簡(jiǎn)介：分類號(hào)分類號(hào)P61813016181301密級(jí)級(jí)公開UDCUDC單位代碼單位代碼104240424學(xué)位論文鄂爾多斯盆地姬塬地區(qū)長(zhǎng)鄂爾多斯盆地姬塬地區(qū)長(zhǎng)45、長(zhǎng)、長(zhǎng)6儲(chǔ)層地質(zhì)學(xué)研究?jī)?chǔ)層地質(zhì)學(xué)研究代磊申請(qǐng)學(xué)位級(jí)別申請(qǐng)學(xué)位級(jí)別碩士學(xué)位碩士學(xué)位專業(yè)專業(yè)名稱稱礦產(chǎn)普查與勘探礦產(chǎn)普查與勘探指導(dǎo)教師姓名指導(dǎo)教師姓名柳益群職稱稱教授山東科技大學(xué)二○○○○六年五月六年五月GEOLOGICALSTUDYONCHANG45ANDCHANG6RESERVOIRSINJIYUANAREAOFORDOSBASINMASTEROFENGINEERINGFROMSHANDONGUNIVERSITYOFSCIENCEANDTECHNOLOGYBYDAILEISUPERVISORPROFESSORLIUYIQUNCOLLEGEOFGEO-INFOSCIENCEANDENGINEERINGMAY2006

簡(jiǎn)介：分類號(hào)N0210710～06111124諼步夫海碩士學(xué)位論文導(dǎo)師姓名職稱申請(qǐng)學(xué)位級(jí)別論文提交日期學(xué)位授予單位地質(zhì)學(xué)中的真?zhèn)沃嫘炖^山段聯(lián)合教授答辯委員會(huì)主席學(xué)位論文評(píng)閱人芮夕捷鄔煜劉強(qiáng)ABSTRACTHEIDEGGERSAID，”THEUNDERSTANDINGTOTHEEXISTENCEISTHEPROVISIONSOFDASEIN’SEXISTENCEINITSELF’’THEEXISTENCEISNOTREALISTIC’’REAL”BUTTHENEVERENDINGTHOUGHTTOEXISTMANIS”DASEIN”WHATPEOPLEUNDERSTANDINTHEGEOLOGICALOBJECTCONSTITUTESTHEEXISTENCEOFTROTHOFGEOLOGYTHEDISTINCTIONBETWEENTRUTHANDFAULTISTHECORNERSTONEOFTHEFIRSTSTEPTOUNDERSTANDTHEEXISTENCEOFGEOLOGYFIRSTOFALL，WHATISTHEPROBLEMOFTHETRUTHANDFAULTINGEOLOGYTAKINGAPANORAMICVIEWOFGEOLOGYHISTORYMOREORLESSITHASGOTHROUGHTHETHREESTAGESTHESIMPLE，THECLASSICANDTHEMODEMGEOLOGYTHEPROBLEMSREFLECTTHEPLIGHTINTERMSOFTHEINTERNALDISCIPLINESOFGEOLOGYTHEYARETHEDIFFICULTIESOFGEOLOGICALDEVELOPMENTBUTINTHEEXTERNALOFTHEOBJECT，THEYARETHEDIFFICULTIESOFGEOLOGICALEVALUATIONTOCLARIFYTHETRUTHORFAULTFROMGEOLOGYISTHEBASISOFGEOLOGYANDGEOLOGICALEVALUATIONANDGEOLOGICALDEVELOPMENTCONSTITUTETHEPROBLEMSOFGEOLOGYSECOND，AFTERANSWERINGWHATTHEPROBLEMISTHEARTICLECONTINUESTOSTUDYTHETHEPROCESSOFTRUTHANDFAULTTHENATUREOFEXPLORATIONLEDTOTHEFACTTHATITISONLYSEEKINGTRUTHFROMTHEFAULT；THENATUREOFTHEHYPOTHESISLEDTOTHETHEORYTHATITISONLYCLOSINGTOTHETRUTHANDSTAYINGAWAYFROMFAULT；THENATUREOFTHINKINGLEDTOTHEMETHODTHATITISNOTONLYTOWARDSTHETRUTHBUTALSOFAULTFINALLYHOWDOESITSOLVETHEPROBLEMTHEARTICLEHASALWAYSBEENHOLDTHEDIALECTICALRELATIONSHIPBETWEENTHETRUTHANDFAULTINFACT，THEDISPUTELULLSTHROUGHTHEWHOLEDEVELOPMENTOFGEOLOGYTHETRUTHOFPLUTONISMHASREFUTEDTHEFAULTOFNEPTUNISMTHETRUTHOFUNIFORMITARIANISMHASREFUTEDTHEFAULTOFCATASTROPHISMTHETRUTHOFINFLATIONHYPOTHESISHASREFUTEDTHEFAULTOFCONTRACTIONHYPOTHESISTHETRUTHOFMOBILISMHASREFUTEDTHEFAULTOFFIXISMISITTHEIRREFUTABLETROTHSCIENCE，ESPECIALLYGEOLOGYHASCHANCETODEVELOPANDEVOLVEINTHEREFUTABILITYTHEDEVELOPMENTOFTHEGEOLOGYCANBESEENASTHEEXPLORATIONTHETRUTHOFTHEGEOLOGICALFACT，ACQUIREMENTTHETRUTHOFTHEGEOLOGICALTHEORYANDTHEESTABLISHMENTTHETRUTHOFTHEGEOLOGICALTHINKINGHOWEVERTHEPROBLEMOFTHEGEOLOGYISNOTRESOLVEDBYITSELFANDITNEEDTOUSETHEPHILOSOPHYOFSCIENCEANALYSISBETWEENTHETRUTHANDFAULTOFTHEGEOLOGYHASGREATTHEORETICALANDPRACTICALSIGNIFICANCEINNURTURINGASCIENTIFICBELIEFTHESPIRITOFSCIENCEANDTHEQUALITYOFSCIENCEKEYWORDSGEOLOGY；TRUTH；FAULT；FACT；THEORYTHINKINGH

