[1]张光亮,温守钦,李建源.2021.内蒙古额尔古纳乌尔根矿田富碱斑岩体成因及 构造启示: 地质年代学和地球化学的证据.大地构造与成矿学,优先出版:001-24.doi:10.16539/j.ddgzyckx.2021.05.019
 ZHANG Guangliang,WEN Shouqin,LI Jianyuan and XIE Wei.2021.Petrogenesis and Tectonic Implications of Alkali-rich Porphyry in the Urgen Ore Field, Erguna Block, Inner Mongolia: Constraints from Geochronology and Geochemistry.Geotectonica et Metallogenia,优先出版:001-24.doi:10.16539/j.ddgzyckx.2021.05.019
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内蒙古额尔古纳乌尔根矿田富碱斑岩体成因及 构造启示: 地质年代学和地球化学的证据
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2021年优先出版
页码:
001-24
栏目:
出版日期:
2022-12-30

文章信息/Info

Title:
Petrogenesis and Tectonic Implications of Alkali-rich Porphyry in the Urgen Ore Field, Erguna Block, Inner Mongolia: Constraints from Geochronology and Geochemistry
作者:
张光亮1 温守钦1 李建源2 谢 伟3
1. 东北大学 地质系 深部金属矿山安全开采教育部重点实验室, 辽宁 沈阳 110819; 2. 辽宁省冶金地质勘查研究院有限责任公司, 辽宁 鞍山 114018; 3. 中国科学院地质与地球物理研究所 矿产资源研究重点实验室, 北京 100029
Author(s):
ZHANG Guangliang1 WEN Shouqin1 LI Jianyuan2 and XIE Wei3
1. Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines, Department of Geology, Northeastern University, Shenyang 110819, Liaoning, China; 2. Liaoning Metallurgical Geological Exploration Research Institute Co., Anshan 114018, Liaoning, China; 3. Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
关键词:
锆石U-Pb年代学 地球化学 富碱斑岩体 乌尔根矿田 额尔古纳地块 内蒙古
Keywords:
zircon U-Pb geochronology geochemistry alkali-rich porphyry Urgen ore field Erguna Block Inner Mongolia
分类号:
P595, P597
DOI:
10.16539/j.ddgzyckx.2021.05.019
文献标志码:
A
摘要:
乌尔根矿田由东珺浅成热液型银铅锌矿床和大加布果斯斑岩型钼矿床组成。野外地质调查揭示富碱斑岩岩浆热事件与浅成热液型银铅锌矿床时空或空间关系密切, 获得成矿期正长斑岩和成矿前石英二长斑岩岩浆锆石U-Pb年龄分别为125 Ma和165 Ma。鉴于大加布果斯斑岩型钼矿床成矿时代为147 Ma, 而浅成热液型银铅锌矿床发生在早白垩世, 进而得出两者为相对独立成矿体系。岩石地球化学特征表明, 侵入岩属偏铝质钾玄岩系列, 与A型花岗岩特征相似。富集大离子亲石元素(LILE)和轻稀土元素(LREE), 亏损高场强元素(HFSE)和重稀土元素(HREE), Eu异常(Eu/Eu=0.65~0.83)不显著, 进而说明岩浆源自富集型岩石圈地幔的部分熔融, 经历了分异结晶并遭受有限的地壳混染; 暗示矿田岩浆-成矿作用与洋壳俯冲有关, 结合区域和矿田相关研究认为中侏罗世矿田处于弧后引张环境, 而晚侏罗世-早白垩世处于蒙古-鄂霍次克洋闭合之后的伸展环境。
Abstract:
Urgen ore field, situated in the northern part of the Erguna Block, hosts the Dongjun epithermal Ag-Pb-Zn deposit and the Dajiabuguosi porphyry Mo deposit. Syenite porphyry is spatially and genetically related to the mineralization of the Dongjun deposit, whose zircon U-Pb age is 125 Ma. This finding indicates that the Dongjun deposit was formed in the Early Cretaceous, later than the formation of the Dajiabuguosi porphyry Mo deposit (mineralization age is 147 Ma). The zircon U-Pb age of quartz monzonite porphyry is 165 Ma (Middle Jurassic), suggesting it is the product of pre-metallogenic magmatism. Owing to the different mineralization ages of the Dajiabuguosi porphyry Mo deposit and Dongjun epithermal Ag-Pb-Zn deposit, we concluded they are independent metallogenic systems. The Urgen intrusions show the petrological, mineralogical, geochemical, and geotectonic characteristics of metaluminous potassium basalt series rocks, and are related to A-type granites. The rocks show enrichment in large-ion lithophile

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备注/Memo

备注/Memo:
收稿日期: 2021-04-25; 改回日期: 2021-06-25
第一作者简介: 张光亮(1988-), 男, 博士研究生, 矿产普查与勘探专业。Email: 872036720@qq.com
通信作者: 温守钦(1963-), 男, 博士, 副教授, 从事矿床地球化学研究工作。Email: wenshouqin@mail.neu.edu.cn
更新日期/Last Update: 2021-11-26