Applications of Light Stable Isotopes(C, O, H) in the Study of Sandstone Diagenesis: A Review
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摘要
This article reviews the applications of light stable isotope, including carbon, oxygen and hydrogen, in thestudies on origin and formation temperature of authigenic carbonate, quartz and clay minerals. Theoretical knowledge andanalytical methods for major light stable isotopes are introduced in detail. Negative and positive δ~(13)C values indicatesignificant differences on the origin of carbonate cements. The δ~(18)O value is an effective palaeotemperature scale forauthigenic minerals formation. Various fractionation equations between δ~(18)O and temperature are proposed for carbonatecements, quartz cements and clay minerals, whose merit and demerit, applicable conditions are clarified clearly. Clumpedisotope analysis can reconstruct the temperature of carbonate precipitation with no requirement on the δ~(18)O of initial waters,which makes temperature calculation of carbonate cements formation more convenient and accurate. Hydrogen and oxygenisotopes mainly reflect the origin of diagenetic fluid for clay mineral formation, providing reliable evidence for diageneticenvironment analysis. This work aims at helping researchers for better understanding the applications of light stable isotopein sandstone diagenesis.
This article reviews the applications of light stable isotope, including carbon, oxygen and hydrogen, in thestudies on origin and formation temperature of authigenic carbonate, quartz and clay minerals. Theoretical knowledge andanalytical methods for major light stable isotopes are introduced in detail. Negative and positive δ~(13)C values indicatesignificant differences on the origin of carbonate cements. The δ~(18)O value is an effective palaeotemperature scale forauthigenic minerals formation. Various fractionation equations between δ~(18)O and temperature are proposed for carbonatecements, quartz cements and clay minerals, whose merit and demerit, applicable conditions are clarified clearly. Clumpedisotope analysis can reconstruct the temperature of carbonate precipitation with no requirement on the δ~(18)O of initial waters,which makes temperature calculation of carbonate cements formation more convenient and accurate. Hydrogen and oxygenisotopes mainly reflect the origin of diagenetic fluid for clay mineral formation, providing reliable evidence for diageneticenvironment analysis. This work aims at helping researchers for better understanding the applications of light stable isotopein sandstone diagenesis.
This article reviews the applications of light stable isotope, including carbon, oxygen and hydrogen, in thestudies on origin and formation temperature of authigenic carbonate, quartz and clay minerals. Theoretical knowledge andanalytical methods for major light stable isotopes are introduced in detail. Negative and positive δ~(13)C values indicatesignificant differences on the origin of carbonate cements. The δ~(18)O value is an effective palaeotemperature scale forauthigenic minerals formation. Various fractionation equations between δ~(18)O and temperature are proposed for carbonatecements, quartz cements and clay minerals, whose merit and demerit, applicable conditions are clarified clearly. Clumpedisotope analysis can reconstruct the temperature of carbonate precipitation with no requirement on the δ~(18)O of initial waters,which makes temperature calculation of carbonate cements formation more convenient and accurate. Hydrogen and oxygenisotopes mainly reflect the origin of diagenetic fluid for clay mineral formation, providing reliable evidence for diageneticenvironment analysis. This work aims at helping researchers for better understanding the applications of light stable isotopein sandstone diagenesis.
引文
Alexandre,A.,Meunier,J.D.,Llorens,E.,Hill,S.M.,and Savin,S.M.,2004.Methodological improvements for investigating silcrete formation:petrography,Ft-IR and oxygen isotope ratio of silcrete quartz cement,Lake Eyre Basin(Australia).Chemical Geology,211(3-4):261-274.
Aplin,A.C.,and Warren,E.A.,1994.Oxygen isotopic indications of the mechanisms of silica transport and quartz cementation in deeply buried sandstones.Geology,22(9):847-850.
Ayalon,A.,and Longstaffe,F.J.,1988.Oxygen isotope studies of diagenesis and pore-water evolution in the western Canada sedimentary basin:evidence from the upper Cretaceous Basal Belly River sandstone,Alberta.Journal of Sedimentary Research,58(3):489-505.
Bath,A.H.,Milodowski,A.E.,and Piro,B.,1987.Diagenesis of carbonate cements in Permo-Triassic sandstones in the Wessex and East Yorkshire-Lincolnshire Basins,UK:a stable isotope study.Geological Society London Special Publications,36(1):173-190.
Bian,Y.,Feng,D.,Roberts,H.H.,and Chen,D.,2013.Tracing the evolution of seep fluids from authigenic carbonates:Green Canyon,northern Gulf of Mexico.Marine and Petroleum Geology,44(3):71-81.
Bigeleisen,J.,and Mayer,M.G.,1947.Calculation of equilibrium constants for isotopic exchange reactions.Journal of Chemical Physics,15(5):261-267.
Birger,R.,2005.Radiometric dating of sedimentary rocks:the application of diagenetic xenotime geochronology.EarthScience Reviews,68(3):197-243.
Bj?rlykke,K.,1998.Clay mineral diagenesis in sedimentary basins-a key to the prediction of rock properties.Examples from the North Sea.Clay Minerals,33:15-34.
Bonifacie,M.,Calmels,D.,Eiler,J.M.,Horita,J.,Chaduteau,C.,Vasconcelos,C.,Agrinier,P.,Katz,A.,Passey,B.H.,Ferry,Jc.luMm.,p aendd iBsootuorprean dt,h eJr.Jm.,o 2m0e1te7r.Cfraolimbr a t2io5n toof t3h5e 0 odCol,o maintde implications for a universal calibration for all(Ca,Mg,Fe)CO3 carbonates.Geochimica et Cosmochimica Acta,200:255-279.
Borthwick,J.,and Harmon,R.S.,1982.A note regarding ClF3 as an alternative to BrF5 for oxygen isotope analysis.Geochimica et Cosmechimica Acta,46(9):1665-1668.
Brint,J.F.,Hamilton,P.J.,Haszeldine,R.S.,Fallick,A.E.,and Brown,S.,1991.Oxygen isotopic analysis of diagenetic quartz overgrowths from the Brent Sands:a comparison of two preparation methods.Journal of Sedimentary Research,61(4):527-533.
Bristow,T.F.,Bonifacie,M.,Derkowski,A.,Eiler,J.M.,and Grotzinger,J.P.,2011.A hydrothermal origin for isotopically anomalous cap dolostone cements from south China.Nature,474(7349):68-71.
Bui,H.B.Ngo,X.T.,Song,Y.,Itaya,T.,Yagi,K.,Khuong,T.H.,and Nguyen,T.D.,2016.K-Ar dating of fault Gouges from the Red River Fault Zone of Vietnam.Acta Geologica Sinica(English Edition),90(5):1653-1663.