簡(jiǎn)介：研究生畢業(yè)論文（全日制學(xué)術(shù)型碩士申請(qǐng)學(xué)位全日制學(xué)術(shù)型碩士申請(qǐng)學(xué)位）論文題目論文題目贛中城上復(fù)式巖體年代學(xué)和地球化學(xué)特征及其地質(zhì)意義學(xué)位申請(qǐng)人學(xué)位申請(qǐng)人沈滔專業(yè)名稱專業(yè)名稱地質(zhì)學(xué)研究方向研究方向地球化學(xué)指導(dǎo)教師指導(dǎo)教師陳正樂（研究員）2016年06月20日

簡(jiǎn)介：分類號(hào)P54107102012127047碩士學(xué)位論文東昆侖南緣東段可可爾塔地區(qū)蛇綠巖與相關(guān)火山巖地質(zhì)特征、年代學(xué)及構(gòu)造環(huán)境研究東昆侖南緣東段可可爾塔地區(qū)蛇綠巖與相關(guān)火山巖地質(zhì)特征、年代學(xué)及構(gòu)造環(huán)境研究王元元導(dǎo)師姓名職稱裴先治教授申請(qǐng)學(xué)位級(jí)別理學(xué)碩士學(xué)科專業(yè)名稱構(gòu)造地質(zhì)學(xué)論文提交日期2015年4月9日論文答辯日期2015年6月2日學(xué)位授予單位長(zhǎng)安大學(xué)

簡(jiǎn)介：分類號(hào)P588．1密級(jí)公開學(xué)校代碼‘10697學(xué)號(hào)201420986▲曠DIP歹C尢N(yùn)ORTHWESTUNIVERSITY學(xué)科名稱礦物學(xué)、巖石學(xué)、礦床學(xué)作者李桐指導(dǎo)老師秦江鋒副教授西北大學(xué)學(xué)位評(píng)定委員會(huì)二。一七年帆3㈣瓢㈣埔㈣引㈣摘要摘要北秦嶺地體位于洛南．欒川斷裂帶和商丹縫合帶之間，是秦嶺造山帶重要的構(gòu)造單元之一。古生代花崗巖記錄了北秦嶺商丹洋演化的重要信息，前人研究成果表明，北秦嶺早古生代花崗質(zhì)巖漿作用可以分為俯沖505～470MA、同碰撞450422MA和后碰撞415～400MA三個(gè)演化階段，但區(qū)域上400MA左右商丹洋碰撞后形成花崗巖體的研究資料相對(duì)薄弱，這些花崗巖成因研究對(duì)探討商丹洋碰撞后地殼物質(zhì)熔融機(jī)理及北秦嶺基底的性質(zhì)等科學(xué)問題具有重要意義。本文主要選取丹鳳地區(qū)商丹縫合帶北側(cè)出露的晚古生代大房溝巖體、兩岔河巖體、窯溝巖體和鐵峪鋪巖體作為研究對(duì)象，對(duì)其進(jìn)行全巖主微量、SRND同位素、礦物化學(xué)、鋯石U。PB年代學(xué)和鋯石HF同位素方面的研究，厘定晚古生代花崗質(zhì)巖漿作用的期次，研究巖漿源區(qū)性質(zhì)及地殼物質(zhì)部分熔融機(jī)理，最后結(jié)合區(qū)域地質(zhì)研究花崗質(zhì)巖漿形成的深部動(dòng)力學(xué)背景。主要取得以下幾方面的認(rèn)識(shí)鋯石UPB年代學(xué)研究表明，北秦嶺晚古生代四個(gè)花崗巖體應(yīng)分為兩期，第一期約在440MA左右，以文中鐵峪鋪巖體為代表，其鋯石加權(quán)平均年齡為438士1．8MA；第二期約在400MA左右，以文中大房溝、兩岔河和窯溝巖體為代表，其中大房溝巖體加權(quán)平均年齡為404．1士2．7MA，兩岔河巖體加權(quán)平均年齡為405．82．8MA，窯溝巖體加權(quán)平均年齡為403士2MA。鐵峪鋪巖體主要由黑云母花崗閃長(zhǎng)巖組成，其SI0269．1％～70．1％，NA204．8％～5．51％，A120315．7％～15．O％，NA20／K20I．9～2．26，為準(zhǔn)鋁質(zhì)一弱過鋁質(zhì)系列，A／CNKI．04～1．10，表現(xiàn)出I型花崗巖的特征；巖石稀土總量較低∑REE55．4～60．8PPM，具有正的EU異常6EU1．04～1．10，其高的SR／Y比值，表現(xiàn)出類似于埃達(dá)克巖漿特征；巖石具有相對(duì)富集的SRND同位素組成，其ENDT值介于一0．6～0．3之間，鋯石￡HFT值變化范圍為2．65到12．89之間；巖石鋯石飽和溫度中等732～739。C，綜合分析其應(yīng)為富斜長(zhǎng)石的新生基性下地殼發(fā)生脫水部分熔融的產(chǎn)物，巖石源區(qū)可能有少量富集組分的加入，導(dǎo)致其相對(duì)富集SRND同位素特征。大房溝巖體主要由黑云母二長(zhǎng)花崗巖組成，SI02含量介于68．4％“71．7％之間，NA204．18％～5．59％，NA20／K201．07“2．74，A1203含量介于15．6％～17．9％之間，為準(zhǔn)鋁質(zhì)一弱過鋁質(zhì)鈣堿性巖系列，具富集的SRND同位素組成￡ND∞一10。4和較低的稀土總量ZREE52．690．4PPM，表現(xiàn)出S型花崗巖特征，8EU0．731．23，鋯石HF同位素比值￡HR0變化于．9．35一0．25之間；巖漿形成溫度最低662～721℃，綜合分析，大房溝二長(zhǎng)花崗巖應(yīng)為古．中元古代古老中上地質(zhì)殼物質(zhì)發(fā)生脫水部分熔融的產(chǎn)物。T

