湖南涟邵煤田测水煤系沉积环境与聚煤规律-.研究

湖南涟邵煤田测水煤系沉积环境与聚煤规律-.研究

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时间:2019-01-29

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1、中南大学硕士论文ABSTRACTLianyuan—-ShaoyangCoalfieldislocatedChangsha-ShaoyangfaultdepressionthecentralandwesternintheSouthChinafoldbelt.northtosouth.Itiswestprominentarcuatestructure山ataseriesofrelativelyClosedanticlineandShortaxissynclinecomposed,accompaniedbytheoverthm

2、stfault.overallistheNorthEast~NNEtrending.Lianyuan—ShaoyangCoalfieldisoneofthemajorcoalproductionbasesofHunanprovinceTheCeshuiCoaloftheEarlyCarboniferousisthemaincoal—bearingstratainthisareaIocalcoalreservesof山isareaisseriousshortageafterbeingdevelopmentandutiliz

3、edforyearsTherefore.thesedimentaryenvironmentsandcoalaccumulationruleontheCeshuiCoalstrataoftheEarlyCarboniferousonthearea,hasaguidingsignificancetofurtherdevelopthesystem,scientificresearchandanalysis.whichwillin山efuturetheregioncoalBasedonthecomprehensivecollec

4、tionandanalysisoftheresearchresultsofthepreviousgeologicaldata,thispaperpresentedthemethodsandprinciplesoftheapplicationofcoalbasinanalysisandcombinationofstratigraphy,sedimentology,petrologyandsequencestratigraphytheory.Lianyuan—ShaoyangCoalfieldEarlyCarbonifero

5、uscoal·-bearingstrataoftheCeshuiCoalrocktype.1ithologicalcharacteristicsandsedimentarystructureswereanalyzedindetailinthepaperconductedthedivisionofthedepositionsystemandthecomprehensiveThedepositionofthesedimentarysystemcharacteristicsandspatialdistributionlawwe

6、rerevealedinthepaperAnalysisresultsshownthatthecoalenvironmentofEarlyCarboniferousCeshuiCoalbarrierisland—lagoondepositionalsystems,tidalfiat,lagoon,tidalchannels,barrierdam,peatswamp.foreshoreoutsidethemuddycontinentalshelfandothertypesofsedimentaryfacieswerepea

7、tswamp.Coal—beatingstratigraphicsequencestratigraphic厅ameworkanddistributioncharacteristicswerepresentedinthepaperTheauthorpointedoatthatthedistributionofcoalSealTISinthe中南大学硕士论文sequencestratigraphicframework,andmadeapaleogeographicmapofthefacies.Finally,accordin

8、gtothestudyareaofthepaleo—tectonic,paleogeographic,paleoclimateandancientplantsthataretherelationshipbetweenandtheevolutionofthedepositionalenvironment,theauth

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