A Comparative Study of the Geological Feature of Marine Shale Gas between China and the United States
Received date: 2015-01-24
Revised date: 2015-04-22
Online published: 2015-09-10
Through detailed studies of marine shale gas in China and investigation of typical shale gas zones in the United States,similarities and differences of geological features of the shale gas in USA and China were summarized.The comparative study is of important theoretical and practical significance for marine shale gas in Sichuan Basin.(1)Barnett,Marcellus and Haynesville shale basins are foreland basin,while Sichuan basin in Paleozoic is intra-craton basin.Their depositional environments are deep water shelf,mainly siliceous and calcareous shale,with high brittleness mineral content.(2)TOC of Barnett shale is 3%-13%,averaged at 4.5%;Marcellus is 3%-12%,averaged at 4.0%;and Haynesville shale is 0.5%-4%.TOC of Wufeng-Longmaxi and Qiongzhusi is 1.5%-3% and 2.5%-4.5%,respectively.(3)Maturity of three major shale formations is moderate,while that of Sichuan Basin is at over-mature stage.The RO values of the Barnett,Marcellus and Haynesville formations are 0.5%-2.1%,1.2%-3.5%,and 1.2%-3%,respectively.However,the ROvalues of the Longmaxi and Qiongzhusi formations are 2.5%-4.5% and 1.5%-3%,respectively.(4)Barnett shale has thickness of 30-180m,porosity of 4%-5%,and permeability less than 1×10-3μm2;Marcellus shale has thickness of 15-60m,porosity averagely of 10%,and permeability less than 1×10-3μm2;Haynesville shale has thickness of 70-100m,porosity of 8%-9%,and permeability less than 5×10-3μm2.Longmaxi shale has thickness of 25-120m,porosity of 3%-10%,and permeability of(0.01-1)×10-3μm2;Qiongzhuxi shale has thickness of 40-100m,porosity of 0.1%-3%,and permeability of(0.01-42)×10-3μm2.(5)Gas contents of Barnett,Marcellus and Haynesville shale are 4.2-9.9,1.70-2.83 and 2.5-9m3/t,respectively,and that of Longmaxi and Qiongzhusi shale are 1.7-4.5 and 0.55-1.2 m3/t,respectively.(6)Except Qiongzhuxi shale,the other four shale formations have good sedimentary cover,which is conducive to gas preservation.(7)American shales have more favorable surface conditions,mostly plains,while mostly hills in Sichuan Basin.(8)Except Haynesville shale,fractures are well developed in other shale formations.(9)Shale gases from both the USA and China have rich resource potential.The Geological and technically recoverable resources of Longmaxi Formation are 17.5×1012m3 and 1.77×1012m3,respectively while that of Qiongzhusi Formation are 8.86×1012m3 and 0.886×1012m3,respectively.
WANG Shu-fang,DONG Da-zhong,WANG Yu-man,LI Xin-jing,HUANG Jin-liang,GUAN Quan-zhong . A Comparative Study of the Geological Feature of Marine Shale Gas between China and the United States[J]. Natural Gas Geoscience, 2015 , 26(9) : 1666 -1678 . DOI: 10.11764/j.issn.1672-1926.2015.09.1666
[1]Rach N M.Drilling expands in Texas′ largest gas field[J].Oil & Gas Journal,2004,102(3):45-50.
[2]Berman A E.Shale plays and lower natural gas prices:A time for critical thinking[J].World Oil,2009,230(1):15.
[3]Zou Caineng,Tao Shizhen,Hou Lianhua,et al.Unconventional Petroleum Geology[M].2nd Edition.Beijing:Geological Publishing House,2013.[邹才能,陶士振,侯连华,等.非常规油气地质[M].第2版.北京:地质出版社,2013.]
[4]Zou Caineng,Yang Zhi,Zhang Guosheng,et al.Conventional and unconventional petroleum “orderly accumulation”:Concept and practical significance[J].Petroleum exploration and development,2014,41(1):14-27.[邹才能,杨智,张国胜,等.常规—非常规油气“有序聚集”理论认识及实践意义[J].石油勘探与开发,2014,41(1):14-27.]
[5]Liu Shugen,Li Zhiwu,Sun Wei,et al.Basic geological features of superimposed basin and hydrocarbon accumulation in Sichuan Basin,China[J].Chinese Journal of Geology,2011,46(1):233-257.[刘树根,李智武,孙玮,等.四川含油气叠合盆地基本特征[J].地质科学,2011,46(1):233-257.]
[6][JP2]Walper J L.Plate tectonic evolution of the Fort Worth Basin[C]//Martin C A,ed.Petroleum Geology of the Fort Worth Basin and Bend Arch Area.Dallas Geological Society,1982,237-251.
[7]Pollastro R M,Jarvie D M,Hill R J,et al.Geologic framework of the Mississippian Barnett Shale,Barnett-Paleozoic total petroleum system,Bend arch-Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):405-436.
[8][JP2]Lash G G,Engelder.Thickness trends and sequence stratigraphy of the Middle Devonian Marcellus Formation,Appalachian Basin:Implications for Acadian foreland basin evolution[J]:AAPG Bulletin,2011,95:61-103.
[9]Schieber J,Zimmerle W,Sethi P S.Shales and mudstones I[C]//Basin Studies,Sedimentology,and Paleontology.Schweizerbartsche Verlagsbuchhandlung,Germany:Stuttgart,1998:384.
