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新疆中亚造山带铁矿床地质特征、时空分布和找矿方向

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在前人研究和野外调查基础上,文章综述了新疆中亚造山带铁及铁多金属矿地质特征、时空分布规律、构造环境和找矿方向.铁及铁多金属矿主要为岩浆型、海相火山岩型、矽卡岩型、IOCG型、岩浆热液脉型、沉积变质型和沉积型,其中海相火山岩型和矽卡岩型是主要类型,主要分布于南阿尔泰、东天山和西天山,少量分布在准噶尔、北山和西南天山.6个主要成矿期:新元古代青白口纪、中-晚志留世、泥盆纪(376~411 Ma)、石炭纪(301~337 Ma)、早-中二叠世(262~295 Ma)和晚三叠世—中侏罗世,其中泥盆纪和石炭纪为主要成矿期.新疆中亚造山带在前寒武纪陆块、洋-陆俯冲增生、陆-陆碰撞、后造山伸展和陆内等地质过程形成了不同类型的铁矿床.泥盆纪—石炭纪为与板块俯冲有关的大洋岛弧和陆缘弧环境,主要形成海相火山岩型和矽卡岩型;二叠纪为后碰撞环境,主要形成岩浆型和矽卡岩型;晚三叠世—中侏罗世为陆内伸展环境.今后的找矿部署是主攻西天山阿吾拉勒,深化南阿尔泰、东天山阿齐山-雅满苏-沙泉子和梧桐沟-天湖矿集区,加快评价准噶尔北缘、伊什基里克和莫托沙拉-库米什矿集区.
A review of geological characteristics,spatiotemporal distribution and prospecting direction of iron deposits in Central Asian Orogenic Belt,Xinjiang
This paper reviews the geological characteristics,spatiotemporal distribution,tectonic settings,and prospec-ting direction of iron and polymetallic deposits in the Xinjiang Central Asian Orogenic Belt(XCAOB).We recog-nize seven types of iron and polymetallic deposits in the XCAOB:magmatic,submarine volcanogenic,skarn,iron oxide-copper-old(IOCG),magmatic-hydrothermal vein,sedimentary-metamorphic,and sedimentary.Of these types,submarine volcanogenic and skarn deposits are the most common.The iron and polymetallic deposits are largely distributed in South Altay,East Tianshan,and West Tianshan,with minor deposits in Junggar,Beishan,and Southwest Tianshan.The ore formation in iron and polymetallic deposits can be divided into six mineraliza-tion phases:Neoproterozoic Qingbaikouan,Middle-Late Silurian,Devonian(376~411 Ma),Carboniferous(301~337 Ma),Early-Middle Permian(262~295 Ma),and Late Triassic-Middle Jurassic.Among these phases,the De-vonian and Carboniferous were the main mineralization phases.Different types of iron and polymetallic deposits were formed in the Precambrian continent,ocean-continent subduction accretion,continental-continent collision orogen,post-orogenic extension,and intracontinental geological processes in the XCAOB.The Devonian to Car-boniferous was an oceanic island arc and marginal arc environment related to plate subduction,which mainly formed submarine volcanogenic and skarn deposits,the Permian was a post-collision environment,which mainly formed magmatic and skarn deposits,and Late Triassic to Middle Jurassic was an intracontinental extensional en-vironment.The future prospecting plan is to focus on the West Tianshan Awulale,deepen the South Altai,East Tianshan Aqishan-Yamansu-Shaquanzi and Wutonggou-Tianhu ore dense districts,speeds up the evaluation of the northern margin of the Junggar,Yishijilike,and Motuosala-Kumishi ore dense districts.

iron depositsgeological characteristicstime-space distributionCentral Asian Orogenic BeltXinjiang

杨富全、耿新霞、杨成栋、张志欣、王成、李守能、李强

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中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室,北京 100037

中国科学院新疆生态与地理研究所新疆矿产资源研究中心,新疆乌鲁木齐 830011

新疆维吾尔自治区人民政府国家305项目办公室,新疆乌鲁木齐 830000

贵州省地质矿产勘查开发局115地质大队,贵州贵阳 551400

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铁矿床 地质特征 时空分布 中亚造山带 新疆

地质调查项目地质调查项目第三次新疆科考项目国土资源部公益性行业科研专项经费项目

DD20240117DD202216842022xjkk1301-10201211073

2024

矿床地质
中国地质学会矿床地质专业委员会 中国地质科学院矿床地质研究所

矿床地质

CSTPCD北大核心
影响因子:2.163
ISSN:0258-7106
年,卷(期):2024.43(5)