簡(jiǎn)介：|』學(xué)校代碼10425I學(xué)號(hào)S0401056中國(guó)石油大學(xué)碩士研究生學(xué)位論文華東申請(qǐng)工學(xué)碩士學(xué)位常用地質(zhì)統(tǒng)計(jì)學(xué)方法軟件開發(fā)及分析學(xué)科專業(yè)培養(yǎng)方向碩士生指導(dǎo)教師礦產(chǎn)普查與勘探含油氣盆地分析閆瑞萍李漢林教授入學(xué)月期2004年9月論文完成日期2007年5月THESOFTWAREDEVELOPMENTANDANALYRSISOFCOMMONGEOSTATISTICSYANRUIPINGMINERALRESOURCEPROSPECTINGANDEXPLORATIONDIRECTEDBYPROFESSORLIHANLINABSTRAETKRIGINGISANIMPORTANTMETHODINTHEPREDICTIONOFRESERVOIRPARAMETERRESPONSESRESERVOIRCHARACTERIZATIONANDISTHEBASISOFESTIMATINGRESERVES，PRODUCTIONPREDICTIONESTIMATINGRECOVERYEFFICIENCYANDEXPLORATIONANDDEVELOPMENTPROJECTTHISRESEARCHMETHODBETIMESALREADYHOTSPOTONTHEBASISOFREADINGLOTSOFDOCUMENTSOFGEOSTAFISTIES，USETHEIDEAOFSOFTWAREENGINEERING，STUDYTHESOFTWAREDESIGNANDDEVELOPMENTOFCOLNLNONGEOSTATISTICS，ANDSTUDYTHETASKS，PROCESS，STRUCTURINGMETHOD，TOOLSOFSOFTWARE，F(xiàn)ORMASERIESOFNECESSARYPICTURESANDDOCUMENTS，ESTABLISHTHEMODELSOFGEOLOGYOFVARIATIONFUNCTIONUNIVERSALGRIGING，INDICATORKRIGINGANDCOMIGINGTHENTESTTHESOFTWAREUSINGTHEREALGEOLOGYDATAVERIFYTHECREDIBILITYOFSORWARETHERESULTINDICATESINDICATORKRIGING’SESTIMATINGEFFECTIVENESSIMPROVESLITTLEWHENDIFFERENCEOFREGIONALIZEDVARIABLEISNOTREMARKABLE，BUTCOKRIGING’SESTIMATINGEFFECTIVENESSISBETTERTHANUNIVERSALKRIGINGANDINDICATORMIGINGUNIVERSALGAIGING，INDICATORKRIGINGANDCOKRIGINGCANREFLECTTHEPHYSICALPROPERTYANDCOKRIGINGSESTIMATINGEFFECTIVENESSISBESTAMONGTHESETHREEMETHODSWHENCORRELATIONOFCHIEFVARIABLEANDIII

簡(jiǎn)介：中山大學(xué)博士學(xué)位論文中國(guó)大陸科學(xué)鉆探（CCSD）HPUHP變質(zhì)巖中石英脈的地質(zhì)地球化學(xué)及成因姓名徐莉申請(qǐng)學(xué)位級(jí)別博士專業(yè)礦物學(xué)、巖石學(xué)、礦床學(xué)指導(dǎo)教師孫曉明20060508中山大學(xué)博士學(xué)位論文中國(guó)大陸科學(xué)鉆探CCSDHPUHP變質(zhì)巖中石英脈的地質(zhì)地球化學(xué)及成因徐莉綠輝石、白云母、方解石、鉀長(zhǎng)石和黃鐵礦等礦物包體，其中磷灰石包體中存在四類出溶物不規(guī)則狀的磁鐵礦和赤鐵礦的連生體A、針狀赤鐵礦B、板狀到菱型的獨(dú)居石C和針狀鍶重晶石D。其中A，B和D類出溶物是在磷灰石中首次發(fā)現(xiàn)。四類出溶物的長(zhǎng)軸和生長(zhǎng)方向均基本平行于磷灰石之C軸，顯示它們可能是基本同時(shí)出溶的；CCSDUHP巖石中氟磷灰石脈體的存在及其鐵氧化物、磷酸鹽和硫酸鹽出溶體的發(fā)現(xiàn)，顯示UHP巖石在折返的過程中，快速減壓曾造成礦物的分解和大量出溶體的形成，伴隨脫水和SI02等硅酸鹽熔體的出溶，還存在少量的磷酸鹽熔體，同時(shí)可能曾經(jīng)有鐵氧化物的熔漿的加入；2較系統(tǒng)的鏡下觀察并結(jié)合流體包裹體顯微測(cè)溫及激光拉曼分析，發(fā)現(xiàn)石英脈和水晶中存在5類流體包裹體I鹽水溶液包裹體，并進(jìn)一步分為中高鹽度鹽水溶液包裹體IA、中等鹽度鹽水溶液包裹體1B和低鹽度鹽水溶液包裹體IC；IINACLCACL2一H20體系包裹體；111N2一CH4體系包裹體；IV含方解石子晶的包裹體；V含烴類的有機(jī)包裹體。其中類和V類包裹體是CCSD鉆孔中榴輝巖石英脈中首次發(fā)現(xiàn)；初步的巖相學(xué)和顯微測(cè)溫研究顯示IA、LB和型流體包裹體主要以原生或假次生的形式賦存在榴輝巖的石英脈或石英顆粒中，它們?cè)诮情W巖相的片麻巖及其石英脈中均未觀察到，顯示它們可能主要被捕獲于榴輝巖的減壓重結(jié)晶或退變質(zhì)階段，而LC型包裹體分布廣泛，表明其主體可能是在超高壓變質(zhì)巖折返過程的最晚階段捕獲的；榴輝巖和片麻巖中石英脈流體包裹體的組成和地球化學(xué)特征存在明顯區(qū)別，但它們各自相似于其寄主巖石中的石英顆粒中包裹體，說明CCSD中HPUHP巖石在板塊折返過程中釋放出的變質(zhì)流體沒有經(jīng)過大規(guī)模的遷移；CCSD榴輝巖中石英脈的主體形成于板塊折返有關(guān)的減壓重結(jié)晶和退變質(zhì)，而片麻巖中石英脈則主要來源于角閃巖相及其后期退變質(zhì)作用；N2CH4純氣相包裹體主要呈孤立和小群狀與IA和IB類包裹體分布于榴輝巖中條帶狀石英脈中，可能主要是在高壓一超高壓榴輝巖相變質(zhì)條件下被捕獲的，說明了部分石英脈曾經(jīng)歷過超高壓變質(zhì)作用；在CCSD石英脈及地表水晶中發(fā)現(xiàn)含烴類有機(jī)包裹體，而且成熟度較低，表明有機(jī)質(zhì)沉積物埋藏沉積成巖過程中，隨著板塊發(fā)生俯沖，帶入地下深部，又隨板塊折返帶回地表，板塊發(fā)生了快速的俯沖和折返，有機(jī)質(zhì)還未來得及成熟演化；3石英脈和水晶中微量元素的RB／SR、NB／TA和ZFLHF變化較大，有的高于有的低于原始地幔相應(yīng)值，說明RB和SR、NB和TA、ZR和HF之間發(fā)生了不

