Geological Evolution and Huge Ore-Forming Belts in the Core Part of the Central Asian Metallogenic Region-中国期刊网

摘要 Themulti-stagegeologicalevolutionandextensivecontinentaldeformationsduringthecourseofitshistorymaketheCentralAsianmetallogenicregion(CAMR)auniqueandcomplicatedlarge-scalemetaldomain.Newgeologicalobservationsandpreciseage-dataallowanimprovedreconstructionofthegeologicalevolutionoftheCAMR.ThispapersummarizesthePaleozoicorogenicevolutionandrelatedoreformationinthecorepartoftheCAMRbasedonthegeologicaldatapublishedbothduringtheSovietperiodandthelastdecades.Fourore-formationprovinces(Altay,BalkhashJunggar,Chu-Yili-Tianshan,andSouthwestTianshan)couldbeclassified.TheBalkhash-JunggarandChu-Yili-Tianshanprovincesarethemajortopicsofthispaper.TheBalkhash-Junggarprovinceconsistsof4hugeore-formingbelts(Zharma-Saur,Tarbahtay-Xiemistay,Aktogay-Baerluke,BalkhashwesternJunggar)with11largeore-collegeareas.TheChu-Yili-Tianshanprovinceconsistsof4hugeore-formingbelts(Alatau-Sairimu,Chu-Yili-Bolehuole,Issyk-Awulale,Kazharman-Nalaty)with22largeore-collegeareas.Formationoflargeore-collegeareacorrespondstoaspecificstageofcontinentalcrustgrowth.ComparisonofgeologyandoredepositsintheCAMRprovidesrichinformationforfutureexplorationandunderstandingofore-formingprocesses.ThePaleo-JunggarOceanclosedatEarlyDevonianintheBalkhash-westernJunggarore-formingbelt.Afterwards,widespreadvolcanic-sedimentaryrocksformedatextensionalstageduetodelaminationofthethicklowercrustformedduringpreviousaccretionaryprocesses.FelsicmagmaintrusioncausedformationofporphyryCu-Audepositat~310Maandrelatedhydrothermalgolddepositsabout10Malater.Forexample,intheHatu-Baobei-SartohayAu-Crore-collegeareaintheBalkhash-westernJunggarore-formingbelt,smallgranitictodioriteplutonsandvariousdykes(312–277Ma)andlargegranitebodies(~300Ma)intrudedintotheDevoniantoEarlyCarboniferousvolcano-sedimentarybasin.Thesemagmaticactivities

1OBOLENSKY;A;BORISENKO. METALLOGENY OF MESOZOIC RIFTOGENIC STRUCTURES OF CENTRAL ASIA (ORE-FORMING SYSTEMS, ORE SUBSTANCE SOURCES).地质学,1994-11.
2BORISENKO;A.S;OBOLENSKY;A.A. CONCENTRATION OF ORE-FORMING SOLUTIONS AS A FACTOR OF FORMATION OF SUPERLARGE DEPOSITS.地质学,1994-01.
3ZHANG Zuoheng;WANG Zhiliang;WANG Longsheng;ZUO Guochao. Metallogenic Epoch and Ore-forming Environment of the Lamasu Skarn-porphyritic Cu-Zn deposit, western Tianshan, Xinjiang, NW China.地质学,2008-04.
4. Historical-Dynamic Integrative Classification of Basinogenesis and Ore-Forming Basins.地质学,1993-01.
5邓军;方云;杨立强;杨军臣;孙忠实;王建平丁式江王庆飞. Numerical Modelling of Ore-forming Dynamics of Fractal Dispersive Fluid Systems.地质学,2001-02.
6肖惠良;周济元;王鹤年;董永观;季俊峰;赵宇. Geochemical Characteristics and source of Ore-Forming Fluid of Duolanasayi Gold Deposit,Xinjiang.地球化学,2003-01.
7. HIST ORICAL-DYNAMIC INTEGRATIVE CLASSIFICATION OF BASINOGENESIS AND ORE-FORMING BASINS.地质学,1994-02.
8BUADZE;V.I. STEPWISE METALLOGENY-THE MODEL OF METALLOGENIC EVOLUTION OF THE REGION (AS IN THE CAUCASUS).地质学,1994-04.
9Igor'V Kemkin Raisa A Kemkina. Microheterogeneity of the Koupol Deposit Fahlores as a Reflection of Changing of Physicochemical Parameters of the Ore-Forming Solution.地质学,2013-02.
10王宝德;牛树银;孙爱群;李红阳. Isotopic Characteristics of Mesozoic Au-Ag Polymetallic Ore Deposits in Northern Hebei and Their Ore-Forming Materials Source.地球化学,2003-03.

Geological Evolution and Huge Ore-Forming Belts in the Core Part of the Central Asian Metallogenic Region

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Geological Evolution and Huge Ore-Forming Belts in the Core Part of the Central Asian Metallogenic Region

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