地质学1.docx

地质学1.docx

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地质学1

Heatofthevolcanoontheundergroundundergroundcavernsandtheroleoftheformationoflargeearthquakes

Abstract:

volcanoes,undergroundcavesandlargeearthquakesarearesultoftheformationofgasandeverythingisundergroundheatgeneratedbytheundergroundpresenceofheatduringtheformationofcrustformationoccursinthehotbubble,rockcooledcondensation,whichchangestheplacewherethehotbubbleintoundergroundcaves,thermalexpansionofthebubbleexpansion,oneormoreoutofthebottomcrusttothesurfacefromthechanneltotheground,emittinglava,theformationofvolcanoes,hotbubblecoolingcontraction,resultinginhotrocklayerabovethebubbledomecollapse,steamexplosioncausedbyamajorearthquake.numerousandvariedactivitiesandgeologicalphenomenaaretheresultofundergroundheatoccurs,theundergroundsteamriseandfalloftheearthmovementandchangethemainmaterial. 

Keywords:

undergroundheat,thecrust,hotbubbles,volcanoes,undergroundcave,earthquake

Undergroundheatandvolcanoes,undergroundcave,amajorearthquake

Abstract:

Volcanoes,undergroundcavesandtheformationoflargeearthquakesarearesultofundergroundhotgas.Undergroundheatgeneratedinthecrust-shapedthethermalbubbleformation,lithospherecoolingcondensation,theplacewherethehotairbubblehavebeingbecomeintoundergroundcave;Thermalbubbleexpansion,outofoneormorechannelsfromthebottomtothesurface,magmaemittedtotheground,causevolcaniceruption.Thehotbubblecoolingcontraction,causedtherocklayersabovethedomebubblecollapse,causeheatexplosion,andoutbreakamajorearthquake.Numerousandvariedgeologicaleventsandphenomenaoccurredaretheresultofundergroundheat. 

Keywords:

:

UndergroundHeat;Crust;ThermalBubble;Volcano;UndergroundCave;Earthquake

Introduction

Hollowglassproductionprocessshowsgashotmagmacanchangeandshapetheshapeofhotmagmabubblescanexistinthehollowformedaftercooling,becomeshollowglassware,whichcandeducetheEarth'smagmacooledcondensingamountainorrocklayerinwrappedinbubble,airbubblesformedintoahollowwheresolidificationtoformcavesandundergroundcavenow.Byextension,theformationofearthquakesandvolcaniccaveundergroundheatfromtheheateffectisgenerated.'sLongeliminationheat,everythingiscausedbygeologicalactivity,generateavarietyofgeologicalphenomena. 

AnUndergroundHeatAndCrustalStructureOfTheResultingHole

1.1HeatGases

Heatthegasproducedmainlyintwoforms:

first,whentheheatmagmaticfluidsubstancesformionswheninheat,blendavarietyofmaterialnon-discriminatorymanner,whentheheatdowntoacertaintemperaturemagmaticfluidlevel,fluidpresentintheheatvarioussubstancestorestoreitsgaseousformandwillbereleasedtoformagaseousformofheat,thesecond,followingheatthebottomcrustwithmagmaticfluidsincontactwithitsexternalphysicalreaction,orheattogenerateavarietyofhotmagmaticfluidsgasreactionbetweenthematerial,generateavarietyofhotgascompoundstoformgaseousformofheatforexample,crustalheatflowfromthebottomofthefollowingtensofthousandsofdegreesCelsiusorsodowntoonethousand,ofwhich,suchasH,O,C,CL,Sandothersubstanceswhichwillrestoreitsgaseousformisreleased,thesesubstancescomeinbetweenoroutsidetheatmosphericpressureoffluidintheheatofthematerialandthematerialintheheatandthechemicalreactionofothercompoundssuchasH2O,CO2,N2,HC,HCL,H2S,HFandothersubstancesingaseousform. 

Through-holestructureofthecrust1.2 

Earthturnedouttobeafireball,constitutetheEarth'ssurfaceheatflowofmaterialincontactwiththeoutsidewiththegasreactsburncalories,andspatialdistributionofheatoutwardgraduallycooleddown,condensedintoamorehardrockandsoftsoillayerofwhitecrust.heatflowfromEarth'ssurfacedowntotheinsidelayersgraduallyfromoutsidetoinsidelayersofcooling,condensingintoanewlayerofrockorsoil,thesecoolnewrockorsoilconstitutetheEarth'scrust.Thisprocesscontinues,thecrustbecomesthickerandthicker. 

Rockandsoilandwhitecrustonthewhole,looseinthemiddleofahoneycombofholesandfullofsmallholes,andthree-dimensionalmeshconnectedstructureofthestate,cantheupperandlowerventilation.Themainreasonsfortheformationofthisstructurehasthefollowingtwospecies:

First,thecrustcooledbelowarecondensedintoahotliquidrockorsoillayers,theexternallayeroftherockiscold,thefluidlevelwithinahighfever,highfeverheatthefluidlayerofrockthroughthehotfluidisradiatedlayer,layerofrockencounteredinthecolderoutside,partofthethermalconvectionXiangbackwithinthefold,sothattheheatconvectioninheatandcoldfluidlayerbetweentherocklayersrepeatedly,iscaughtinthemiddleoftherocksoillayerofhotfluidassteamedbuns,filledwithfluffymiddletoformthree-dimensionalnetworkstructureoftheshapeoftheholescanbeinternalandexternalventilation,whenthesoilafteritcooledcondensingdiagenesis,thisshapeisfixeddown. 

