34323.襄樊—廣濟(jì)斷裂帶的構(gòu)造變形特征研究

1、合肥工業(yè)大學(xué)碩士學(xué)位論文襄樊—廣濟(jì)斷裂帶的構(gòu)造變形特征研究姓名：黃文成申請(qǐng)學(xué)位級(jí)別：碩士專業(yè)：構(gòu)造地質(zhì)學(xué)指導(dǎo)教師：宋傳中20100401ResearchonthetectonicdeforlTlationofXiangFanGuangJifaultzoneABSTRACTVariouss缸眥tllraIphenomenacallbeobservedinthelong—termevolutionofXiangFan—GuangJifaul

2、t，whichhaarecordedtherichinformationaboutthesubductionandcollisionoftheQinLingmicro—continentalblocksandtheYangtzeplateT11ispapersummarizestheconstructionofrockcompositionofJingShanandShuiZhouwhicharerespectivelytransiti

3、onalsubstratecombinationcombinationofTablelandTablelandmargincombinationofTablelandriftedgeandcombinationofforelandbasinfromthenewstratumtotheoldAtthesametime，wecanrecognizedthattheareastudiedhasexperiencedalongtermtecto

4、nicdeformationevolutionfromYangtzeperiodtotheIndosinianandthattheformationofforelandbasinoftheHimalayantransformedbyseveraltectonicdeformationsmadecontributiontothepresenttectonicpatternResearchareahasthefea_tureofzonati

5、onfromtheNortheasttotheSouthwestItCanbedividedintoforelandthrustbeltofShuiZhouforelandfaultfoldbeltofDaHongmountainforelandbasinofJingShanaccordingtothedifferencesinthetectonicdeformationandthetectonicenvironment；Inaddit

6、ionthestructurallayerofresearchareacanbedividedintotheYangtzestructurallayerIndo—structurallayerlate—Yangtzestructurallayerandthestructurallayerofthecontinentalmargin，whichstandforatectoniccycleaccordingtothefeatureofthe

7、tectonicevolutionFoldsandfaultscomformedbythesubductionandcollisionoftheQinLingmicro—continentalblocksandtheYangtzeplateinmeIndosinianformedastructurMtrack，I11epaperresolvedthedeformationmetamorphicstructures，andtheforma

8、tionprocessofthefaultzonebythemethodsofstudingtheregionalstructuralgeologycombinedwithfieldsurveydataandexperimentsonmicrostructuredeformationanddeformationgeometrycharacteristicsofShouZhouandJingShanBesides，thepaperprov