簡(jiǎn)介：研究生畢業(yè)論文申請(qǐng)碩士學(xué)位申請(qǐng)碩士學(xué)位論文題論文題目贛江下游南昌段河流沉積物碎屑鋯石UPB年代學(xué)和LUHF同位素研究及其地質(zhì)意義學(xué)位申請(qǐng)學(xué)位申請(qǐng)人李小聰專業(yè)名稱地質(zhì)資源與地質(zhì)工程研究方向礦產(chǎn)普查與勘探指導(dǎo)教指導(dǎo)教師王安東2017年6月15日DISSERTATIONFMASTER’SDEGREEOFEASTCHINAUNIVERSITYOFTECHNOLOGYCOUPLEDUPBLUHFISOTOPICANALYSESOFDETRITALZIRCONSINTHESEDIMENTSFROMTHENANCHANGSECTIONOFGANJIANGRIVERDOWNSTREAMITSGEOLOGICALSIGNIFICANCEPOSTGRADUATELIXIAOCONGDISCIPLINEGEOLOGICALRESOURCESGEOLOGICALENGINEERINGDIRECTIONMINERALRESOURCEPROSPECTINGEXPLATIONMENTWANGONGJUNE2017NANCHANGPRCHINA

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簡(jiǎn)介：成都理工大學(xué)碩士學(xué)位論文基于地質(zhì)統(tǒng)計(jì)學(xué)的固體礦床儲(chǔ)量估算的研究與實(shí)踐姓名劉愛平申請(qǐng)學(xué)位級(jí)別碩士專業(yè)應(yīng)用數(shù)學(xué)指導(dǎo)教師郭科20090501成都理工大學(xué)碩士學(xué)位論文IITHERESEARCHPRACTICEOFSOLIDMINERALRESERVESESTIMATIONBASEDONGEOSTATISTICSINTRODUCTIONOFTHEAUTHLIUAIPINGMALEWASBNINAUGUST1982WHOSETUTWASPROFESSGUOKEHEGRADUATEDFROMCHENGDUUNIVERSITYOFTECHNOLOGYINAPPLIEDMATHMAJWASGRANTEDTHEMASTERDEGREEINJUNE2009ABSTRACTINRECENTYEARSWITHGEOSTATISTICSDEEPLYSTUDIEDWIDELYUSEDINCHINAITHASBEENMADEGREATPROGRESSINTHESOLIDMINERALRESERVESESTIMATIONCONDITIONALSIMULATIONNUMERICALANALYSISHASBEENWIDELYUSEDINTHEFIELDOFAGRICULTURALMETEOLOGICALENVIRONMENTALOILGASSOONINTHESOLIDMINERALRESERVESESTIMATIONITHASDEVELOPEDINTOTHEINDUSTRYSTARDFESTIMATINGRESERVESHASALSOPRODUCEDEXCELLENTRESEARCHRESULTSALARGENUMBEROFMATURESOFTWARESINTHISPAPERITFIRSTINTRODUCEDTHECONTENTSOFTHEGEOSTATISTICSITSADVANTAGESTOTRADITIONALMETHODSOFCALCULATINGMINERESERVESCLASSICALPROBABILITYSTATISTICSTHENITINTRODUCEDREGIONALVARIABLESVARIOGRAMTHETHEETICALMODELVARIATIONCURVESTRUCTURALANALYSISDINARYKRIGINGMETHODSOONINTHEPARTOFRESCEESTIMATIONITDIVIDEDTHEBODYOFJIAMADEPOSITINTOMANYUNITSOFCALCULATIONCONSIDEREDEACHUNITITEDAPPROPRIATEMETHODOFESTIMATIONFEACHUNITTOTHENO1UNITITINTRODUCEDHOWTOUSEKRINGMETHODTOESTIMATETHERESERVESINCLUDINGDATAANALYSISDATAPREPROCESSINGSPECIFICVALUEPROCESSINGDATAVISUALIZATIONVARIOGRAMKRIGINGESTIMATIONRESERVESCALCULATIONSOONINTHISSECTIONITINCLUDEDNOTONLYTHEESSENCEOFTHETHINKINGOFTHEKRIGINGINCLUDINGVARIOGRAMANALYSISKRIGINGVALUATIONETCBUTALSOGAVEADETAILEDEXAMPLECOMBINEDWITHTHECUDEPOSITITEDTHEAPPROPRIATEALGITHMCALCULATEDVARIATIONFUNCTIONDREWTHEFIGURESOFVARIATIONFUNCTIONINEACHDIRECTIONEDTHEPARAMETERSOFBLOCKMODELSTHENUNDERTHEMATLABPLATFMITESTIMATEDTHERESERVESOFCUMOFINALLYTHERESULTOFRESERVESCALCULATIONISRELIABLEBYCONTRASTINGITWITHTHERESULTOFRESERVESCALCULATIONWITHSDSOFTWAREINADDITIONCOMBINEDWITHTHEDEPOSITTHISPAPERGAVETHEFIGUREOFTHESPATIALDISTRIBUTIONOFDRILLHOLESTHESPATIALFMOFTHEMINETHEFIGUREOFTHREEDIMENSIONALSIMULATIONOFTHETERRAINSOONUNDERTHEMATLABKEYWDSRESERVESESTIMATESGEOSTATISTICSCUDEPOSIT

