秦嶺印支期構造背景、巖漿活動及成礦作用

秦嶺印支期構造背景、巖漿活動及成礦作用一、本文概述Overviewofthisarticle本文旨在深入探討秦嶺地區(qū)印支期的構造背景、巖漿活動以及與之相關的成礦作用。秦嶺，作為中國重要的地理和地質分界線，其地質歷史復雜且獨特，特別是在印支期，該地區(qū)的構造活動和巖漿作用對區(qū)域乃至全球的地質演化產生了深遠影響。因此，對秦嶺印支期構造背景、巖漿活動及成礦作用的研究，不僅有助于深化我們對中國乃至全球大陸動力學過程的理解，而且對于礦產資源的勘查和開發(fā)也具有重要的實際意義。Thisarticleaimstoexploreindepththetectonicbackground,magmaticactivity,andrelatedmineralizationprocessesoftheIndosinianperiodintheQinlingMountainsregion.TheQinlingMountains,asanimportantgeographicalandgeologicalboundaryinChina,haveacomplexanduniquegeologicalhistory,especiallyduringtheIndosinianperiod.Thetectonicactivitiesandmagmatismintheregionhavehadaprofoundimpactontheregionalandevenglobalgeologicalevolution.Therefore,thestudyoftheIndosiniantectonicbackground,magmaticactivity,andmineralizationintheQinlingMountainsnotonlydeepensourunderstandingofthedynamicprocessesofChinaandeventheglobalcontinent,butalsohasimportantpracticalsignificancefortheexplorationanddevelopmentofmineralresources.本文將首先概述秦嶺地區(qū)印支期的構造背景，包括地殼運動、板塊相互作用、構造帶的形成和演化等。接著，將詳細分析這一時期的巖漿活動，包括巖漿巖的類型、分布、巖石學特征及其成因等。在此基礎上，本文將探討巖漿活動與成礦作用的關系，分析巖漿活動如何為成礦作用提供物質來源和能量條件，以及成礦作用的時空分布規(guī)律和成礦模式。ThisarticlewillfirstoutlinethetectonicbackgroundoftheIndosinianperiodintheQinlingMountainsregion,includingcrustalmovement,plateinteractions,andtheformationandevolutionoftectonicbelts.Next,adetailedanalysisofthemagmaticactivityduringthisperiodwillbeconducted,includingthetypes,distribution,petrologicalcharacteristics,andgenesisofmagmaticrocks.Onthisbasis,thisarticlewillexploretherelationshipbetweenmagmaticactivityandmineralization,analyzehowmagmaticactivityprovidesmaterialsourcesandenergyconditionsformineralization,aswellasthespatiotemporaldistributionpatternsandmineralizationmodelsofmineralization.通過本文的研究，我們期望能夠建立起秦嶺地區(qū)印支期構造背景、巖漿活動與成礦作用之間的內在聯系，揭示這一時期的地質演化過程，為深入理解大陸動力學提供新的視角和思路。本文的研究成果也將為秦嶺地區(qū)的礦產資源勘查和開發(fā)提供科學依據，促進地方經濟的可持續(xù)發(fā)展。Throughtheresearchinthisarticle,wehopetoestablishtheinherentconnectionbetweentheIndosiniantectonicbackground,magmaticactivity,andmineralizationintheQinlingMountainsregion,revealthegeologicalevolutionprocessofthisperiod,andprovidenewperspectivesandideasforadeeperunderstandingofcontinentaldynamics.TheresearchresultsofthisarticlewillalsoprovidescientificbasisfortheexplorationanddevelopmentofmineralresourcesintheQinlingregion,andpromotethesustainabledevelopmentofthelocaleconomy.二、秦嶺印支期構造背景QinlingIndosiniantectonicbackground秦嶺地區(qū)在印支期（約245-205百萬年前）經歷了復雜而重要的構造演化，這一時期的地質活動對于理解秦嶺乃至整個中國的地質歷史具有深遠的意義。印支期正值古特提斯洋閉合與華北、華南板塊匯聚的關鍵時期，秦嶺地區(qū)作為這兩大板塊之間的關鍵結合帶，其構造背景顯得尤為復雜。