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1、分類號(hào):——密級(jí):——單位代碼:!鰻2Z學(xué)號(hào):2QQ壘!Q!緞西北大學(xué)博士學(xué)位論文題目:郢巫璽蚯坌地土直生晝沉塑住丕及濁氫宣塞趣徨班塞指導(dǎo)教師:奎塞厘專業(yè)技術(shù)職務(wù):數(shù)援學(xué)科(專業(yè)):濁氫圈地廈皇玨筮答辯日期:星QQZ生魚學(xué)位授予日期:二0O七年六月ResearchonsedimentarysystemsandhydrocarbonsenHchmentoftheUpperPalaeozoicoftheOrdosBasinAbstractA

2、imingatthesubtlegasreservoirscharacteristicoflowporelowpermeabilitylowabundanceandlargeareasdistributionoftheupperPaleozoicinO/dosbasin。inthewayofstudyingtypicalgasreservoirsintheclueofthehighbanefieialreservoirdistribut

3、ionandgasmigrationandonthe鯽phasisofgasreservoirdistributionandhighpermeabiliv/reservoirgenerationandaccumulationregulation,thepaperisbasedontheexistingresearchdatacombinedwiththen哪theoryandprogressofthesedimentologyseque

4、ncestratigraphyreservoirsedimentologypetroleumgeologyereandanalyzessystematicallygeologicalcondition,accumulationmodelhigIlboneficiaIreservoirformationmechanicsdistributionregulationofthelithologicai北servo弧andpointstheva

5、lidexplorationOnthebasisofstratigraphieclassificationandcomparisonstudythestratafromBenxiformationtoIaterShiheziformationwasdividedintotwoIOKlersequences(supertermstratigraphiebaselevelcirele)andeightIIord盯sequences(midd

6、letermslratigraphiebaselevelcirclc),and22IllordersequencesmiddlecyclescouldbeendividedintomanyshortcyclesBasedonthesequencesofsedimentarycharacteristic,theUpperPaleozoiccoulddistinguish3sedimentarysystemgroup8sedimentary

7、system(faeies),22subfaciesand40microfaeiesanddisemseddetaillytheehameteristicofallkindsoffaciessubfaeiesandmierofaciesandspatiotempomldistributionofthemBasedonanalyzingtheregionalgeologicbackground,imlaeocurnmtdirectionl

8、ightmineral,heavymineraisrocktraceelemantcharacteristicstheauthorconcludedthattherehadthreepI譏arysedimentaryprovenancesinnorthandfouxprimarysedimentaryprovenancesinsouthemOrdnsBasinandputforwardthenewviewpointthatthewest

9、provenancebegantosupplysinceHe一8stageFurthermoretheauthorconsideredthatthestructuralattributecharactersofthesouthandnorthsedimentaryoriginswG目reevidentlydifferentbyutilizingtherockgeochemicalcharaeteristicstoanalyzestruc

10、tumlehameteristiesofsedimentaryoriginsWhereaReranalyzingthepalaeogeograpbyandevolutionofOrdosBasinindifferentperiodsinneopaleozoic,theauthorgainedthenewstandpointsthattheredevelopedthefandeltasinnorthinearlypermianandthe

11、highconstructivebraidedriverdeltainlIe8stageandthoughtthatmainlvdevelopedthreecoalformingmodeIsofthebarriercoastriver(or(Iel協(xié)plain)andthetidaldelta11磚SOUl口CerocksofUpperPalcozoichadgasformingcentersinwestandeastofOrdnsBa

12、sin11聆gasaccumulationmodelswas‘widelycovered”coalfⅢrnedgasreservoirthathadcontinuousgasgeneratingcapaeityandthegasgenerationpeakofgasgenerationintheeastern撇isearlierthanthatin血ewcstan硼魂The陀sefvoirrockbodieshadthreepetrol

13、ogiccharacteristicthatwe糟highcolltelll$offillingmateriaIshi曲compositionalmaturityandlowtexturalmaturityn幅reservoirqualitywasmainiycontrolledbyprovenancesandsedimentaryfaciesmmainlyreservoirtyp髂hadtypeI、Ⅱ、ⅢandIVandthetype

14、IIandIliweretheprimaryreservoirtypesThehighteffectivereservoirmainlydevelopedinc∞怫gramgravelbearingcoarsegrainedandmediumcoarsequartzsandstonethatdepositedbyhighenergywaterchanneIsandmainlyappearedinthesubsequeneecycleso

15、frapidmaril把(1a蛐transgressiontooscillatingrear1ake)transgressionsandregressions(progradationsandbody),andtorelativeinactiveperiodoflowstandsystemtlaetsporeassemblagetypesmainlyweretheintergranularpores帆theiI】恤卿ularporesd

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