Came,R.E.,Eiler,J.M.,Veizer,J.,Azmy,K.,Brand,U.,and Weidman,C.R.,2007.Coupling of surface temperatures and atmospheric CO2 concentrations during the Palaeozoic era.Nature,449:198-201.
Cao,Jian,Hu,Wenxuan,Yao,Suping,Zhang,Yijie,Wang,Xulong,Zhang,Yueqian and Huang,Zhijiu,2007.Carbon,Oxygen and strontium Iisotope composition of calcite veins in the Carboniferous to Permian source sequences of the Junggar basin:Implications on petroleum fluid migration.Acta Sedimentologica Sinica,25(5):722-729(in Chinese with English abstract).
Capuano,R.M.,1992.The temperature dependence of hydrogen isotope fractionation between clay minerals and water:evidence from geopressured systems.Geochimica et Cosmechimica Acta,56(6):2547-2554.
Chacko,T.,and Deines,P.,2008.Theoretical calculation of oxygen isotope fractionation factors in carbonate systems.Geochimica et Cosmechimica Acta,72(15):3642-3660.
Chen,Z.,and Zhang,L.,1992.Hydrogen and oxygen isotope fractionation mechanism in the hydrothermal system and its geologic significance.Acta Geologica Sinica(English Edition),66(4):397-409.
Clayton,R.N.,Jones,B.F.,and Berner,R.A.,1968.Isotope studies of dolomite formation under sedimentary conditions.Geochimica et Cosmechimica Acta,32(4):415.
Clayton,R.N.,O’Neil,J.R.,and Mayeda,T.K.,1972.Oxygen isotope exchange between quartz and water.Journal of Geophysical Research,77,3057-3067.
Cole,D.R.,1985.A preliminary evaluation of oxygen isotopic exchange between chlorite and water.Geological Society of America,Abstracts with Program,17:550.
Coplen,T.B.,Kendall,C.,and Hopple,J.,1983.Comparison of stable isotope reference samples.Nature,302(5905):236-238.
Craig,H.,1961.Standard for reporting concentrations of deuterium and oxygen-18 in natural waters.Science,133(3467):1833-1834.
Curtis,C.D.,1972.Possible links between sandstone diagenesis and depth-related geochemical reactions occurring in enclosing mudstones.Journal of the Geological Society,135(1):107-117.
Davidson,J.P.,Tepley,F.J.,and Knesel,K.M.,1998.Isotopic fingerprinting may provide insights into evolution of magmatic systems.Eos Transactions American Geophysical Union,79(15):185-193.
Denny,A.C.,Kozdon,R.,Kitajima,K.,and Valley,J.W.,2017.Issaontdosptiocnaellsy o fz otnheed I llcianrobios n aBtaes icn:e mδe18ntOs ainnd Eδ1a3rlCy r ePcaolredosz o iocf burial and fluid flow.Sedimentary Geology,361:93-110.
Eiler,J.M.,2007.’Clumped-isotope’geochemistry-The study of naturally-occurring multiply-substituted isotopologues.Earth&Planetary Science Letters,262(3-4):309-327.
Eiler,J.M.,2011.Paleoclimate reconstruction using carbonate clumped isotope thermometry.Quaternary Science Reviews,
Eil3er0,(2 J5.):M 3.,5 7a5n-d3 5 8S8c.hauble,E.,2004.18O13C16O in earth’s atmosphere.Geochimica et Cosmechimica Acta,68(23):4767-4777.
Friedman,I.,O’Neil,J.R.,1977.Compilation of stable isotope fractionation factors of geochemical interest(6th ed).Data of Geochemistry,Geol Surv Prof Pap 440KK.
Fritz,P.,and Smith,D.G.W.,1970 Isotopic composition of secondary dolomites.Geochimica et Cosmechimica Acta,34(11):1161-1173.
Fu,Yangang,Hu,Guyue,Tang,Juxing,Liu,Qiuping and Wang,Hao,2017.Low Sulfidation epithermal Ag Pb Zn deposit in Sinongduo,Tibet:Tracer application of Si H Ostable isotope geochemistry.Acta Geologica Sinica,91(4):836-848(in Chinese with English abstract)
GhEo.sAh,.,P.S,cAhrdakgi,n s,D J.,.,aAnfdf e kE,i lHer.,,BJ.alMta.,,B2.0,0G6.uo1,3 CW-1.8F.O,Sbcohnadusb lien,carbonate minerals:A new kind of paleothermometer.Geochimica et Cosmechimica Acta,70(6):1439-1456.
Gieskes,J.M.,and Lawrence,J.R.,1981.Alteration of volcanic matter in deep sea sediments:evidence from the chemical composition of interstitial waters from deep sea drilling cores.Geochimica et Cosmechimica Acta,45(10):1687-1703.
Girard,J.P.,Munz,I.A.,Johansen,H.,Hill,S.,and Canham,A.,2001.Conditions and timing of quartz cementation in Brent reservoirs,Hild Field,North Sea:constraints from fluid inclusions and SIMS oxygen isotope microanalysis.Chemical Geology,176(1-4):73-92.
Guo,W.,Mosenfelder,J.L.,Goddard III,W.A.,and Eiler,J.M.,2009.Isotopic fractionations associated with phosphoric acid digestion of carbonate minerals:Insights from first-principles theoretical modeling and clumped isotope measurements.Geochimica et Cosmochimica Acta,73(24):7203-7225.
Harwood,J.,Aplin,A.C.,Fialips,C.L.,Lliffe,J.E.,Kozdon,R.,Ushikubo T.,and Valley,J.W.,2013.Quartz cementation history of sandstones revealed by high-resolution SIMSoxygen isotope analysis.Journal of Sedimentary Research,83(7):522-530.
Haszeldine,R.S.,Brint,J.F.,Fallick,A.E.,Hamilton,P.J.,and Brown,S.,1992.Open and restricted hydrologies in Brent Group diagenesis:North Sea.Geological Society of London Special Publications,61(1):401-419.
Head,I.M.,Jones,D.M.,and Larter,S.R.,2003.Biological activity in the deep subsurface and the origin of heavy oil.Nature,426:344-352.
Hill,P.S.,Tripati,A.K.,and Schauble,E.,2014.Theoretical constraints on the effects of pH,salinity,and temperature on clumped isotope signatures of dissolved inorganic carbon species and precipitating carbonate minerals.Geochimica et Cosmechimica Acta,125:610-652.
Hoefs,J.,2009.Stable Isotope Geochemistry(6th ed).Berlin:Verlag Berlin Heidelberg,53.
Horita,J.,2014.Oxygen and carbon isotope fractionation in the system dolomite-water-CO2 to elevated temperatures.Geochimica Et Cosmochimica Acta,129(8):111-124.