簡(jiǎn)介：長(zhǎng)安大學(xué)碩士學(xué)位論文應(yīng)用水文地質(zhì)學(xué)及其網(wǎng)絡(luò)CAI開發(fā)姓名李世龍申請(qǐng)學(xué)位級(jí)別碩士專業(yè)環(huán)境工程指導(dǎo)教師錢會(huì)20040101ABSTRACTSINCEITSNAISSANCEINTHEBEGINNINGOFTHE19“CENTURY，AFTERCONTINUOUSENRICHMENT，NOWHYDROGEOLOGYHASBECOMEAINTEGRATEDANDSYSTEMICSUBJECT．ANDOURCOUNTRYHASGONETHROUGHAGRADUALPROGRESSFROMSCRATCH，THERANGEOFRESEARCHINGHASEXPANDEDTOTHELARGESYSTEMOFGROUNDWATERSPHEREANDHYDROSPHERECONSISTEDOFRESOURCES、ENVIRONMENT、ZOOLOGY、TECHNOLOGY、ECONOMYANDSOCIETY；WHILETHECONTENTTURNEDTOTHEINTERSECTRELATIONSAMONGGROUNDWATERSYSTEM、ENVIRONMENTSYSTEMANDSOCIETYECONOMYSYSTEMAPPLIEDHYDROGEOLOGYISAVERYIMPORTANTBRANCHOFHYDROGEOLOGY，JUSTADVANCEDINRECENTFEWYEARS．BYNOW,ITISN’TCONSUMMATEANDNEEDMOREPROFESSIONALSTOMAKEFURTHERSTUDY．COMPUTERASSISTEDINSTRUCTIONCAIWHICHDEVELOPEDIN20。CENTURYISONEOFTHEHARDMEASURESTOREALIZETHEMODERNEDUCATION，BEINGUSEDINMANYSUBJECTSINANUMBEROFPRIMARYSCHOOLANDHIGHSCHOOL，EVENTHOUGHNROSTOFTHECOLLEGES．CAICANEMBODYWELLTHEPOLICYFOREDUCATIONOF‘‘THESTUDENTTAKESASTHEMAINBODY,WHILETHETEACHERTAKESASLEADINGFACTOR．‘’ITISABLETOPLAYAREMARKABLEROLEINTRAININGSTUDENTS’INITIATIVESPIRITANDCREATIVITY．AFTERDOZENSOFYEARS’PRACTICE，TURNSOUTAGOODTEACHINGRESULT．ESPECIALLYWITHTHEDEVELOPMENTOFCOMPUTERANDINTERNETTECHNOLOGYINRECENTYEARS，CAICOMBINEWITHTHEMULTIMEDIA、INTEMETANDINTELLIGENCETECHNOLOGY,MOSTOFSCHOOLSHAVESETUPDISTANCEEDUCATIONANDINTEMETCOLLEGEINSUCCESSION，OFFERINGAWIDERSTUDYPLATFORMFORPEOPLE，WHICHISAMAJORDIRECTIONOFTHEFUTUREEDUCATION，ANDHAVEABRIGHTPROSPECT．THISPAPERWILLDISCUSSTHEUNITEOFTHEFOREMENTIONEDTWOSIDES一APPLIEDHYDROGEOLOGYNETWORKCAICOURSEWARE，IT’STHEORIGINALINTENTIONTOSHOWNEWKNOWLEDGEINANEWFORM．THROUGHDISSERTATINGCURRENTSITUATIONANDTHEDEVELOPMENTTRENDOFNETWORKCAI，HAVEMADETHEDESIGNTRAINOFTHOUGHTOF{APPLIEDHYDROGEOLOGY}CAICLEARFURTHER,POINTEDOUTPRINCIPLESTHATSHOULDBEFOLLOWEDOFTHISNETWORKANDQUESTIONSTHATSHOULDBEPAIDATTENTIONTO．INTHECOURSEOFWRITINGTHESCRIPT，CONSULTEDALARGEAMOUNTOFDOCUMENTS，ICHOOSETHEBOOKOF{APPLIEDHYDROGEOLOGY}．WHICHISWRITTENBYC．拜FETTER,PREVAILEDANDUSEDEXTENSIVELYWITHINTHERANGEOFWORLDATPRESENT．ONTHEBASISOFTRANSLATINGANDPUTITINORDER，COMBINEDWITHRELEVANTTEACHINGMATERIALSANDCURRENTSITUATIONOFRESEARCHABOUTHYDROGEOLOGYOFOURCOUNTRY,HAVESUPPLEMENTEDIT，MADEITSUITTHEREALITYOFOUROWNCOUNTRYEVENMOREPAYATTENTIONTOTHELINKINGUPANDPIECINGTOGETHEROFCONTENTDURINGTHECOURSEOFPRODUCING，ANDCONVENIENTTOREAD，GOODINTEGRALITY，ALSOLIVELYANDTERSEFORMBYMAKINGANDUSINGLOTSOFMATERIALS，TURNEDOUTAVERYGOODRESULT．ANDTHISTOTALLYBENEFITSFROMTHECHOICEOFTHESUITABLESOFTWARE，WHATISELECTEDFORUSEISAUTHORING’

