简介：TheCandHisotopiccompositionsofthemethaneinmorethan160gassamplesfrom10basinsinChinaarepresentedinthispaper.Thenaturalgasesareclassifiedasfourtypes:biogenicgas,bio-thermocatalytictransitionalgas,gasassociatedwithcondensateoil,andcoal-typegas.Theisotopiccompositionsofthesegasescloselyrelatedtothedepositionalbasins,thetypesoforganicmatter,thestagesofthermalevolutionandthegeneticcharacteristicsofdifferentgasreservoirs.StudiesoftheCandHisotopiccompositionsofterrigenousnaturalgaseswillprovidevalua-bleinformationontheprospectinganddevelopmentofnaturalgasesofdifferentgenetictypes.

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简介：Kaolinite(anddickite)isdioctahedral1:1layersilicate.Owingtotheinfluenceofdifferentgeologicalconditionsonthemineralduringandafteritsformation,naturalkaolinite,ingeneral,possessesdifferentdegreesofinternalstructuralorder.PlanconandTchoubar(1977a,1977b),Tchoubaretal.(1982)establishedthattheprinci-paltypeofdisorderinnaturalkaoliniteisthedisplacementofthevacantoctahedral

简介：Oil-gasremotesensinginformationisobtainedfromsatelliteTMdatathroughgraphictreatmentinthelightofthehydrocarbon-microseepagetheory.Theninetargetareas(ofthreetypes)selectedonthisbasisconcidewellwiththeoccurrenceofnaturalgasesandhavebeenprovedbysubsequentprospecting.Plantsinthetargetgreasarecharacterized.asaresultofhydrocarbon-microseepage,byabnormalspectralfeatureswiththeabsorptionpeaksofchlorophyllshiftingtowardbluelight,reflectivityintherangeofvisiblelightincreasingandreflectivityinthenearinfraredregiondecreasing.

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简介：Onthebasisofthecarbonisotopiccompositionsofmethane(CH4)anditshomologuesandthedifferencesinisotopicvaluesforCH4andethane(C2H6)andthecorrelationandcompositionalchar-acteristicsofhydrocarbongases,theauthorhasproposedageneticclassificationofnaturalgasesintheoil-gaszone.Theyareclassifiedasbiogeneticandabiogeneticgasesintermsofthetypesofhydrocarbon-generatingprecursors(orparentmaterials)andtheirthermalevolutionstages.Biogeneticgasescanalsobefurtherdividedintotwoseries:biochemicalandthermochemicalgases,withthelat-terformedatdifferentevolutionstages.Gasesgeneratedfromtype-Iand-II1organicmatterarecalledoil-seriesgases,thosefromtype-III,coal-series,andthosetype-II2,mixture-typegases.Gasesgeneratedfromtwoormorethantwotypesofprecursorsarecalledmixture-sourcegases.Accordingtothosementionedabove,naturalgasesfromthemajoroil-gaspoolsintheSichuanBasinhavebeendiscriminantlyanalyzed,andtheresultsareconcordantwiththedistributionandde-velopmentofhydrocarbon-sourcerocksaswellaswiththeircharacteristics,indicatingaprospectiveapplication.

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简介：中央煤气的地是在中国的Ordos盆的一块著名的大尺寸的煤气的地。然而，在这气体的奥陶纪水库的主要煤气的来源的鉴定回答遗体思索。根据天然气上的很多geo化学的数据和地质的研究，从奥陶纪的天然气的特征和来源在Ordos盆在中央煤气的领域里捱过外壳水库被学习。结果显示从在中央气体的捱过的外壳水库在Ordos盆回答的奥陶纪的天然气有类似的化学药品和同位素组成到高度成熟、在成熟上的干燥气体。导出煤的气体和油类型气体在Ordos盆在中央煤气的领域里共存。前者从更低的古生代的海洋的碳酸盐主要从含碳二叠的煤措施和后者被导出。当油类型气体可以在Ordos盆主要在中央煤气的领域的北、西方、南部的部分被生产时，导出煤的气体发生在中央煤气的领域的东方部分，这被建议。

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简介：HavingstudiedthebiomarkercompositionandmaturityofdissolvedhydrocarbonsfromOrdovicianformationwaters,theauthorspresentedmoleculargeochemicalevidenceforthecontroversialoriginofnaturalgasesincentralOrdosBasin.ThedissolvedhydrocarbonsinWellShan12andWellShan78arerelativelyhighinabundanceoftricylicterpane,pregnaneseriesanddibenzothiopheneseriesandlowinPr/Ph(＜2)andhopane/steraneratios,indicatingthesourceinputofmarinecarbonates.Incontrast,thedissolvedhydrocarbonsinWellShan81arefreefromtricyclicterpaneandpregnaneseries,withtracedibenzothiopheneseriesandhighPr/Ph(3.27)andhigherhopane/steraneratios,whicharethetypicalfeaturesofterrestrialorganicmatter.Furthermore,WellShan37andWellShan34arebetweenthetwosituations,havingamixedsourceofmarinecarbonateandterrestrialorganicmatter.Thematurityofbiomarkersalsosupportstheabovesuggestions.Theseresultsareconsistentwiththegeologicalbackgroundandsourcerockdistributioninthisregion.

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简介：有CO2的高内容的天然气水池在探索Hailar-Tamtsag盆的中间的差错地区期间被发现。到目前为止有有碳同位素的特征的CO2的这种煤气的水库是特殊的。在学习区域的CO2的稳定的碳同位素与13$C_是相对轻的{CO_2}$C_{CO_2}价值从13.1～8.2。联系的氩气体的40Ar/36Ar价值从916～996，与1.201.26的R/Ra。基于全面分析，在这个学习区域的CO2气体具有外壳披风来源，这被相信。

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