Huntington,K.W.,Eiler,J.M.,Affek,H.P.,Guo,W.,Bonifacie,M.,Yueng,L.Y.,Thiagarajan,N.,Passey,B.,Tripati,A.,Daeron,M.,and Came,R.,2009.Methods and limitations of’clumped’CO2 isotope(Δ47)analysis by gas-source isotope ratio mass spectrometry.Journal of Mass Spectrometry,44(9):1318-1329.
Irwin,H.,Curtis,C.,and Coleman,M.,1977.Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments.Nature,269(5625):209-213.
Jay,Q.,Huntington,K.,Matthew,D.,Joel,S.,Ryan,L.,Peter,D.,and Barbara,C.,2013.Clumped and conventional isotope paleoaltimetry and diagenesis in Tibet.Acta Geologica Sinica(English Edition),87(z1):62.
Jiang,L.,Xu,H.C,and Qiao,H.J.,2017.Biomediated precipitation of calcium carbonate in a slightly acidic hot spring,Yunnan Province.Acta Geologica Sinica(English Edition),91(1):145-155.
Keith,L.M.,and Weber,N.J.,1964.Carbon and oxygen isotopic composition of selected limestones and fossils.Geochimica et.Cosmochimica Acta,28(10-11):1787-1816.
Kelly,J.,Fu,B.,Kita.,N.,and Valley,J.W.,2007.Optically continuous silcrete quartz cements of the St.Peter Sandstone:High precision oxygen isotope analysis by ion microprobe.Geochimica et Cosmechimica Acta,71(15):3812-3832.
Lambert,S.J.,and Epstein,S.,1980.Stable isotope investigations of an active geothermal system in Valles Caldera,Jemez Mountains,New Mexico.Journal of Volcanology&Geothermal Research,8(1):111-129.
Land,L.S.,and Dutton,S.P.,1978.Cementation of a Pennsylvanian deltaic sandstone:isotopic data.Journal of Sedimentary Petrology,48:1167-1176.
Lander,R.H.,and Bonnell,L.M.,2010.A model for fibrous illite nucleation and growth in sandstones.AAPG Bulletin,94:1161-1187.
LeeN,orMt.h,1S9e8a:4.KD-iAarg,e1n8eOsi/s1 6oOf tahne d P peertmrioagnr aRpohtilci e geveindde nscaen.d sOtohnioe:,Case Western Reserve University(Ph.D thesis):346.
Lehmann,K.,Pettke,T.,and Ramseyer,K.,2011.Significance of trace elements in syntaxial quartz cement,Haushi Group sandstones,Sultanate of Oman.Chemical Geology,280(1):47-57.
Liewig,N.,Clauer,N.,and Sommer,F.,1987.Rb-Sr and K-Ar Dating of Clay Diagenesis in Jurassic Sandstone Oil Reservoir,North Sea.AAPG Bulletin,71(12):1467-1474.
Liua,nYn.u,alT alanyge,rsG.r,eLvienagl,e dX.b,y Hsue,a sCo.,n aaln dS ILMi,SXδ.,1 82O0 1m5.e aSspuerleeomtehnetsm.Science China:Earth Sciences,58(10):1741-1747.
Lynch,L.F.,Mack,E.L.,and Land,S.L.,1997.Burial diagenesis of illite/smectite in shales and the origins of authigenic quartz and secondary porosity in sandstones.Geochimica et Cosmechimica Acta,61(10):1995-2006.
Lyu,Fenglin,Liu,Chenglin,Jiao,Pengcheng,Zhang,Hua,Sun,Xiaohong and Zhang,Yongming,2018.Carbon and oxygen isotopic compositions of the lacustrine carbonate in Lop Nur since the Mid-Pleistocene and their paleoenvironment significance.Acta Geologica Sinica,93(8),1589-1604(in Chinese with English abstract)
Macaulay,C.I.,Fallick,A.E.,Haszeldine,R.S.,and Mcaulay,dGi.sEtr.i,b u2t0io0n0.o fO icla r bmoingraattei ocne mmenatk eδs1 3 tCh ein dnifofretrheenrnc e:N orretghi oSneaal Tertiary sandstones.Clay Minerals,35(1):69-76.
Mangenot,X.,Bonifacie,M.,Gasparrini,M.,G?tz,A.,Chaduteau,C.,Ader,M.,and Rouchon,V.,2017.CouplingΔ47 and fluid inclusion thermometry on carbonate cements to precisely reconstruct the temperature,salinity andδ18O of paleo-groundwater in sedimentary basins.Chemical Geology,472:44-57.
Mansour,A.S.,Rifai,R.I.,and Shaaban,M.N.,2014.Geochemical constraint on the origin of the multi-mineralogic carbonate cements in the subsurface Middle Jurassic sandstones,Central Sinai,Egypt.Journal of Geochemical Exploration,143:163-173.
Marchand,A.M.E.,Macaulay,C.L.,Haszeldine,R.S.,and Fallick,A.E.,2002.Pore water evolution in oilfield sandstones:constraints from oxygen isotope microanalyses of quartz cement.Chemical Geology,191(4):285-304.
Matthews,A.,and Katz,A.,1977.Oxygen isotope fractionation during the dolomitization of calcium carbonate.Geochimica et Cosmechimica Acta,41(11):1431-1438.
McCrea,J.M.,1950.On the isotopic chemistry of carbonates and a paleotemperature scale.Journal of Chemical Physics,18(6):849-857.
Mernagh,T.P.,2015.A review of fluid inclusions in diagenetic systems.Acta Geologica Sinica(English Edition),89(3):697-714.
Méheut,M.,Lazzeri,M.,Balan,E.,and Mauri,F.,2007.Equilibrium isotopic fractionation in the kaolinite,quartz,water system:Prediction from first-principles densityfunctional theory.Geochimica et Cosmochimica Acta,71(13):3170-3181.
Morad,S.,Al-Aasm,I.S.,Ramseyer,K.,Marfil,R.,and Aldahan,A.A.,1990.Diagenesis of carbonate cements in Permo-Triassic sandstones from the Iberian Range,Spain:evidence from chemical composition and stable isotopes.Sedimentary Geology,67(3-4):281-295.
Morad,S.,Worden,R.H.,and Ketzer,J.M.,2003.Oxygen and hydrogen isotopic composition of diagenetic clay minerals in sandstones:a review of the data and controls.International Association of Sedimentologists.Special Publication,34:63-91.
Noh,J.H.,and Lee,I.,1999.Diagenetic pore fluid evolution in the Pohang Miocene sediments:oxygen isotopic evidence of septarian carbonate concretions and authigenic mineral phases.Geosciences Journal,3(3):141-149.
Northrop,D.A.,and Clayton,R.N.,1966.Oxygen-isotope fractionations in systems containing dolomite.Journal of Geology,74:174-196.