[10]Locks R G,Ruppel S C.Mississippian Barnett shale:Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):579-601.
[11][JP2]Brett C E,Baird G C.Middle Devonian sedimentary cycles and sequences in the northern Appalachian Basin[C]//Witzke B J,Ludvigson G A,Day J,et al.Paleozoic Sequence Stratigraphy:Views from the North American Craton Boulder,Colorado:Geological Society of America Special Paper,1996:213-241.
[12]Ulmishe G F,Klemme H D.Depositional controls,distribution,and effectiveness of world’s petroleum source rocks[J].US Geological Survey Bulletin,1990,1931:59.
[13]John B C.Fractured shale gas systems[J].AAPG Bulletin,2002,86(11):1921-1938.
[14]Chalmers R G,Bustin R M,Power M I.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.
[15]Hammes U,Hamlin H S,Ewing T E.Geologic analysis of the Upper Jurassic Haynesville shale in east Texas and west Louisiana[J].AAPG,2011,95(10):1643-1666.
[16]Kitty L M,William L E,Robert MR,et al.Grain assemblages and stronge diagenetic overprinting in siliceous mudrcoks,Barnett Shale Mississippian,Fort Worth Basin,Texas[J].AAPG Bulletin,2012,96(8):1553-1578.
[17]Liang Digang,Guo Tonglou,BianLizeng,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China( part 3):Controlling factors on the sedimentary facies and development of paleozoic marine source rocks[J].Marine Origin Petroleum Geology,2009,14(2):1-19.[梁狄刚,郭彤楼,边立曾,等,中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.]
[18]Wang G,Timothy R C.Organic-rich Marcellus shale lithofacies modeling and distribution pattern analysis in the Appalachian Basin[J].AAGP Bulletin,2013,97(12):2173-2205.
[19]Zou Caineng,Dong Dazhong,Wang Shejiao,et al.Geological characteristics,formation mechanism and resource potential of shale gas in China[J].Petroleum Exploration and Development,2010,37(6):641-653.[邹才能,董大忠,王社教,等.中国页岩气形成机理、地质特征及资源潜力[J].石油勘探与开发,2010,37(6):641-653.]
[20]Huang Jinliang,Zou Caineng,Li Jianzhong,et al.Shale gas generation and potentional of the Lower Cambrian Qiongzhusi Formation in southern Sichuan Basin,China[J].Petroleum Exploration and Development,2012,39(1):69-76.[黄金亮,邹才能,李建忠,等.川南下寒武统筇竹寺组页岩气形成条件及资源潜力[J].石油勘探与开发,2012,39(1):69-76.]
[21]Curtis J B.Fractured shale-gas systems[J].AAPG Bulletin,2002,86(11):1921-1938.
[22]Slat R M,O’Brien N R.Pore types in Barnett and Woodford gas shales:Contributions to understanding gas storage and migration pathways in fine-grained rocks[J].AAPG Bulletin,2011,95(11):2017-2030.
[23]Loucks R G,Reed R M,Ruppel S C,et al.Morphology,genesis and distribution of nanometer-scale pores in siliceous mudstones of the Mississippian Barnett shale[J].Journal of Sedimentary Research,2009,79(12):848-861.
[24]Li Xinjing,Hu Suyun,Cheng Keming,Suggestions from the development of fractured shale gas in North America[J].Petroleum Exploration and Development,2007,34(4):392-400.[李新景,胡素云,程克明,北美裂缝性页岩气勘探开发的启示[J].石油勘探与开发,2007,34(4):392-400.]
[25]Wang Xiang,Liu Yuhua,Zhang Min,et al.Conditons of Formation and Accumulation for shale gas[J].Natural Gas Geoscience,2010,21(2):350-356.[王祥,刘玉华,张敏,等.页岩气形成条件及成藏影响因素研究[J].天然气地球科学,2010,21(2):350-356.]
[26]Zhang Jinchuan,Jin Zhijun,Yuan Mingsheng,Reservoiring mechanism of shale gas and its distribution[J].Natural Gas Industry,2004,24(7):15-18.[张金川,金之钧,袁明生.页岩气成藏机理和分布[J].天然气工业,2004,24(7):15-18.]
[27]Gale J F W,Reed RM,Holder J.Natural fractures in the Barnett Shale and their importance for hydraulic fracture treatments[J].AAPG Bulletin,2007,91(4):603-622.
[28]Engelder TG,Lash G,Uzcategui R S.Joint sets that enhance production from Middle and Upper Devonian gas shales of the Appalachian Basin[J].AAPG Bulletin,2009,93(7):857-889.
[29]Daniel J K,Ross R,MarcBustin.Sediment geochemistry of the Lower Jurassic Gordondale Member,northeastern British Columbia[J].Bulletin of Canadian Petroleum Geology,2006,54(4):337-365.
[30]Zhang Linye,Li Zheng,Zhu Rifang.The formation and exploitation of shale gas[J].Natural Gas Industry,2009,29(1):124-128.[张林晔,李政,朱日房.页岩气的形成与开发[J].天然气工业,2009,29(1):124-128.]
[31]EIA.Annual energy outlook 2011[J/OL].[2010-12-16].http//www.eia.gov/forecasts/aeo/pdf/0383er(2011).pdf
/
〈 |
|
〉 |