簡(jiǎn)介：內(nèi)蒙古農(nóng)業(yè)大學(xué)碩士學(xué)位論文地質(zhì)統(tǒng)計(jì)學(xué)在水文地質(zhì)參數(shù)空間變異性應(yīng)用中幾個(gè)問題的研究姓名王亮申請(qǐng)學(xué)位級(jí)別碩士專業(yè)水文學(xué)及水資源指導(dǎo)教師朝倫巴根20070501SEVERALPROBLEMSOFAPPLYINGGEOSTATISTICFORTHESTUDYONSPATIALVARIABILITYOFHYDROGEOLOGICPARAMETERSABSTRAOTTHEHYDROGEOLOGICPARAMETERSARETHEIMPORTANTPARAMETERSOFTHEGROUNDWATERRESOURCESASSESSMENTNUMERICALMODELINGIDENTIFICATIONON、INSPECTIONANDPREDICTIONHOWEVERITSTEMPORALANDSPATIALVARIABILITYISVERYHIGH勰INFECTEDBYTHEHYDROGEOLOGICCONDITIONANDEXPLOITATIONSOTHESTUDYOFSPATIALVARIABILITYONHYDROGEOLOGICPARAMETERSISVERYIMPORTANTFORINCREASETHEPRECISIONOFTHEGROUNDWATERRESOURCESASSESSLLLENTTHISPAPERISSUPPORTEDBYTHEPROJECTOF‘‘ASTUDYOFSCIENTIFICALLOCATIONOFWATERRESOURCESFORVEGETATIONCONSTRUCTIONINTHESANDYAREABETWEENBEIJINGANDINNERMONGOLIA’，DISCUSSINGSEVERALPROBLEMSOFAPPLYINGGEOSTATISTIEFORTHESTUDYONSPATIALVARIABILITYOFHYDROGEOLOGIEPARAMETERS，ANDUSINGTHEORDINARYIMGMGMETHOD、UNIVERSALKRIGINGMETHOD、COKRIGINGMETHODANDCOUNIVERSALKRIGINGMETHODTOSTUDYTHESPATIALVARIABILITYOFHYDROGEOLOGICPARAMETERSINTHESTUDYREGIONONTHEBASISOFTHEABOVERESUITTHEMAINCONTENTSOFTHEPAPERAREASFOLLOWS1THECHOICEOFTHELARGESCALE、NONLINEARANDUNEQUIDISTANTSAMPLINGNET2THESTUDYONTHESPATIALCORRELATIONOFTHEREGIONALIZEDVARIABLEANDCOREGIONALIZEDVARIABLE3THERELATIONBETWEENTHEHGDISTANCEANDTHEREASONABLENUMBEROFDATAPAIRWHENCALCULATINGTHEEXPERIMENTALVARIOGRAMINTHELARGESCALE、NONLINEARANDUNEQUIDISTANTSARAPTINGNET4THEOBTAINOFTHEVARIOGRAMOFNONSTATIONARYREGIONALIZEDVARIABLE5THESTUDYONTHEMETHODOFOBTAININGTHEROBUSTVARIOGRAM_6THEOBTAINANDAFFWMANEEOFTHETHEORETICALVARIOGRAM7THEEXAMPLEOFAPPLYINGORDINARYL【RIGINGMETHOD、UNIVERSALKRIGINGMETHOD、COKRIGINGMETHODANDCOUNIVERSALKRIG啦METHODTOSTUDYTHESPATIALVARIABILITYOFHYDROGEOLOGICPARAMETERSKEYWORDSKRIGINGMETHOD，SPATIALCORRELATION；HYDROGEOLOGICPARAMETERS；SPATIALVARIABILITYDIREOTEDBYPROFOHAOIUNBAGEN

簡(jiǎn)介：西北大學(xué)碩士學(xué)位論文秦嶺北麓現(xiàn)代河流碎屑鋯石UPB年代學(xué)研究及其地質(zhì)意義姓名張紅申請(qǐng)學(xué)位級(jí)別碩士專業(yè)礦物學(xué)、巖石學(xué)、礦床學(xué)指導(dǎo)教師孫勇20080604帶之南的碎屬記錄，因此物源復(fù)雜，我們可稱其為混合墅物源區(qū)。該區(qū)河流碎屑鋯石除保黧與前述北秦嶺構(gòu)造帶完全相同的記錄外，尚存在稀蔬的新太吉代2500MA和中元古代1600MA地質(zhì)記錄。推測(cè)這些記錄可能源竇商丹帶之南的南秦嶺基底。在本區(qū)河流分水嶺附近發(fā)育的佛坪巖群或長(zhǎng)角壩巖群有可能是其物源。關(guān)鍵詞北秦嶺構(gòu)造帶，河流碎屑鋯石，UPB年代學(xué)，物質(zhì)來源，地質(zhì)事件