Sample,J.C.,Torres,M.E.,Fisher,A.,Hong,W.,Destrigneville,C.,Defliese,W.F.,and Tripati,A.E.,2017.Geochemical constraints on the temperature and timing of carbonate formation and lithification in the Nankai Trough,NanTroSEIZE transect.Geochimica et Cosmochimica Acta,198:92-114.
Santos Jr,A.E.de A.,Rossetti,D.de F.,and Murray,H.H.,2007.bOyr iδg1i8nOs oafn tdhδe DR iaon aClyaspeism.Akapoplliineidt eCs l(anyo rStchieernnc eB,r3a7z(ils)3 r-e4v):e a2l8e1d-294.
Savin,S.M.,and Epstein,S.,1970.The oxygen and hydrogen isotope geochemistry of clay minerals.Geochimica et Cosmochimica Acta,34:25-42.
Savin,S.M.,and Lee,M.,1988.Isotopic studies of phyllosilicates.Michigan,Bookcrafter Inc.,Michigan,MI,189-223.
Schfoarumblaet,i o nE.,o f G13hCos-1h8,O P b.,o nadnsd i nE iclaerr,b oJn.aMte.,m2i0n0e6r.a l sP,r eesfteirmenattieadl using first-principles lattice dynamics.Geochimica et Cosmochimica Acta,70(10):2510-2529.
Schmidt,M.,Xeflide,S.,Botz,R.,and Mann,S.,2005.Oxygen isotope fractionation during synthesis of CaMg-carbonate and implications for sedimentary dolomite formation.Geochimica et Cosmochimica Acta,69(1):4665-4674.
Sheppard,S.M.F.,and Gilg,H.A.,1996.Stable isotope geochemistry of clays.Clay Mineral,31:1-24.
Siebel,W.,Reitter,E.,Wenzel,T.,and Blaha,U.,2005.Sr isotope systematics of K-feldspars in plutonic rocks revealed by the Rb-Sr microdrilling technique.Chemical Geology,222(3):183-199.
?liwiński,M.G.,Kitajima,K.,Kozdon,R.,Spicuzza,M.J.,Fournelle,J.H.,Denny,A.,and Valley,J.W.,2015.Secondary IAonn k eMriatse,s SPpaerctt r Io:m eδt1r8yO B iaMsa torinx I sEotffoepcet s.R a tGioeso sitna nDdoalrodms i te&-Geoanalytical Research,40(2):173-184.
?liVwiańllsekyi,,J.MW.G.,.,2 0K1o6.z dMoni,c r oRa.,n a lKyistiasj i omf a,c a rKb.,o n aDtee n cney,m eAn.t,δa18nOd in a CO2-storage system seal:Insights into the diagenetic history of the Eau Claire Formation(Upper Cambrian),Illinois Basin.AAPG Bulletin,100(6):1003-1031.
Smalley,P.C.,Stijfhoom,D.E.,1989.Raheim A.,Johansen H.,and Dickson J.A.D,1989.The laser microprobe and its application to the study of C and O isotopes in calcite and aragonite.Sedimentary Geology,65(3-4):211-221.
Suess,E.,and Whiticar,M.J.,1989.Methane-derived CO2 in pore fluids expelled from the Oregon subduction zone.Palaeogeography Palaeoclimatology Palaeoecology,71(1-2):119-136.
Tran,M.D.,Liu,J.,Li,X.,and Dang,M.C.,2016.Geology,fluid inclusion and isotopic study of the Neoproterozoic Suoi Thau Copper Deposit,Northwest Vietnam.Acta Geologica Sinica(English Edition),90(3):913-927.
Tian,Hui,Li,Huaikun,Liu,Huan,Zhang,Jian,Zhou,Hongying,Zhang,Kuo,Xiang,Zhenqun,Qu,Lesheng and Wang,Zhixian,2018.Characteristics of C and O isotopes of the Shennongjia Group in the northern margin of the Yangtze Craton and their constraints on paleoenvironment and depositional age.Acta Geologica Sinica,92(12):2508-2533.(In Chinese with English abstract)
Urey,H.C.,1947.The thermodynamic properties of isotopic substances.Journal of the Chemical Society,562.
VasBceornncaeslcoosn,i,C.,S.MM.,cKe2n0z0i5e.,J.CAa.l,ib r atWioarnth moafnn,t heR.,δa18nOd paleothermometer for dolomite precipitated in microbial cultures and natural environments.Geology,33:317-320.
Wang,Darui,2000.Stable Isotope Geochemistry of Petroleum.Beijing,Petroleum Industry Press,22-23.(In Chinese)
Wesnernpeer,n t inDi.zBa.t,io na n dof Tualtyrlaorm,a f iHc.Pr.,ock1s97b1.a s eTde muppeorna tu1r8eOs/1 6oOf fractionation between coexisting serpentine and magnetite.Contributions to Mineralogy and Petrology,32(3):165-185.
Williams,L.B.,Hervig,R.L.,and Bj?rlykke,K.,1997.New evidence for the origin of quartz cements in hydrocarbon reservoirs revealed by oxygen isotope microanalyses.Geochimica et Cosmechimica Acta,61(12):2529-2538.
Woo,K.S.,and Khim,B.K.,2006.Stable oxygen and carbon isotopes of carbonate concretions of the Miocene Yeonil Group in the Pohang Basin,Korea:types of concretions and formation condition.Sedimentary Geology,183(1):15-30.
Worden,R.H.,Smalley,P.C.and Oxtoby,N.H.,1996.The effects of thermochemical sulfate reduction upon formation water salinity and oxygen isotopes in carbonate gas reservoirs.Geochimica et Cosmechimica Acta,60(20):3925-3931.
Xi,K.,Cao,Y.,Jahren,J.,Zhu,R.,Bj?rlykke,K.,Haile,B.G.,Zheng,L.,and Hellevang,H.,2015.Diagenesis and reservoir quality of the lower cretaceous quantou formation tight sandstones in the southern Songliao basin,China.Sedimentary Geology,330(C):90-107.
Xi,K.,Cao,Y.,Zhu,R.,Haile,B.G.,and Hellevang,H.,2016a.Evidences of localized CO2-induced diagenesis in the Cretaceous Quantou Formation,southern Songliao Basin,China.International Journal of Greenhouse Gas Control,52(C):155-174.
Xi,K.,Cao,Y.,Haile,B.G.,Zhu,R.,Jahren,J.,Bj?rlykke,K.,Zhang,X.,Hellevang,H.,2016b.How does the pore-throat size control the reservoir quality and oiliness of tight sandstones?The case of the Lower Cretaceous Quantou Formation in the southern Songliao Basin,China.Marine and Petroleum Geology,76:1-15.
