20660.富黃探區(qū)西部長6儲層特征研究

1、西安石油大學(xué)碩士學(xué)位論文富黃探區(qū)西部長6儲層特征研究姓名：崔建軍申請學(xué)位級別：碩士專業(yè)：石油與天然氣工程指導(dǎo)教師：趙永剛王念喜20121110Subject：Speciality：Name：Instructor：ResearchonCharacteristicsofChang6SectioninWestFuxian—HuanglingExplorationAreaPetroleumandnaturalgasengineeringCuiJ

2、ianjun(signatu№》乙五‘2疊兇業(yè)ZHaoYonggang(signature)ABS’l’RACrl’FuxianHuanglingexplorationarea，mainbodyinShaanxiprovinceislocatedinthesouthofYanancityinFuxianandHuanglingxianInthearealstruture，ItislocatedinErdosBasininthesouth

3、ernpartofthenorthernShaanxi、SslopeInthisarticletheresearchareaofFuHuangprospectingarea、swestern，Huai6一Huangcan38isthefocusarea，thelocaldevelopmentofnoseupliftNowwiththeFuHuangprospectingareainwesternHuai6Huangcan38wellfi

4、eldofpetroleumprospectingobtainsmajorbreakthrough，havemoreattractedattentionInthisthesis，usingstratigraphysedimentologypetrologyreservoirgeologypetroleumgeologyandotheraspectsofthetheoryandresearchofevaluationtechnique，b

5、asedonthestatic，dynamicandanalysisandtestdatatodevelopFuHuangprospectingarea、swesternChang6reservoircharacteristicresearchThroughtheresearchofChang6sectionofsubfaciesdivisionandcorrelation，furtherresearchshowsthattheChan

6、g6sectionofdeltafrontsubfaciesblockheavybeddedsandbodyupgrowth，locallyformeddeltafrontunderwaterslumpturbiditefan，middlefandevelopmentischaracteristicofit，Chang61，Chang62，Chang63threesubgroupsofsedimentaryfaciesplanedist

7、ributionfeaturesarebasicallysimilar；reservoirsandstoneismainlychondroarcoseandaverysmallamountofchondrosyrosemarcose，itscompositionalmaturityandtexturalmaturitywaslowmechanicalcompactionandcementationreducestheporositype

8、rmeabilitydissolutionimprovereservoirphysicalpropertymetasomatismofthereservoirhaslittleeffectonoverallReservoiraverageporosityis78％，themeanpermeabilityofO33x10‘jlam2，belongstoultralowporosityandultralowpermeablesublayer

9、fromChang63Chang62toChang61，propertyhasanoverallgoodtrend；Thereservoirmainporetypeshasintergranularpore，feldspathicdissolvedpores，detritaldissolvedporeandmicrofracturePoreouscombinationfrommiddletosmallandfromfinetotinyt

10、hroatmainly；Thechang6ofeachsubgroupissimilarbetweenheterogeneity；TheChang6innortheastsorthwestandnorthwestsortheasttothefracturesaremostdeveloped，andthemaindevelopmentoftectonicmicrofracture；TheChang6reservoirfourpropert