TheQinlingregionunderwentcomplexandimportanttectonicevolutionduringtheIndosinianperiod(approximately245-205millionyearsago),andthegeologicalactivitiesduringthisperiodhaveprofoundsignificanceforunderstandingthegeologicalhistoryoftheQinlingMountainsandeventheentireChina.TheIndosinianperiodwasacriticalperiodfortheclosureoftheancientTethysOceanandtheconvergenceoftheNorthandSouthChinaplates.Asakeyjunctionzonebetweenthesetwoplates,theQinlingMountainsregionhadaparticularlycomplextectonicbackground.在印支期初期，秦嶺地區(qū)受到古特提斯洋俯沖的影響，形成了大規(guī)模的巖漿弧和弧后盆地。隨著洋殼的消減和陸殼的匯聚，秦嶺地區(qū)發(fā)生了一系列的構造變形和巖漿活動。這些巖漿活動以中酸性侵入巖和火山巖為主，廣泛分布于秦嶺造山帶的南北兩側。IntheearlyIndosinianperiod,theQinlingregionwasinfluencedbythesubductionoftheancientTethysOcean,forminglarge-scalemagmaticarcsandbackarcbasins.Withthereductionofoceaniccrustandtheconvergenceofcontinentalcrust,aseriesoftectonicdeformationsandmagmaticactivitiesoccurredintheQinlingregion.Thesemagmaticactivitiesaremainlycomposedofintermediateacidicintrusiverocksandvolcanicrocks,widelydistributedonthenorthandsouthsidesoftheQinlingorogenicbelt.印支期中晚期，隨著華北和華南板塊的最終碰撞，秦嶺地區(qū)發(fā)生了強烈的造山運動。這一時期的構造變形主要表現為褶皺、逆沖推覆和走滑斷裂等。這些構造變形不僅改變了秦嶺地區(qū)的地貌格局，也深刻影響了該地區(qū)的巖漿活動和成礦作用。InthemidtolateIndosinianperiod,withthefinalcollisionoftheNorthChinaandSouthChinaplates,astrongorogenyoccurredintheQinlingregion.Thestructuraldeformationduringthisperiodmainlymanifestedasfolding,reversethrust,andstrikeslipfaults.ThesestructuraldeformationsnotonlychangedthegeomorphicpatternoftheQinlingMountainsregion,butalsoprofoundlyinfluencedthemagmaticactivityandmineralizationintheregion.秦嶺印支期的構造背景是復雜的，它涉及到古特提斯洋的閉合、板塊匯聚、巖漿活動以及構造變形等多個方面。這些地質作用共同構成了秦嶺印支期豐富多樣的地質特征，也為后續(xù)的成礦作用提供了重要的構造背景和物質基礎。ThetectonicbackgroundoftheQinlingIndosinianperiodiscomplex,involvingmultipleaspectssuchastheclosureoftheancientTethyanOcean,plateconvergence,magmaticactivity,andtectonicdeformation.ThesegeologicalprocessestogetherconstitutetherichanddiversegeologicalfeaturesoftheQinlingIndosinianperiod,andalsoprovideimportantstructuralbackgroundandmaterialbasisforsubsequentmineralization.三、秦嶺印支期巖漿活動QinlingIndosinianmagmaticactivity秦嶺地區(qū)在印支期的巖漿活動極為豐富，這不僅體現在巖漿活動的頻繁和廣泛，還體現在巖漿巖種類的多樣性和巖漿活動的復雜性。印支期巖漿活動的顯著特點包括花崗巖類的大量出現和火山巖的廣泛分布。ThemagmaticactivityintheQinlingregionduringtheIndosinianperiodwasextremelyrich,whichwasnotonlyreflectedinthefrequentandextensivemagmaticactivity,butalsointhediversityofmagmaticrocktypesandthecomplexityofmagmaticactivity.ThesignificantcharacteristicsofIndosinianmagmaticactivityincludetheabundantoccurrenceofgraniteandthewidespreaddistributionofvolcanicrocks.秦嶺印支期巖漿活動的主要巖石類型有花崗巖、閃長巖、輝長巖等，其中花崗巖類尤為發(fā)育。這些巖漿巖的化學成分和礦物組合反映了其巖漿源區(qū)的多樣性，既有來自地殼深部的巖漿，也有來自地幔的巖漿。巖漿活動過程中還伴隨著豐富的成礦作用，如銅、金、鎢、錫等金屬礦產的形成。ThemainrocktypesoftheIndosinianmagmaticactivityintheQinlingMountainsincludegranite,diorite,gabbro,etc.Amongthem,graniteisparticularlydeveloped.Thechemicalcompositionandmineralcompositionofthesemagmaticrocksreflectthediversityoftheirmagmasourceareas,includingmagmafromdeepcrustandmantle.Theprocessofmagmaticactivityisalsoaccompaniedbyrichmineralization,suchastheformationofmetalmineralssuchascopper,gold,tungsten,tin,etc.