Garcia-Mondejar J,Fernández-Mediola P A.Sequence stratigraphy and systems tracts of a mixed carbonate and siliciclastic platform-basin setting:the Albian of Lunada and Soba,northern Spain[J].AAPG Bulletin,1993,77(2):245-275.
[36]Steven G,Driese R H,Dott J.Model for sandstone-carbonate“cyclothems”based on upper member of Morgan Formation(Middle Pennsylvanian)of Northern Utah and Colorado[J].AAPG Bulletin,1984,68(5):574-597.
[37]Bechstǎdt T,Schweizer T.The carbonate-clastic cycles of the East-Alpine Raibl Group:Result of third-order sea-level fluctuations in the Carnian[J].Sedimentary Geology,1991,70(2/4):241-270.
[38]蔡进功,李从先.内蒙西南部石炭系碎屑岩-碳酸盐岩混合沉积特征[J].石油与天然气地质,1994,15(1):80-87.
[39]李祥辉.层序地层中的混合沉积作用及其控制因素[J].高校地质学报,2008,14(3):395-404.
[40]冯进来,胡凯,曹剑,等.陆源碎屑与碳酸盐混积岩及其油气地质意义[J].高校地质学报,2011,17(2):297-307.
[41]Davies H R.Shelf sandstones in the Mowry Shale:Evidence for deposition during Cretaceous sea level falls[J].Journal of Sedimentary Research,1989,59(4):548-560.
[42]王国忠.南海北部大陆架现代礁源碳酸盐与陆源碎屑的混合沉积作用[J].古地理学报,2001,3(2):47-54.
[43]Coffey B P,Read J F.Mixed carbonate-siliciclastic sequence stratigraphy of a Paleogene transition zone continental shelf,southeastern USA[J].Sedimentary Geology,2004,166(1/2):21-57.
[44]司马立强,杨毅,吴丰,等.柴西北小梁山地区狮子沟组混积岩储层评价[J].现代地质,2005,28(1):173-180.
[45]张金亮,司学强.断陷湖盆碳酸盐与陆源碎屑混合沉积:以东营凹陷金家地区古近系沙河街组第四段上亚段为例[J].地质论评,2007,53(4):448-454.
[46]张娣,侯中健,王亚辉,等.板桥-北大港地区沙河街组沙一段湖相碳酸盐岩沉积特征[J].岩性油气藏,2008,20(4):92-97.
[47]孙娇鹏,陈世悦,胡忠亚,等.柴东北缘古生代碎屑岩-碳酸盐岩混积相发育特征及组合模式研究[J].天然气地球科学,2014,25(10):1586-1694.
[48]Campbell A E.Shelf-geometry response to changesin relative sea level on a mixed carbonate-siliciclastic shelf in the Guyana Basin[J].Sedimentary Geology,2005,175(1/4):259-275.
[49]Garcia-Garcia F,Soria J M,Viseras C,et al.High-frequency rhythmicity in a mixed siliciclastic-carbonate shelf(Late Miocene,Guadix basin,Spain):A model of interplay between climatic oscillations,subsidence,and sediment dispersal[J].Journal of Sedimentary Research,2009,79(5/6):302-315.
[50]Miller R P,Hiller P L.Depositional framework and controls on mixed carbonate-siliciclastic gravity flows:Pennsylvanian-Permian shelf to basin transect,south-western Great Basin,USA[J].Sedimentology,1994,41(1):1-20.
[51]李祥辉,曾允孚.扬子西缘泥盆纪碳酸盐与陆源碎屑的混合沉积层序和层序混合沉积模式[J].沉积学报,1999,17(3):339-344.
[52]El-Azabi M H,El-Araby A.Depositional framework and sequence stratigraphic aspects of the Coniacian-Santonian mixed siliciclastic/carbonate Matulla sediments in Nezzazat and Ekma blocks,Gulf of Suez,Egypt[J].Journal of African Earth Sciences,2007,47(4/5):179-202.
[53]Korngreen D,Bialik O M.The characteristics of carbonate system recovery during a relatively dry event in a mixed carbonate/siliciclastic environment in the Pelsonian(Middle Triassic)proximal marginal marine basins:A case study from the tropical Tethyan northwest Gondwana margins[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2015,440:793-812.
[54]Hersi O S,Abbasib I A,Al-Harthy A.Sedimentology,rhythmicity and basin-fill architecture of a carbonate ramp depositional system with intermittent terrigenous influx:The Albian Kharfot Formation of the Jeza-Qamar Basin,Dhofar,Southern Oman[J].Sedimentary Geology,2016,331:114-131.
[55]Zahra S,Annette D G,Maurice E T.Sequence development of a latest Devonian-Tournaisian distally-steepened mixed carbonate-siliciclastic ramp,Canning Basin,Australia[J].Sedimentary Geology,2016,333:164-183.
[56]张少敏,操应长,朱如凯,等.湖相细粒混合沉积岩岩石类型划分:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].地学前缘,2018,25(4):198-209.
[57]张亚奇,马世忠,高阳,等.吉木萨尔凹陷芦草沟组致密油储层沉积相分析[J].沉积学报,2017,35(2):358-370.
[58]马克,侯加根,刘钰铭,等.吉木萨尔凹陷二叠系芦草沟组咸化湖混合沉积模式[J].石油学报,2017,38(6):636-648.