Second,therockofthehotfluidiscontainedinthegaseoussubstancesarenotcompletelyreleased,themagmatoformbubblesofdifferentsizes,aftercooling,airbubblesintherocklayerwheretheformationofporesofdifferentsizes,empty,youcanupanddowntheventilation,undergroundcavernsandcavesissoformed. 

Eventhepurerock,thoughhard,compact,ofwhichtherearestillmanyamongthesmallholesandsmallcracks,thegascanbenormaltraffic. 

Theselayershavecooleddownthroughtheporestructureofrockandsoiltogethertoformathrough-holestructureofthecrust,thecrustoftheearththrough-holeconstructiontoensurethatthematerialinsideandoutsidethenormalexchangeofenergyinthelong-termevolutionofthecrust,Astheformationofthemovement,pushing,lifting,thickening,andvolcaniceruptionsandotherreasons,geologicaldeformation,insomeplacestheformationoftheventilationfunctionisweakened,orevenlossofventilatoryfunction,buttheoverallstructureofthecrustandtheventilationwillnotbetoobigchange. 

2UndergroundSteamAndVolcanicEruptions

2.1TheCausesOfVolcanic

2.1.1TheBasicPrincipleOfVolcanicEruptions

Thebasicprincipleofavolcaniceruptionisapressurecooker-typeheatexpansion. 

2.1.2VolcanicFormationOfTheThreeBasicConditions

Volcanicformationofthethreebasicconditions:

First,thebottomcrusttoformlargebubblesofhotgasgatheringorlargearches,thesecondisthebottomcrustalotofheatinalargebubbleofgasgatheringandcontinuetobeheated,thirdfromthebottomtothesurfacecrustviadifferentformsofthree-dimensionalnetworkstructure. 

Crustunderlyingtheproductionofemptyorarchesinseveralsituations:

first,crustalmovementcausedbytheunderlyingcrustispushed,upliftandtheformationofarches,thesecond,condensedintoasolidcrustandtheunderlyinglavarocklayer,duetoairbubblesinsidethemagmaAfterleavingthecondensationoftherocklayerwherethereisempty,thethird,thecrustbelowthebottomofthehotgasheatfluidtoproduceamoresparsesoftpushupthebottomofthecrusttoformarches. 

Materialformofhotgasinthecrustunderlyingtheformationofalotofhotairbubbles,orholesinthecrustofthebottomofthearchcometogethertoformlargehotbubbles,hotbubbleoffluidtokeeptheheatbelowitaddedtothehotgas,andheatingiscontinued,sothatthemajorhotbubblescontinuetoexpandandexpand,amixofhotgasbubblebecomeshotflammableandexplosive,thepowderkegreadytoexplode. 

Through-holestructureofthecrust,sothatalargeholeinthecrustorthebottomoftheholearchexpansiongatheredsteamheatandpressuretoexpandspacehasbecomeeasier,andthermalbubbleformationcanfollowthehole,cracks,voidscontinuouslyfromtheinsideoutgroundswelling,promote,expand,openupthebottomcrusttothesurfacefromthechannel,andfinally,redopengroundemittinghotgasandmagma,formingvolcanoes. 

2.1.3Eruption

Highheatflowbelowthebottomofthecrustcontainsavarietyofbodysubstances,suchasH,O,CL,Candothergasesarereleasedform,graduallypromotetheformationofthecrustunderlyingthesofthotmagmabubbles,orholesinthecrustofalargeconcentrationofthebottomofthearchtogethertoformahotbubble,theother,heatthefluidmaterialandothersubstancesforchemicalreactionofvariouscompoundsinthegaseousform,suchasH2O,CO2,N2,HC,HCLandothergaseouscompoundsintheholetogether,creatingahybridheatbubbles.heatthefluidmovementandkeptforchemicalreactions,alargevarietyofhotgasisconstantlycreated,continuouslyheatingandgasaddbubblestothesurroundingthermalexpansion,theexpansionspaceintoahotbubble,orsmallthermalexpansionoftheexpandingbubbleintoonebighotbubble,hotairbubblesorcracksinrocklayersalongtheholestretchupwardexpansionoftheexpansion,outofoneormorebubblestothesurfacefromthehotchannel.Crustalheatflowbelowthebottomoftheheatingandtheweightofthecrustformationunderpressure,heatalargehigh-pressurewarmairinthestate,whenitsenergyisaccumulatedtobeabletoforcetheexpansionofithaswasheddowntheopenchannelsoutoftheground,heatthegaswillbespewingoutfromthechannel,largebubblesofhotmagmabelowbyhigh-pressurefluidisfollowed,sprayground,whichisavolcaniceruption. 

2.2SomeCharacteristicsOfDiffe