在秦嶺地區(qū)，印支期巖漿活動的時間和空間分布具有明顯的規(guī)律性。時間上，巖漿活動主要集中在印支期的早期和中期，晚期相對較少?？臻g上，巖漿活動主要集中在秦嶺的南部和中部地區(qū)，尤其是南秦嶺地區(qū)，巖漿活動尤為頻繁和強烈。IntheQinlingregion,thetemporalandspatialdistributionofIndosinianmagmaticactivityhasobviousregularity.Intermsoftime,magmaticactivityismainlyconcentratedintheearlyandmiddlestagesoftheIndosinianperiod,withrelativelylesslatestage.Spatially,magmaactivityismainlyconcentratedinthesouthernandcentralregionsoftheQinlingMountains,especiallyinthesouthernQinlingMountains,wheremagmaactivityisparticularlyfrequentandintense.印支期巖漿活動的成因機制與秦嶺地區(qū)當時的構造背景密切相關。這一時期，秦嶺地區(qū)處于板塊俯沖和碰撞的構造環(huán)境，地殼增厚、縮短，巖漿活動頻繁。同時，地幔物質的上涌和地殼物質的熔融也為巖漿活動提供了豐富的物質來源。ThegeneticmechanismofIndosinianmagmaticactivityiscloselyrelatedtothetectonicbackgroundoftheQinlingregionatthattime.Duringthisperiod,theQinlingregionwasinatectonicenvironmentofplatesubductionandcollision,withcrustalthickeningandshortening,andfrequentmagmaticactivity.Meanwhile,theupwellingofmantlematerialandthemeltingofcrustalmaterialalsoprovideabundantmaterialsourcesformagmaticactivity.印支期巖漿活動對秦嶺地區(qū)的構造演化和地殼演化產生了深遠的影響。一方面，巖漿活動導致了地殼的增厚和縮短，進一步塑造了秦嶺地區(qū)的構造格局；另一方面，巖漿活動為金屬礦產的形成提供了重要的物質基礎和熱源條件，對秦嶺地區(qū)的成礦作用產生了重要的影響。TheIndosinianmagmaticactivityhashadaprofoundimpactonthetectonicandcrustalevolutionoftheQinlingregion.Ontheonehand,magmaticactivityhasledtothickeningandshorteningofthecrust,furthershapingthestructuralpatternoftheQinlingMountainsregion;Ontheotherhand,magmaticactivityprovidesanimportantmaterialbasisandheatsourceconditionsfortheformationofmetallicminerals,andhashadasignificantimpactonthemineralizationprocessintheQinlingregion.秦嶺印支期巖漿活動是該地區(qū)地殼演化和構造演化的重要組成部分，也是成礦作用的重要驅動力。對秦嶺印支期巖漿活動的研究不僅有助于深入理解秦嶺地區(qū)的構造演化和地殼演化歷史，也為尋找和勘探金屬礦產提供了重要的理論依據。TheIndosinianmagmaticactivityintheQinlingMountainsisanimportantcomponentofthecrustalandtectonicevolutionintheregion,aswellasanimportantdrivingforceformineralization.ThestudyoftheIndosinianmagmaticactivityintheQinlingMountainsnotonlyhelpstogainadeeperunderstandingofthetectonicandcrustalevolutionhistoryoftheQinlingregion,butalsoprovidesimportanttheoreticalbasisforthesearchandexplorationofmetallicminerals.四、秦嶺印支期成礦作用QinlingIndosinianmineralization秦嶺地區(qū)在印支期的成礦作用表現出顯著的復雜性和多樣性。這一時期，由于構造運動的活躍和巖漿活動的頻繁，為成礦作用提供了有利的地質環(huán)境。ThemineralizationprocessintheQinlingregionduringtheIndosinianperiodshowedsignificantcomplexityanddiversity.Duringthisperiod,theactivetectonicmovementandfrequentmagmaticactivityprovidedafavorablegeologicalenvironmentformineralization.秦嶺印支期的成礦作用與巖漿活動密切相關。巖漿活動不僅為成礦提供了必要的熱能和物質來源，同時也為成礦元素的遷移和聚集提供了通道和空間。