簡(jiǎn)介：摘要對(duì)陜甘寧盆地、塔里木盆地以及長(zhǎng)江三角洲的部分沉積地質(zhì)學(xué)問題進(jìn)行了研究。主要內(nèi)容包括陜甘寧盆地新構(gòu)造活動(dòng)與地貌，塔里木盆地東部地區(qū)形變構(gòu)造系統(tǒng)及其構(gòu)造組合樣式，陜甘寧、塔里木盆地中上奧陶統(tǒng)薄互層泥、灰?guī)r沉積特征，趙老峪、平?jīng)鼋M遺跡化石與沉積環(huán)境，長(zhǎng)江三角洲晚第四紀(jì)地層生物成因的原生沉積構(gòu)造以及與地層結(jié)構(gòu)相關(guān)的環(huán)境地質(zhì)災(zāi)害等。主要認(rèn)識(shí)如下1陜甘寧盆地內(nèi)部新構(gòu)造活動(dòng)較為明顯，控制著現(xiàn)代地貌、地形及水系的發(fā)育。1控制主千河流及其支流的走向呈現(xiàn)出明顯的鋸齒狀，鋸齒方位主要為北北東、北北西和北西向2盆地南部黃土高原植被、含水性及地貌呈菱形塊狀分布，菱形塊狀邊界主要呈北北西和北東走向3盆地北部哪爾多斯高原內(nèi)部湖沼及鹽沼的展布主要為北西向。毛烏素沙漠的巨大沙隴呈北西走向。2在塔里木東部地區(qū)，形變作用力主要來自于天山造山帶的擠壓作用以及阿爾金斷裂帶的走滑作用。從演化序列上看，古生界的變形構(gòu)造樣式多屬墓底卷入型。中生界的變形構(gòu)造樣式多屬蓋層滑脫型新生界變形作用微弱，僅在盆地邊緣發(fā)育走滑以及逆沖構(gòu)造從平面分布上看，驀底卷入型在盆緣及盆地內(nèi)部都有發(fā)育，而蓋層滑脫型主要發(fā)育于盆地邊緣帶。3中上奧陶統(tǒng)平?jīng)鼋M、趙老峪組、克里摩里組、公烏素組、烏拉力克組、斯家溝組、其浪組、斜稼組、坎嶺組等沉積地層之中都發(fā)育典型的泥、灰?guī)r薄互層沉積MLML的重要特征是發(fā)育多級(jí)別的旋回。其中發(fā)育有濁流、火山、陸架崩塌、風(fēng)暴等多種事件沉積，以及豐富的形態(tài)較為完整的屬于ZOOPHYCOSNEREITES或者兩者混合相的遺跡化石組合。首次在趙老峪組發(fā)現(xiàn)風(fēng)暴沉積。4在趙老峪組中共發(fā)現(xiàn)屬于NEREIT“遺跡相的遺跡化石17屬25種，其中15屬為本地區(qū)新發(fā)現(xiàn)。遺跡組合反映趙老峪組主體形成于濱外最天風(fēng)攀浪蕃面以下海水較深和安靜的沉積環(huán)境之中。在平?jīng)鼋M中首次發(fā)現(xiàn)屬子典型的深水NEREITES相遺跡化石4屬3種，1未定種。其中MEGAGRAPTONSQODICTYON形成于事件前，PALEOLITESSABULARIA形成于事件后，該遺跡組合說明平?jīng)鼋M黑色筆石頁(yè)巖中發(fā)育有濁流事件沉積。其中發(fā)育SABULARIA一為UAMODICTYON組合遺跡化石的薄層灰?guī)r多是由臺(tái)地相鈣質(zhì)碎屑物質(zhì)的突然輸入形成，即事件沉積。5在長(zhǎng)江三角洲晚第四紀(jì)地層連續(xù)取芯鉆探工作中，通過選用大功率鉆機(jī)以及活動(dòng)頭雙套取土器，采用無泵干鉆工藝，使得取芯率達(dá)到90以上，且?guī)r芯內(nèi)部原生沉積層理清晰，取芯擾動(dòng)小。在巖芯中，發(fā)育生物遺跡、生物擾動(dòng)及植物根痕跡等原生生物成因的沉積栩造。關(guān)長(zhǎng)詞沉積地質(zhì)學(xué)，遺跡化石，塔里木盆地，俠甘寧盆地，長(zhǎng)江三角洲NUJ呂陜甘寧盆地、塔里木盆地以及長(zhǎng)江三角洲沉積地質(zhì)學(xué)研究是我博士后期間部分研究工作的初步總結(jié)。之所以選擇如此一個(gè)又大又泛的題目，緣起兩點(diǎn)，一是繼續(xù)博士期間的工作，二是在古今結(jié)合的基礎(chǔ)上，從沉積過程到地層記錄，從地層記錄返回到過程，力求有所創(chuàng)新。第一章研究陜甘寧盆地網(wǎng)狀斷裂與地貌和水系發(fā)育之間的關(guān)系，試圖闡明構(gòu)造穩(wěn)定區(qū)域內(nèi)部弱構(gòu)造變動(dòng)帶的特點(diǎn)及其對(duì)沉積作用的控制作用。第二章研究塔里木盆地東部地區(qū)的構(gòu)造系統(tǒng)，討論不同深度的斷裂構(gòu)造，以及薄皮構(gòu)造和厚皮構(gòu)造展布的特征。沉積地質(zhì)學(xué)研究如果不與構(gòu)造作用結(jié)合起來，盆地沉積演化、層序發(fā)育等研究就難以深入。顯然。掌握良好的構(gòu)造地質(zhì)學(xué)基礎(chǔ)，對(duì)我今后沉積地質(zhì)學(xué)研究是極為有益的。第三章研究了我國(guó)西北地區(qū)中上奧陶統(tǒng)發(fā)育的典型泥、灰?guī)r薄互層沉積MLML的重要特征是背景沉積穩(wěn)定，其中發(fā)育有濁流、火山、崩塌、風(fēng)暴等多種事件沉積。從豐富的沉積記錄中，可望闡明多種海洋事件沉積的相互關(guān)系，這對(duì)加深沉積過程的了解，建立災(zāi)害預(yù)報(bào)模型都是十分有益的。第四章研究了中上奧陶統(tǒng)趙老峪組豐富的遺跡化石及其環(huán)境意義，首次報(bào)道了平?jīng)鼋M發(fā)育的NEREITES相遺跡化石組合。生物成因的原生沉積構(gòu)造具有原生性、不混生性、對(duì)沉積環(huán)境反映敏感等優(yōu)點(diǎn)，將會(huì)在沉積過程的研究中發(fā)揮重要作用。第五章探討了長(zhǎng)江三角洲晚第四紀(jì)地層連續(xù)取芯鉆探技術(shù)。對(duì)巖芯中發(fā)育的生物遺跡、生物擾動(dòng)及植物根痕跡等生物成因的原生沉積構(gòu)造進(jìn)行了初步研究。此外，對(duì)長(zhǎng)江三角洲地區(qū)與沉積地層結(jié)構(gòu)相關(guān)的環(huán)境地質(zhì)災(zāi)害問題也進(jìn)行了初步探討。以上工作并不是雜亂無章和奄無關(guān)聯(lián)的，都是在同一個(gè)主題一一沉積地質(zhì)學(xué)之下，貫穿所有的工作之中。應(yīng)當(dāng)指出，對(duì)于陜甘寧盆地、塔里木盆地以及長(zhǎng)江三角洲的相關(guān)沉積地質(zhì)學(xué)研究這一綜合性很強(qiáng)的重大命題來說，本文只是在某幾個(gè)方面進(jìn)行了論證，有的僅僅提出了工作模式或假說，論證尚未深入，難免有不妥之處，懇請(qǐng)?jiān)u閱者批評(píng)指正。以利于今后工作更加深入的開展。在同濟(jì)大學(xué)良好的科研條件下，力圖有所創(chuàng)新，是我一直堅(jiān)持和努力的，也應(yīng)該是一個(gè)年青地質(zhì)工作者所必備的素質(zhì)。

