青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)

青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)

ID:33737670

大小:3.47 MB

页数:82页

时间:2019-02-28

青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)_第1页
青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)_第2页
青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)_第3页
青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)_第4页
青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)_第5页
资源描述:

《青海祁漫塔格地区它温查汉西铁多金属矿床地质特征与成因探讨-(6240)》由会员上传分享,免费在线阅读,更多相关内容在行业资料-天天文库

1、AbstractTheTawenchahanxiFe-polymetallicdepositislocatedinthesoutheastsection(probably300degreesdirection)oftheQimantageHillinQinghaiprovince,whichisabout200kmfromthenorthwestofGeermucity.Inrecentyears,itisanothermedium-sizedFe-polymetallicdepositaftertheShaqiu,ChangshanandNiukutoudeposits,

2、whichcontainsmorethan40milliontonsofprovenironoreresources.Theorebodyandore-formingrockmassarecoveredbyQuaternaryeoliansand.ThegeotectonicpositionofminingareaislocatedintheNorthQimantageEarlyPaleozoicmagmaticarcbelt,whichisalsolocatedinthenorthofNalinggelefractureintheEastKunLun.Thedeposit

3、islocatedamongeastlongitude292°31'-92°52',northlatitude36°55'-37°00',withatotalareaabout100km.Throughanalysisthegeologicalcharacteristics,themineralizationalterationzoningofthedepositandgeochemicalcharacteristicsoftheore-formingrockmass,thisarticleisinordertofindoutthegeologicalgenesisofth

4、edeposit,mineralization,orecontrollingfactorsandprospectingmodel.Bycomparingwithotherdeposits,inthelargerareaestablishthemaintypeoforedepositandsummarizethemetallogenicregularity,soastoguidethemineralexplorationandpractice.Finally,relatedtotherelationshipoftectonicmagmaticmineralizationinQ

5、imantageareaandthegeologicalcharacteristicsandgenesisofthedeposit,wegetthemainresearchresultsareasfollows:(1)CardingsummeduptheconclusionsthatinEarlyTriassicapproximatelyduring(242~239Ma),thewesternofEast-Kunlunorogenicbelt(Qimantagearea)isduringthetransitionstagewhichisintheendoftheoceani

6、ccrustsubductiontothebeganofthecontinentalcrustcollision,whiletranslateintostretchafterthecollisionstageduring(237~204Ma).Atthesametimethemantle-derivedmagmainvasionandcrust-mantlemixingactionhasoccurredonalargescale.Especially,theMiddle-LateTriassic(210~237Ma)granitoidsarepredominantandmo

7、stcloselyrelatedwithmineralization.(2)BytheLA-ICP-MSzirconU-Pbdating,thispapergetstheporphyriticgranodioriteintheZK25408borehole,(236.12±1.2Ma)Ma,whichrepresentthemagmaticcrystallizationage,belongingtotheTriassic(T2).Accordancingwiththepreviousscholars’results

当前文档最多预览五页,下载文档查看全文

此文档下载收益归作者所有

当前文档最多预览五页,下载文档查看全文
温馨提示:
1. 部分包含数学公式或PPT动画的文件,查看预览时可能会显示错乱或异常,文件下载后无此问题,请放心下载。
2. 本文档由用户上传,版权归属用户,天天文库负责整理代发布。如果您对本文档版权有争议请及时联系客服。
3. 下载前请仔细阅读文档内容,确认文档内容符合您的需求后进行下载,若出现内容与标题不符可向本站投诉处理。
4. 下载文档时可能由于网络波动等原因无法下载或下载错误,付费完成后未能成功下载的用户请联系客服处理。