Xiao,Wanfeng,Liu,Hong,Li,Guangming,Huang,Hanxiao,Ma,Dongfang,Zhang,Zhilin,Yan,Guoqiang and Zhang,Hong,2017.Low to moderate temperature,low salinity and enrichment of CO2 hydrothermal fluid at Shangxu orogenic gold deposit in Shuanghu,Northern Xizang(Tibet):Evidence from fluid inclusions,H-O isotopic composition.Geological Review,63(3):793-808(in Chinese with English abstract)
Yang,W.,Hu,S.,Zhang,J.,Hao,J,and Lin,Y.,2015.NanoSIMS analytical technique and its applications in earth sciences.Science China(Earth Science),58(10):1758-1767.
Yeh,H.W.,1980.D/H ratios and late stage dehydration of shales during burial.Geochimica et Cosmechimica Acta,44(2):341-352.
Zhang,X.,Su,Z.,and Gao,Y.,2017.Zircon U-Pb Geochronology and geochemistry of the early Cretaceous volcanic rocks from the Manitu Formation in the Hongol Area,Northeastern Inner Mongolia.Acta Geologica Sinica(English Edition),91(4):1286-1304.
Zheng,Jianfeng,Li,Jin,Ji,Hancheng,Huang,Lili,Hu,Anping and Ma,Mingxuan.,2017.Clumped isotope thermometry and its application in dolomite reservoir:A case study of the Middle-Lower Cambrian in Traim Basin.Marine Origin Petroleum Geology,22(2):1-7.(In Chinese)
Ziegler,K.,Sellwood,B.W.,and Fallick,A.E.,1994.Radiogenic and stable isotope evidence for age and origin of authigenic illites in the Rotliegend,Southern North Sea.Clay Minerals,29(4):555-565.
Zhu D.Y.,Liu,Q.Y.,JIN Z.J.,Meng,Q.Q.,and Hu,W.X.,2017.Effects of deep fluids on hydrocarbon generation and accumulation in Chinese petroliferous basins.Acta Geologica Sinica(English Edition),91(1):301-319.
Aplin,A.C.,and Warren,E.A.,1994.Oxygen isotopic indications of the mechanisms of silica transport and quartz cementation in deeply buried sandstones.Geology,22(9):847-850.
Ayalon,A.,and Longstaffe,F.J.,1988.Oxygen isotope studies of diagenesis and pore-water evolution in the western Canada sedimentary basin:evidence from the upper Cretaceous Basal Belly River sandstone,Alberta.Journal of Sedimentary Research,58(3):489-505.
Bath,A.H.,Milodowski,A.E.,and Piro,B.,1987.Diagenesis of carbonate cements in Permo-Triassic sandstones in the Wessex and East Yorkshire-Lincolnshire Basins,UK:a stable isotope study.Geological Society London Special Publications,36(1):173-190.
Bian,Y.,Feng,D.,Roberts,H.H.,and Chen,D.,2013.Tracing the evolution of seep fluids from authigenic carbonates:Green Canyon,northern Gulf of Mexico.Marine and Petroleum Geology,44(3):71-81.
Bigeleisen,J.,and Mayer,M.G.,1947.Calculation of equilibrium constants for isotopic exchange reactions.Journal of Chemical Physics,15(5):261-267.
Birger,R.,2005.Radiometric dating of sedimentary rocks:the application of diagenetic xenotime geochronology.EarthScience Reviews,68(3):197-243.
Bj?rlykke,K.,1998.Clay mineral diagenesis in sedimentary basins-a key to the prediction of rock properties.Examples from the North Sea.Clay Minerals,33:15-34.
Bonifacie,M.,Calmels,D.,Eiler,J.M.,Horita,J.,Chaduteau,C.,Vasconcelos,C.,Agrinier,P.,Katz,A.,Passey,B.H.,Ferry,Jc.luMm.,p aendd iBsootuorprean dt,h eJr.Jm.,o 2m0e1te7r.Cfraolimbr a t2io5n toof t3h5e 0 odCol,o maintde implications for a universal calibration for all(Ca,Mg,Fe)CO3 carbonates.Geochimica et Cosmochimica Acta,200:255-279.
Borthwick,J.,and Harmon,R.S.,1982.A note regarding ClF3 as an alternative to BrF5 for oxygen isotope analysis.Geochimica et Cosmechimica Acta,46(9):1665-1668.
Brint,J.F.,Hamilton,P.J.,Haszeldine,R.S.,Fallick,A.E.,and Brown,S.,1991.Oxygen isotopic analysis of diagenetic quartz overgrowths from the Brent Sands:a comparison of two preparation methods.Journal of Sedimentary Research,61(4):527-533.
Bristow,T.F.,Bonifacie,M.,Derkowski,A.,Eiler,J.M.,and Grotzinger,J.P.,2011.A hydrothermal origin for isotopically anomalous cap dolostone cements from south China.Nature,474(7349):68-71.
Bui,H.B.Ngo,X.T.,Song,Y.,Itaya,T.,Yagi,K.,Khuong,T.H.,and Nguyen,T.D.,2016.K-Ar dating of fault Gouges from the Red River Fault Zone of Vietnam.Acta Geologica Sinica(English Edition),90(5):1653-1663.
Came,R.E.,Eiler,J.M.,Veizer,J.,Azmy,K.,Brand,U.,and Weidman,C.R.,2007.Coupling of surface temperatures and atmospheric CO2 concentrations during the Palaeozoic era.Nature,449:198-201.
Cao,Jian,Hu,Wenxuan,Yao,Suping,Zhang,Yijie,Wang,Xulong,Zhang,Yueqian and Huang,Zhijiu,2007.Carbon,Oxygen and strontium Iisotope composition of calcite veins in the Carboniferous to Permian source sequences of the Junggar basin:Implications on petroleum fluid migration.Acta Sedimentologica Sinica,25(5):722-729(in Chinese with English abstract).
Capuano,R.M.,1992.The temperature dependence of hydrogen isotope fractionation between clay minerals and water:evidence from geopressured systems.Geochimica et Cosmechimica Acta,56(6):2547-2554.
Chacko,T.,and Deines,P.,2008.Theoretical calculation of oxygen isotope fractionation factors in carbonate systems.Geochimica et Cosmechimica Acta,72(15):3642-3660.
Chen,Z.,and Zhang,L.,1992.Hydrogen and oxygen isotope fractionation mechanism in the hydrothermal system and its geologic significance.Acta Geologica Sinica(English Edition),66(4):397-409.
Clayton,R.N.,Jones,B.F.,and Berner,R.A.,1968.Isotope studies of dolomite formation under sedimentary conditions.Geochimica et Cosmechimica Acta,32(4):415.
Clayton,R.N.,O’Neil,J.R.,and Mayeda,T.K.,1972.Oxygen isotope exchange between quartz and water.Journal of Geophysical Research,77,3057-3067.
Cole,D.R.,1985.A preliminary evaluation of oxygen isotopic exchange between chlorite and water.Geological Society of America,Abstracts with Program,17:550.