簡(jiǎn)介：Y932076分類號(hào)UDC密級(jí)中國(guó)地質(zhì)科學(xué)院碩士學(xué)位論文酉壘皇蘭壘迦江縫盒瑩酉段部?jī)L巖邃蚩地匱生岱堂盈地璉他堂掛筵GEOCHRONOLOGYANDGEOCHEMISTRYCHARACTERSONSOMEMAGRNATICROCKSINTHEWESTOFXIIIRULANJINSHAIIANGSUTUREZONE指導(dǎo)教師姓名塞彪班宜雖睦塞班塞雖2專業(yè)名稱絲蔓業(yè)堂論文答辯日期答辯委員會(huì)主席評(píng)閱人學(xué)位授予日期2006年月日CHRONOLOGYANDGEOCHEMICALCH鍛AAEMONSOMEMAGMATICROCKSINTHEWESTOFXIJIRULANJINSHAJIANGSUTUREZONEABSTRACTI玨ORDERTOKNOWTHEEVOLUTIONHISTORYOFTHEWESTOFTHEXIJIRULANJINSHAJIMGSUTUREZONESOMEROCKSCLOSELYRELATEDWITHTHEPALEOTETHYSWERESTUDIEDINGEOEHEMISTRYANDGEOCHRONOLOGYONTHEBASEOFFIELDGEOLOGICALSURVEYSTHEMAGMATICROCKSWITHTHEPALECTATHYS，SUCHASBASALTS，QTMRTZDIORITES，GABBROSFROMTHEOPHIOLITES，ANDTRACHYTESANDGRANITESFORMEDBYCOLLISIONOFINDIAPLATEANDTHEEURASIANPLATEANDSOONWERECOLLECTEDBYⅡLEU巾BSHRIMPDATINGANDGEOCHEMICALANALYZINGOFTHESAMPLESTHEFOLLOWINGCONCLUSIONSWEREOBTAINED1THEGABBMOFNIEQIAQUOPHIOLITEHASTHESPECIALTIESOFMORBANDTHEZIRCONFROMTHEROCKGAVEA貓P妒3吣AGEOF265士TLMA2THECOMPAGESOFJIZANENGBASICULTRABESICROCKSINZADUOCOUNTYBELONGSTOCALCALKALINESERIES強(qiáng)EZIRCONINTHEGABHROFROMTHECOMPAGESGAVEA批P∥3吣MEANAGEOF25246MA，髓EROCKMIGHTBEPRODUCEDBYTHESUBDUCTIONOFTHEOCEANICCRUSTOFPALEOTETHYSINLATEPERMIANCONTRASTINGWITHTHECONTEMPORARYADAKITE3。THEINDOSINIANGRANITESATYUSHUZHIDUOANAWOREDATEDAS209士4MAT敦EGEOCHEMICALCHARACTERSINDICATEDTHATTHEYMIGHTBEFORMEDINVOLCANICARCENVIRONMENTBYMEP1ATCSUBDUCTIONSO，ITISBELIEVEDTHATALONGTHEXIJIRULANJINSHAJIANGSUTUREZONETHESUBDUCTIONOFTHECRUSTALREMNANTSOFTHEPATEOTETHYSWITHCONCOMITANCEOFTHEPLATECOLLISION。WERESTILLCARDEDONTMTILLATETRIAS4TELONGSALVOLCANICROCKSINZADUOCOUNTYMAINLYBELONGINGTOTHECALC采KALINESERIESWEREFORMEDINEPICONTINENTALVOLCANICAREENVIRONME蠅POSSIBLYBMUGHT姆THESUBDUCTIONOFTHERESIDUALOCEANICCRESTOFPALEOTETHYSTOZADUOMICROCONTINENTS，ANDTHEUPBAGEOFTHEZIRCONINDICATEDTHATTHEVOLCANOERUPTEDAT217士9MA5，THEREMNANTZIRCONS，BEINGOFPROTEROZOICAGES。WEREFOUNDINTHEGABBROOFNIEQIAQUOPHIOLITES，WHICHSHOWEDTHATTHEMATERIALOFTHEBASEMENTMIGHTTAKEPARTINTHE豁_?！轘SOFTHEFORMATIONOFTHEOPHIOLITES，6，AFTERMEASURINGZIRCONUPBAGEPRECISELYITWASCONFIRMEDTHATTHESHANGLAXIUVOLCANOERUPTIONSHOULDBEAT50圭IMAANDTHEBAIMAHAIGRMAHEWASEMPLACEDAT49士LMA。BOTHOFTHEMMITBEPRODUCEDBYTHELONGDISTANCEEFFECTSOFTHESUBDUCTIONCOLLISIONSBETWEENTHEINDIANPLATEANDEURASIANPLATEKEYWORDSSUTUREZONE，PALEOTETHYSXIJIRULANJINSHAJIANG0PHIOLITE，PLATESUBDUETION，GEOCHRONOLOGYGEOCHEMISTRY