在這一時期，秦嶺地區(qū)出現了大量的巖漿巖，如花崗巖、閃長巖等，它們富含多種成礦元素，如Cu、Pb、Zn、Au、Ag等。這些元素在巖漿巖的形成過程中，通過巖漿的演化和分異作用，逐漸聚集并形成礦體。ThemineralizationoftheQinlingIndosinianperiodiscloselyrelatedtomagmaticactivity.Magmaticactivitynotonlyprovidesnecessarythermalandmaterialsourcesformineralization,butalsoprovideschannelsandspacesforthemigrationandaccumulationofore-formingelements.Duringthisperiod,alargenumberofmagmaticrocksappearedintheQinlingregion,suchasgraniteanddiorite,whichwererichinvariousore-formingelementssuchasCu,Pb,Zn,Au,Ag,etc.Theseelementsgraduallyaccumulateandformorebodiesduringtheformationprocessofmagmaticrocksthroughtheevolutionanddifferentiationofmagma.秦嶺印支期的成礦作用與構造運動密切相關。構造運動不僅為巖漿活動和成礦作用提供了動力，同時也為成礦元素的遷移和聚集提供了通道和空間。在這一時期，秦嶺地區(qū)經歷了多次構造運動，如擠壓、伸展等，這些構造運動不僅形成了許多斷裂和褶皺，同時也為成礦元素的遷移和聚集提供了有利的空間。ThemineralizationoftheQinlingIndosinianperiodiscloselyrelatedtotectonicmovements.Thetectonicmovementnotonlyprovidesimpetusformagmaticactivityandmineralization,butalsoprovideschannelsandspacesforthemigrationandaccumulationofore-formingelements.Duringthisperiod,theQinlingregionexperiencedmultipletectonicmovements,suchascompressionandextension,whichnotonlyformedmanyfaultsandfolds,butalsoprovidedfavorablespaceforthemigrationandaccumulationofore-formingelements.秦嶺印支期的成礦作用還具有明顯的時空分布特征。從空間分布上看，成礦作用主要集中在秦嶺地區(qū)的北部和南部，其中北部以銅、鉛、鋅等金屬礦產為主，南部則以金、銀等貴金屬礦產為主。從時間分布上看，印支期的成礦作用主要集中在中期和晚期，其中中期以巖漿活動和構造運動的頻繁為特點，晚期則以成礦作用的集中爆發(fā)為特點。ThemineralizationoftheQinlingIndosinianperiodalsohasobviousspatiotemporaldistributioncharacteristics.Fromaspatialdistributionperspective,mineralizationismainlyconcentratedinthenorthernandsouthernpartsoftheQinlingMountains,withthenorthernpartbeingdominatedbymetallicmineralssuchascopper,lead,andzinc,whilethesouthernpartisdominatedbypreciousmetalmineralssuchasgoldandsilver.Fromatemporaldistributionperspective,themineralizationoftheIndosinianperiodwasmainlyconcentratedinthemiddleandlatestages,withthemiddlestagecharacterizedbyfrequentmagmaticandtectonicactivity,andthelatestagecharacterizedbyconcentratederuptionsofmineralization.秦嶺印支期的成礦作用是在巖漿活動和構造運動的共同作用下形成的。這一時期的成礦作用具有多樣性、復雜性和時空分布特征，對于深入了解秦嶺地區(qū)的地質演化和礦產資源分布具有重要意義。也為后續(xù)的礦產勘查和開發(fā)提供了重要的理論依據和指導。ThemineralizationoftheQinlingIndosinianperiodwasformedunderthejointactionofmagmaticactivityandtectonicmovement.Themineralizationprocessduringthisperiodhasdiversity,complexity,andspatiotemporaldistributioncharacteristics,whichisofgreatsignificanceforadeeperunderstandingofthegeologicalevolutionandmineralresourcedistributionintheQinlingregion.Italsoprovidesimportanttheoreticalbasisandguidanceforsubsequentmineralexplorationanddevelopment.五、秦嶺印支期構造、巖漿活動與成礦作用的相互關系TheinterrelationshipbetweenQinlingIndosiniantectonic,magmaticactivity,andmineralization秦嶺地區(qū)在印支期的構造、巖漿活動與成礦作用之間存在著密切的相互關系，這些關系不僅反映了該地區(qū)地殼演化的歷史，也對礦產資源的形成和分布產生了深遠的影響。