Coplen,T.B.,Kendall,C.,and Hopple,J.,1983.Comparison of stable isotope reference samples.Nature,302(5905):236-238.
Craig,H.,1961.Standard for reporting concentrations of deuterium and oxygen-18 in natural waters.Science,133(3467):1833-1834.
Curtis,C.D.,1972.Possible links between sandstone diagenesis and depth-related geochemical reactions occurring in enclosing mudstones.Journal of the Geological Society,135(1):107-117.
Davidson,J.P.,Tepley,F.J.,and Knesel,K.M.,1998.Isotopic fingerprinting may provide insights into evolution of magmatic systems.Eos Transactions American Geophysical Union,79(15):185-193.
Denny,A.C.,Kozdon,R.,Kitajima,K.,and Valley,J.W.,2017.Issaontdosptiocnaellsy o fz otnheed I llcianrobios n aBtaes icn:e mδe18ntOs ainnd Eδ1a3rlCy r ePcaolredosz o iocf burial and fluid flow.Sedimentary Geology,361:93-110.
Eiler,J.M.,2007.’Clumped-isotope’geochemistry-The study of naturally-occurring multiply-substituted isotopologues.Earth&Planetary Science Letters,262(3-4):309-327.
Eiler,J.M.,2011.Paleoclimate reconstruction using carbonate clumped isotope thermometry.Quaternary Science Reviews,
Eil3er0,(2 J5.):M 3.,5 7a5n-d3 5 8S8c.hauble,E.,2004.18O13C16O in earth’s atmosphere.Geochimica et Cosmechimica Acta,68(23):4767-4777.
Friedman,I.,O’Neil,J.R.,1977.Compilation of stable isotope fractionation factors of geochemical interest(6th ed).Data of Geochemistry,Geol Surv Prof Pap 440KK.
Fritz,P.,and Smith,D.G.W.,1970 Isotopic composition of secondary dolomites.Geochimica et Cosmechimica Acta,34(11):1161-1173.
Fu,Yangang,Hu,Guyue,Tang,Juxing,Liu,Qiuping and Wang,Hao,2017.Low Sulfidation epithermal Ag Pb Zn deposit in Sinongduo,Tibet:Tracer application of Si H Ostable isotope geochemistry.Acta Geologica Sinica,91(4):836-848(in Chinese with English abstract)
GhEo.sAh,.,P.S,cAhrdakgi,n s,D J.,.,aAnfdf e kE,i lHer.,,BJ.alMta.,,B2.0,0G6.uo1,3 CW-1.8F.O,Sbcohnadusb lien,carbonate minerals:A new kind of paleothermometer.Geochimica et Cosmechimica Acta,70(6):1439-1456.
Gieskes,J.M.,and Lawrence,J.R.,1981.Alteration of volcanic matter in deep sea sediments:evidence from the chemical composition of interstitial waters from deep sea drilling cores.Geochimica et Cosmechimica Acta,45(10):1687-1703.
Girard,J.P.,Munz,I.A.,Johansen,H.,Hill,S.,and Canham,A.,2001.Conditions and timing of quartz cementation in Brent reservoirs,Hild Field,North Sea:constraints from fluid inclusions and SIMS oxygen isotope microanalysis.Chemical Geology,176(1-4):73-92.
Guo,W.,Mosenfelder,J.L.,Goddard III,W.A.,and Eiler,J.M.,2009.Isotopic fractionations associated with phosphoric acid digestion of carbonate minerals:Insights from first-principles theoretical modeling and clumped isotope measurements.Geochimica et Cosmochimica Acta,73(24):7203-7225.
Harwood,J.,Aplin,A.C.,Fialips,C.L.,Lliffe,J.E.,Kozdon,R.,Ushikubo T.,and Valley,J.W.,2013.Quartz cementation history of sandstones revealed by high-resolution SIMSoxygen isotope analysis.Journal of Sedimentary Research,83(7):522-530.
Haszeldine,R.S.,Brint,J.F.,Fallick,A.E.,Hamilton,P.J.,and Brown,S.,1992.Open and restricted hydrologies in Brent Group diagenesis:North Sea.Geological Society of London Special Publications,61(1):401-419.
Head,I.M.,Jones,D.M.,and Larter,S.R.,2003.Biological activity in the deep subsurface and the origin of heavy oil.Nature,426:344-352.
Hill,P.S.,Tripati,A.K.,and Schauble,E.,2014.Theoretical constraints on the effects of pH,salinity,and temperature on clumped isotope signatures of dissolved inorganic carbon species and precipitating carbonate minerals.Geochimica et Cosmechimica Acta,125:610-652.
Hoefs,J.,2009.Stable Isotope Geochemistry(6th ed).Berlin:Verlag Berlin Heidelberg,53.
Horita,J.,2014.Oxygen and carbon isotope fractionation in the system dolomite-water-CO2 to elevated temperatures.Geochimica Et Cosmochimica Acta,129(8):111-124.
Huntington,K.W.,Eiler,J.M.,Affek,H.P.,Guo,W.,Bonifacie,M.,Yueng,L.Y.,Thiagarajan,N.,Passey,B.,Tripati,A.,Daeron,M.,and Came,R.,2009.Methods and limitations of’clumped’CO2 isotope(Δ47)analysis by gas-source isotope ratio mass spectrometry.Journal of Mass Spectrometry,44(9):1318-1329.
Irwin,H.,Curtis,C.,and Coleman,M.,1977.Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments.Nature,269(5625):209-213.
Jay,Q.,Huntington,K.,Matthew,D.,Joel,S.,Ryan,L.,Peter,D.,and Barbara,C.,2013.Clumped and conventional isotope paleoaltimetry and diagenesis in Tibet.Acta Geologica Sinica(English Edition),87(z1):62.
Jiang,L.,Xu,H.C,and Qiao,H.J.,2017.Biomediated precipitation of calcium carbonate in a slightly acidic hot spring,Yunnan Province.Acta Geologica Sinica(English Edition),91(1):145-155.
Keith,L.M.,and Weber,N.J.,1964.Carbon and oxygen isotopic composition of selected limestones and fossils.Geochimica et.Cosmochimica Acta,28(10-11):1787-1816.
Kelly,J.,Fu,B.,Kita.,N.,and Valley,J.W.,2007.Optically continuous silcrete quartz cements of the St.Peter Sandstone:High precision oxygen isotope analysis by ion microprobe.Geochimica et Cosmechimica Acta,71(15):3812-3832.
Lambert,S.J.,and Epstein,S.,1980.Stable isotope investigations of an active geothermal system in Valles Caldera,Jemez Mountains,New Mexico.Journal of Volcanology&Geothermal Research,8(1):111-129.
Land,L.S.,and Dutton,S.P.,1978.Cementation of a Pennsylvanian deltaic sandstone:isotopic data.Journal of Sedimentary Petrology,48:1167-1176.