[59]邵雨,杨勇强,万敏,等.吉木萨尔凹陷二叠系芦草沟组沉积特征及沉积相演化[J].新疆石油地质,2015,36(6):635-641.
[60]张锦泉,叶红专.论碳酸盐与陆源碎屑的混合沉积[J].成都地质学院学报,1989,16(2):87-92.
[61]Dorsey R J,Kidwell S M.Mixed carbonate-siliciclastic sedimentation on a tectonically active margin:Example from the Pliocene Baja California Sur,Mexico[J].Geology,1999,27(10):935-938.
[62]Harrowfield M,Keep M.Tectonic modification of the Australian North-West Shelf:Episodic rejuvenation of long-lived basin divisions[J].Basin Research,2005,17(2):225-239.
[63]陈怀龙,王兆峰,汪文,等.阿富汗喀什喀里油田下白垩统阿普第阶地层混合沉积特征研究[J].石油天然气学报,2013,35(11):11-15.
[64]赵灿,李旭兵,郇金来,等.碳酸盐与硅质碎屑的混合沉积机理和控制因素探讨[J].地质论评,2013,59(4):615-626.
[65]江茂生,沙庆安.碳酸盐与陆源碎屑的混合沉积体系研究进展[J].地球科学进展,1995,10(6):551-554.
[66]匡立春,唐勇,雷德文,等.准噶尔盆地二叠系咸化湖相云质岩致密油形成条件与勘探潜力[J].石油勘探与开发,2012,39(6):657-668.
[67]孟元林,祝恒东,李新宁.白云岩溶蚀的热力学分析与次生孔隙带预测:以三塘湖盆地二叠系芦草沟组二段致密凝灰质白云岩为例[J].石油勘探与开发,2014,41(6):690-696.
[68]李婷婷,朱如凯,白斌,等.混积岩储层特征:以酒泉盆地青西凹陷下白垩统混积岩为例[J].沉积学报,2015,33(2):376-384.
[69]高岗,向宝力,王轩,等.准噶尔盆地吉木萨尔凹陷芦草沟组湖相混合沉积中缝合线发育与有机质富集研究[J].天然气地球科学,2016,27(11):1963-1969.
[70]Poeppelreiter M,Aigner T.Unconventional pattern of reservoir facies distribution in epeiric successions:Lessons from an outcrop analogy(Lower Keuper,Germany)[J].AAPG Bulletin,2003,87(1):39-70.
[71]Palermol D,Aignerl T,Geluk M.Reservoir potential of a lacustrine mixed carbonate/siliciclastic gas reservoir the lower Triassic Rogenstein in the Netherlands[J].Journal of Petroleum Geology,2008,31(1):61-96.
[72]李新宁,马强,梁辉,等.三塘湖盆地二叠系芦草沟组二段混积岩致密油地质特征及勘探潜力[J].石油勘探与开发,2015,42(6):763-772.
[73]闫伟鹏,杨涛,李欣,等.中国陆上湖相碳酸盐岩地质特征及勘探潜力[J].中国石油勘探,2014,19(4):11-17.
[74]张新顺,王红军,马锋,等.致密油资源富集区与“甜点区”分布关系研究:以美国威利斯顿盆地为例[J].石油实验地质,2015,37(5):619-626.
[75]杨跃明,杨家静,杨光,等.四川盆地中部地区侏罗系致密油研究新进展[J].石油勘探与开发,2016,43(6):873-882.
[76]徐伟,陈开远,曹正林,等.咸化湖盆混积岩成因机理研究[J].岩石学报,2014,30(6):1804-1809.
[77]赵贤正,陈子料,陈洪德.柴达木盆地西部地区第二系湖相藻(蓝细菌)灰岩储层成因类型[J].沉积学报,2004,22(2):216-224.
[78]伏美燕.混积背景下碳酸盐岩储层形成机理[D].成都:成都理工大学,2013.
[79]尹柯惟,刘颖,赵文婷,等.混合沉积研究进展及其油气地质意义[J].天然气技术与经济,2017,11(3):15-18.
[80]丁一,李智武,冯逢,等.川中龙岗地区下侏罗统自流井组大安寨段湖相混合沉积及其致密油勘探意义[J].地质论评,2013,59(2):389-400.
[81]王晓琦,孙亮,朱如凯,等.利用电子束荷电效应评价致密储集层储集空间:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].石油勘探与开发,2015,42(4):472-480.
[82]高岗,向宝力,李涛涛,等.吉木萨尔凹陷芦草沟组致密油系统的成藏特殊性[J].沉积学报,2017,35(4):824-833.
[83]邱振,施振生,董大忠,等.致密油源储特征与聚集机理:以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例[J].石油勘探与开发,2016,43(6):928-939.
[84]葸克来,操应长,朱如凯,等.吉木萨尔凹陷二叠系芦草沟组致密油储层岩石类型及特征[J].石油学报,2015,36(12):1495-1507.
[85]刘冬冬,张晨,罗群,等.准噶尔盆地吉木萨尔凹陷芦草沟组致密储层裂缝发育特征及控制因素[J].中国石油勘探,2017,22(4):36-47.
[86]刘效妤.新疆准噶尔盆地吉木萨尔凹陷致密储层裂缝发育程度与岩性的关系[J].石化技术,2017,24(10):119.