Thereisacloseinterrelationshipbetweenthestructure,magmaticactivity,andmineralizationintheQinlingregionduringtheIndosinianperiod.Theserelationshipsnotonlyreflectthehistoryofcrustalevolutionintheregion,butalsohaveaprofoundimpactontheformationanddistributionofmineralresources.印支期構造運動對秦嶺地區(qū)的巖漿活動和成礦作用起到了重要的控制作用。在印支期，秦嶺地區(qū)經歷了一系列的構造運動，包括地殼的擠壓、抬升和斷裂等，這些構造運動為巖漿的上升和就位提供了通道和空間。同時，構造運動還導致了地殼內部的應力場和溫度場的變化，為巖漿的形成和演化提供了必要的條件。TheIndosiniantectonicmovementplayedanimportantcontrollingroleinthemagmaticactivityandmineralizationintheQinlingregion.DuringtheIndosinianperiod,theQinlingregionexperiencedaseriesoftectonicmovements,includingcrustalcompression,uplift,andfaulting,whichprovidedchannelsandspacefortheascentandemplacementofmagma.Atthesametime,tectonicmovementsalsoleadtochangesinthestressandtemperaturefieldsinsidethecrust,providingnecessaryconditionsfortheformationandevolutionofmagma.巖漿活動在印支期對秦嶺地區(qū)的構造和成礦作用產生了重要影響。隨著巖漿的上升和就位，巖漿中的揮發(fā)分、金屬元素和其他成礦元素被帶入地殼淺部，并在適當的條件下形成了各種類型的礦床。這些礦床的形成不僅與巖漿的成分和演化程度有關，還與巖漿活動的空間和時間分布密切相關。MagmaticactivityhadasignificantimpactonthestructureandmineralizationoftheQinlingregionduringtheIndosinianperiod.Asmagmarisesandempresses,volatiles,metalelements,andotherore-formingelementsfrommagmaarebroughtintotheshallowcrust,andvarioustypesofdepositsareformedunderappropriateconditions.Theformationofthesemineraldepositsisnotonlyrelatedtothecompositionandevolutionofmagma,butalsocloselyrelatedtothespatialandtemporaldistributionofmagmaactivity.印支期的構造和巖漿活動共同控制了秦嶺地區(qū)的成礦作用。在印支期，秦嶺地區(qū)形成了一系列與構造和巖漿活動有關的礦床，包括巖漿型礦床、熱液型礦床和接觸交代型礦床等。這些礦床的形成是構造運動和巖漿活動相互作用的結果，它們不僅為秦嶺地區(qū)的經濟發(fā)展提供了重要的礦產資源，也為研究該地區(qū)地殼演化和成礦作用提供了重要的地質證據。ThetectonicandmagmaticactivitiesduringtheIndosinianperiodjointlycontrolledthemineralizationintheQinlingregion.DuringtheIndosinianperiod,aseriesofmineraldepositsrelatedtotectonicandmagmaticactivitieswereformedintheQinlingregion,includingmagmaticdeposits,hydrothermaldeposits,andcontactmetasomaticdeposits.Theformationofthesemineraldepositsistheresultoftheinteractionbetweentectonicmovementandmagmaticactivity.TheynotonlyprovideimportantmineralresourcesfortheeconomicdevelopmentoftheQinlingregion,butalsoprovideimportantgeologicalevidenceforthestudyofcrustalevolutionandmineralizationintheregion.秦嶺地區(qū)印支期的構造、巖漿活動與成礦作用之間存在著密切的相互關系。構造運動為巖漿活動和成礦作用提供了必要的條件，巖漿活動則通過攜帶和釋放成礦元素等方式影響了成礦作用的發(fā)生和發(fā)展。這些相互關系的研究不僅有助于深入了解秦嶺地區(qū)地殼演化的歷史，也為該地區(qū)的礦產資源勘查和開發(fā)提供了重要的指導。Thereisacloseinterrelationshipbetweenthestructure,magmaticactivity,andmineralizationduringtheIndosinianperiodintheQinlingregion.Thetectonicmovementprovidesnecessaryconditionsformagmaticactivityandmineralization,andmagmaticactivityaffectstheoccurrenceanddevelopmentofmineralizationthroughcarryingandreleasingore-formingelements.ThestudyoftheseinterrelationshipsnotonlyhelpstogainadeeperunderstandingofthehistoryofcrustalevolutionintheQinlingMountainsregion,butalsoprovidesimportantguidancefortheexplorationanddevelopmentofmineralresourcesintheregion.