Lander,R.H.,and Bonnell,L.M.,2010.A model for fibrous illite nucleation and growth in sandstones.AAPG Bulletin,94:1161-1187.
LeeN,orMt.h,1S9e8a:4.KD-iAarg,e1n8eOsi/s1 6oOf tahne d P peertmrioagnr aRpohtilci e geveindde nscaen.d sOtohnioe:,Case Western Reserve University(Ph.D thesis):346.
Lehmann,K.,Pettke,T.,and Ramseyer,K.,2011.Significance of trace elements in syntaxial quartz cement,Haushi Group sandstones,Sultanate of Oman.Chemical Geology,280(1):47-57.
Liewig,N.,Clauer,N.,and Sommer,F.,1987.Rb-Sr and K-Ar Dating of Clay Diagenesis in Jurassic Sandstone Oil Reservoir,North Sea.AAPG Bulletin,71(12):1467-1474.
Liua,nYn.u,alT alanyge,rsG.r,eLvienagl,e dX.b,y Hsue,a sCo.,n aaln dS ILMi,SXδ.,1 82O0 1m5.e aSspuerleeomtehnetsm.Science China:Earth Sciences,58(10):1741-1747.
Lynch,L.F.,Mack,E.L.,and Land,S.L.,1997.Burial diagenesis of illite/smectite in shales and the origins of authigenic quartz and secondary porosity in sandstones.Geochimica et Cosmechimica Acta,61(10):1995-2006.
Lyu,Fenglin,Liu,Chenglin,Jiao,Pengcheng,Zhang,Hua,Sun,Xiaohong and Zhang,Yongming,2018.Carbon and oxygen isotopic compositions of the lacustrine carbonate in Lop Nur since the Mid-Pleistocene and their paleoenvironment significance.Acta Geologica Sinica,93(8),1589-1604(in Chinese with English abstract)
Macaulay,C.I.,Fallick,A.E.,Haszeldine,R.S.,and Mcaulay,dGi.sEtr.i,b u2t0io0n0.o fO icla r bmoingraattei ocne mmenatk eδs1 3 tCh ein dnifofretrheenrnc e:N orretghi oSneaal Tertiary sandstones.Clay Minerals,35(1):69-76.
Mangenot,X.,Bonifacie,M.,Gasparrini,M.,G?tz,A.,Chaduteau,C.,Ader,M.,and Rouchon,V.,2017.CouplingΔ47 and fluid inclusion thermometry on carbonate cements to precisely reconstruct the temperature,salinity andδ18O of paleo-groundwater in sedimentary basins.Chemical Geology,472:44-57.
Mansour,A.S.,Rifai,R.I.,and Shaaban,M.N.,2014.Geochemical constraint on the origin of the multi-mineralogic carbonate cements in the subsurface Middle Jurassic sandstones,Central Sinai,Egypt.Journal of Geochemical Exploration,143:163-173.
Marchand,A.M.E.,Macaulay,C.L.,Haszeldine,R.S.,and Fallick,A.E.,2002.Pore water evolution in oilfield sandstones:constraints from oxygen isotope microanalyses of quartz cement.Chemical Geology,191(4):285-304.
Matthews,A.,and Katz,A.,1977.Oxygen isotope fractionation during the dolomitization of calcium carbonate.Geochimica et Cosmechimica Acta,41(11):1431-1438.
McCrea,J.M.,1950.On the isotopic chemistry of carbonates and a paleotemperature scale.Journal of Chemical Physics,18(6):849-857.
Mernagh,T.P.,2015.A review of fluid inclusions in diagenetic systems.Acta Geologica Sinica(English Edition),89(3):697-714.
Méheut,M.,Lazzeri,M.,Balan,E.,and Mauri,F.,2007.Equilibrium isotopic fractionation in the kaolinite,quartz,water system:Prediction from first-principles densityfunctional theory.Geochimica et Cosmochimica Acta,71(13):3170-3181.
Morad,S.,Al-Aasm,I.S.,Ramseyer,K.,Marfil,R.,and Aldahan,A.A.,1990.Diagenesis of carbonate cements in Permo-Triassic sandstones from the Iberian Range,Spain:evidence from chemical composition and stable isotopes.Sedimentary Geology,67(3-4):281-295.
Morad,S.,Worden,R.H.,and Ketzer,J.M.,2003.Oxygen and hydrogen isotopic composition of diagenetic clay minerals in sandstones:a review of the data and controls.International Association of Sedimentologists.Special Publication,34:63-91.
Noh,J.H.,and Lee,I.,1999.Diagenetic pore fluid evolution in the Pohang Miocene sediments:oxygen isotopic evidence of septarian carbonate concretions and authigenic mineral phases.Geosciences Journal,3(3):141-149.
Northrop,D.A.,and Clayton,R.N.,1966.Oxygen-isotope fractionations in systems containing dolomite.Journal of Geology,74:174-196.
Sample,J.C.,Torres,M.E.,Fisher,A.,Hong,W.,Destrigneville,C.,Defliese,W.F.,and Tripati,A.E.,2017.Geochemical constraints on the temperature and timing of carbonate formation and lithification in the Nankai Trough,NanTroSEIZE transect.Geochimica et Cosmochimica Acta,198:92-114.
Santos Jr,A.E.de A.,Rossetti,D.de F.,and Murray,H.H.,2007.bOyr iδg1i8nOs oafn tdhδe DR iaon aClyaspeism.Akapoplliineidt eCs l(anyo rStchieernnc eB,r3a7z(ils)3 r-e4v):e a2l8e1d-294.
Savin,S.M.,and Epstein,S.,1970.The oxygen and hydrogen isotope geochemistry of clay minerals.Geochimica et Cosmochimica Acta,34:25-42.
Savin,S.M.,and Lee,M.,1988.Isotopic studies of phyllosilicates.Michigan,Bookcrafter Inc.,Michigan,MI,189-223.
Schfoarumblaet,i o nE.,o f G13hCos-1h8,O P b.,o nadnsd i nE iclaerr,b oJn.aMte.,m2i0n0e6r.a l sP,r eesfteirmenattieadl using first-principles lattice dynamics.Geochimica et Cosmochimica Acta,70(10):2510-2529.
Schmidt,M.,Xeflide,S.,Botz,R.,and Mann,S.,2005.Oxygen isotope fractionation during synthesis of CaMg-carbonate and implications for sedimentary dolomite formation.Geochimica et Cosmochimica Acta,69(1):4665-4674.
Sheppard,S.M.F.,and Gilg,H.A.,1996.Stable isotope geochemistry of clays.Clay Mineral,31:1-24.
Siebel,W.,Reitter,E.,Wenzel,T.,and Blaha,U.,2005.Sr isotope systematics of K-feldspars in plutonic rocks revealed by the Rb-Sr microdrilling technique.Chemical Geology,222(3):183-199.