六、結論Conclusion通過對秦嶺地區(qū)印支期構造背景、巖漿活動及成礦作用的綜合研究，本文得出以下ThroughacomprehensivestudyoftheIndosiniantectonicbackground,magmaticactivity,andmineralizationintheQinlingMountainsregion,thisarticleconcludesthefollowing:秦嶺地區(qū)在印支期經歷了復雜的構造演化，主要表現為板塊俯沖、碰撞造山以及陸內造山等過程。這些構造活動不僅形成了多期的巖漿巖，還為成礦作用提供了有利的地質環(huán)境。TheQinlingregionexperiencedcomplextectonicevolutionduringtheIndosinianperiod,mainlymanifestedasplatesubduction,collisionorogeny,andintracontinentalorogeny.Thesetectonicactivitiesnotonlyformedmulti-stagemagmaticrocks,butalsoprovidedafavorablegeologicalenvironmentformineralization.印支期巖漿活動在秦嶺地區(qū)表現強烈，形成了大量的花崗巖、閃長巖等巖漿巖。這些巖漿巖的地球化學特征表明，它們主要來源于地殼的部分熔融，并受到了一定程度的地幔物質的貢獻。巖漿活動的時間、空間分布與區(qū)域構造演化密切相關，反映了構造活動對巖漿作用的重要控制作用。TheIndosinianmagmaticactivitywasstrongintheQinlingregion,formingalargenumberofmagmaticrockssuchasgraniteanddiorite.Thegeochemicalcharacteristicsofthesemagmaticrocksindicatethattheymainlyoriginatefrompartialmeltingofthecrustandarecontributedtoacertainextentbymantlematerial.Thetimeandspatialdistributionofmagmaticactivityarecloselyrelatedtoregionaltectonicevolution,reflectingtheimportantcontrolroleoftectonicactivityonmagmaticactivity.成礦作用在秦嶺印支期構造背景和巖漿活動的共同作用下得以發(fā)生。本文研究發(fā)現，印支期巖漿活動為成礦提供了熱源和物質來源，而構造活動則為成礦提供了有利的空間和通道。因此，印支期是秦嶺地區(qū)重要的成礦時期，形成了一系列具有經濟價值的礦床。ThemineralizationoccurredunderthecombinedactionofthetectonicbackgroundandmagmaticactivityduringtheIndosinianperiodintheQinlingMountains.ThisstudyfoundthattheIndosinianmagmaticactivityprovidedaheatsourceandmaterialsourceformineralization,whiletectonicactivityprovidedfavorablespaceandchannelsformineralization.Therefore,theIndosinianperiodwasanimportantmineralizationperiodintheQinlingregion,formingaseriesofeconomicallyvaluablemineraldeposits.本文通過對秦嶺地區(qū)印支期構造背景、巖漿活動及成礦作用的綜合分析，揭示了它們之間的內在聯系和演化規(guī)律。這些認識不僅有助于深化對秦嶺地區(qū)地質演化的理解，也為未來的礦產資源勘查和開發(fā)提供了重要的科學依據。ThisarticlerevealstheinternalconnectionsandevolutionarylawsbetweentheIndosiniantectonicbackground,magmaticactivity,andmineralizationintheQinlingregionthroughacomprehensiveanalysis.TheseunderstandingsnotonlycontributetoadeeperunderstandingofthegeologicalevolutionoftheQinlingMountainsregion,butalsoprovideimportantscientificbasisforfuturemineralresourceexplorationanddevelopment.秦嶺地區(qū)印支期構造背景、巖漿活動及成礦作用是一個復雜的地質過程，它們之間的相互作用和演化關系對秦嶺地區(qū)的地質環(huán)境和礦產資源具有重要的影響。未來的研究應進一步深入探討這些過程的細節(jié)和機制，為地質學和相關領域的發(fā)展做出更大的貢獻。TheIndosiniantectonicbackground,magmaticactivity,andmineralizationintheQinlingregionarecomplexgeologicalprocesses,andtheirinteractionsandevolutio