?liwiński,M.G.,Kitajima,K.,Kozdon,R.,Spicuzza,M.J.,Fournelle,J.H.,Denny,A.,and Valley,J.W.,2015.Secondary IAonn k eMriatse,s SPpaerctt r Io:m eδt1r8yO B iaMsa torinx I sEotffoepcet s.R a tGioeso sitna nDdoalrodms i te&-Geoanalytical Research,40(2):173-184.
?liVwiańllsekyi,,J.MW.G.,.,2 0K1o6.z dMoni,c r oRa.,n a lKyistiasj i omf a,c a rKb.,o n aDtee n cney,m eAn.t,δa18nOd in a CO2-storage system seal:Insights into the diagenetic history of the Eau Claire Formation(Upper Cambrian),Illinois Basin.AAPG Bulletin,100(6):1003-1031.
Smalley,P.C.,Stijfhoom,D.E.,1989.Raheim A.,Johansen H.,and Dickson J.A.D,1989.The laser microprobe and its application to the study of C and O isotopes in calcite and aragonite.Sedimentary Geology,65(3-4):211-221.
Suess,E.,and Whiticar,M.J.,1989.Methane-derived CO2 in pore fluids expelled from the Oregon subduction zone.Palaeogeography Palaeoclimatology Palaeoecology,71(1-2):119-136.
Tran,M.D.,Liu,J.,Li,X.,and Dang,M.C.,2016.Geology,fluid inclusion and isotopic study of the Neoproterozoic Suoi Thau Copper Deposit,Northwest Vietnam.Acta Geologica Sinica(English Edition),90(3):913-927.
Tian,Hui,Li,Huaikun,Liu,Huan,Zhang,Jian,Zhou,Hongying,Zhang,Kuo,Xiang,Zhenqun,Qu,Lesheng and Wang,Zhixian,2018.Characteristics of C and O isotopes of the Shennongjia Group in the northern margin of the Yangtze Craton and their constraints on paleoenvironment and depositional age.Acta Geologica Sinica,92(12):2508-2533.(In Chinese with English abstract)
Urey,H.C.,1947.The thermodynamic properties of isotopic substances.Journal of the Chemical Society,562.
VasBceornncaeslcoosn,i,C.,S.MM.,cKe2n0z0i5e.,J.CAa.l,ib r atWioarnth moafnn,t heR.,δa18nOd paleothermometer for dolomite precipitated in microbial cultures and natural environments.Geology,33:317-320.
Wang,Darui,2000.Stable Isotope Geochemistry of Petroleum.Beijing,Petroleum Industry Press,22-23.(In Chinese)
Wesnernpeer,n t inDi.zBa.t,io na n dof Tualtyrlaorm,a f iHc.Pr.,ock1s97b1.a s eTde muppeorna tu1r8eOs/1 6oOf fractionation between coexisting serpentine and magnetite.Contributions to Mineralogy and Petrology,32(3):165-185.
Williams,L.B.,Hervig,R.L.,and Bj?rlykke,K.,1997.New evidence for the origin of quartz cements in hydrocarbon reservoirs revealed by oxygen isotope microanalyses.Geochimica et Cosmechimica Acta,61(12):2529-2538.
Woo,K.S.,and Khim,B.K.,2006.Stable oxygen and carbon isotopes of carbonate concretions of the Miocene Yeonil Group in the Pohang Basin,Korea:types of concretions and formation condition.Sedimentary Geology,183(1):15-30.
Worden,R.H.,Smalley,P.C.and Oxtoby,N.H.,1996.The effects of thermochemical sulfate reduction upon formation water salinity and oxygen isotopes in carbonate gas reservoirs.Geochimica et Cosmechimica Acta,60(20):3925-3931.
Xi,K.,Cao,Y.,Jahren,J.,Zhu,R.,Bj?rlykke,K.,Haile,B.G.,Zheng,L.,and Hellevang,H.,2015.Diagenesis and reservoir quality of the lower cretaceous quantou formation tight sandstones in the southern Songliao basin,China.Sedimentary Geology,330(C):90-107.
Xi,K.,Cao,Y.,Zhu,R.,Haile,B.G.,and Hellevang,H.,2016a.Evidences of localized CO2-induced diagenesis in the Cretaceous Quantou Formation,southern Songliao Basin,China.International Journal of Greenhouse Gas Control,52(C):155-174.
Xi,K.,Cao,Y.,Haile,B.G.,Zhu,R.,Jahren,J.,Bj?rlykke,K.,Zhang,X.,Hellevang,H.,2016b.How does the pore-throat size control the reservoir quality and oiliness of tight sandstones?The case of the Lower Cretaceous Quantou Formation in the southern Songliao Basin,China.Marine and Petroleum Geology,76:1-15.
Xiao,Wanfeng,Liu,Hong,Li,Guangming,Huang,Hanxiao,Ma,Dongfang,Zhang,Zhilin,Yan,Guoqiang and Zhang,Hong,2017.Low to moderate temperature,low salinity and enrichment of CO2 hydrothermal fluid at Shangxu orogenic gold deposit in Shuanghu,Northern Xizang(Tibet):Evidence from fluid inclusions,H-O isotopic composition.Geological Review,63(3):793-808(in Chinese with English abstract)
Yang,W.,Hu,S.,Zhang,J.,Hao,J,and Lin,Y.,2015.NanoSIMS analytical technique and its applications in earth sciences.Science China(Earth Science),58(10):1758-1767.
Yeh,H.W.,1980.D/H ratios and late stage dehydration of shales during burial.Geochimica et Cosmechimica Acta,44(2):341-352.
Zhang,X.,Su,Z.,and Gao,Y.,2017.Zircon U-Pb Geochronology and geochemistry of the early Cretaceous volcanic rocks from the Manitu Formation in the Hongol Area,Northeastern Inner Mongolia.Acta Geologica Sinica(English Edition),91(4):1286-1304.
Zheng,Jianfeng,Li,Jin,Ji,Hancheng,Huang,Lili,Hu,Anping and Ma,Mingxuan.,2017.Clumped isotope thermometry and its application in dolomite reservoir:A case study of the Middle-Lower Cambrian in Traim Basin.Marine Origin Petroleum Geology,22(2):1-7.(In Chinese)
Ziegler,K.,Sellwood,B.W.,and Fallick,A.E.,1994.Radiogenic and stable isotope evidence for age and origin of authigenic illites in the Rotliegend,Southern North Sea.Clay Minerals,29(4):555-565.
Zhu D.Y.,Liu,Q.Y.,JIN Z.J.,Meng,Q.Q.,and Hu,W.X.,2017.Effects of deep fluids on hydrocarbon generation and accumulation in Chinese petroliferous basins.Acta Geologica Sinica(English Edition),91(1):301-319.
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