内蒙古白音诺尔铅锌矿床成矿时代及其地质意义——来自侵入岩地球化学及年代学的制约

doi:10.13278/j.cnki.jjuese.20170228

吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (6): 1696-1710.doi: 10.13278/j.cnki.jjuese.20170228

内蒙古白音诺尔铅锌矿床成矿时代及其地质意义——来自侵入岩地球化学及年代学的制约

杨帆^1,2, 汪岩¹, 那幅超¹, 付俊彧¹, 张广宇¹, 孙巍¹, 庞雪娇¹, 陈井胜¹, 刘淼¹, 李斌¹

1. 中国地质调查局沈阳地质调查中心, 沈阳 110034;
2. 吉林大学地球科学学院, 长春 130061

收稿日期:2017-09-11 出版日期:2018-11-26 发布日期:2018-11-26
通讯作者: 张广宇(1981-),男,博士研究生,主要从事地理信息系统方面的研究,E-mail:zhgy1981@126.com E-mail:zhgy1981@126.com
作者简介:杨帆(1987-),男,博士研究生,工程师,主要从事区域地质、矿产方面的研究,E-mail:541810741@qq.com
基金资助:
中国地质调查局项目（DD20160048-1，DD20160343-08，DD20160048-16，DD20160201-01）

Geological Significance and Metallogenic Epoch of the Baiyinnuoer Pb-Zn Deposit in Inner Mongolia: Constraints from Geochemistry and Chronology of Intrusive Rocks

Yang Fan^1,2, Wang Yan¹, Na Fuchao¹, Fu Junyu¹, Zhang Guangyu¹, Sun Wei¹, Pang Xuejiao¹, Chen Jingsheng¹, Liu Miao¹, Li Bin¹

1. Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China

Received:2017-09-11 Online:2018-11-26 Published:2018-11-26
Supported by:
Supported by Project of China Geological Survey(DD20160048-1,DD20160343-08,DD20160048-16,DD20160201-01)

摘要/Abstract

摘要： 内蒙古白音诺尔铅锌矿床位于大兴安岭成矿带南段，是一个典型的矽卡岩型矿床。为了精确厘定该矿床的成矿时代，对区内与成矿关系密切的花岗闪长斑岩及流纹斑岩中的锆石进行了LA-ICP-MS定年，获得花岗闪长斑岩与流纹斑岩的形成年龄分别为（253.4±0.9）Ma和（133.6±0.7）Ma。岩石地球化学研究表明，花岗闪长斑岩为准铝质岩石，流纹斑岩为过铝质岩石，两者均具有轻重稀土分异明显、富集大离子亲石元素（LILE）、相对亏损高场强元素（HFSE）的特点。结合矿床地质特征及前人在区域上的研究成果，认为白音诺尔铅锌矿床存在两期明显的矿化事件，早期矿化发生在253.4 Ma左右，晚期矿化发生在133.6 Ma左右。白音诺尔铅锌矿床早期矿化很可能与古亚洲洋闭合碰撞后伸展有关，晚期矿化受蒙古-鄂霍茨克洋俯冲的影响。

关键词: 矽卡岩型矿床, LA-ICP-MS锆石定年, 侵入岩, 地球化学, 白音诺尔铅锌矿床, 内蒙古

Abstract: Located in the south section of the Daxing'anling metallogenic belt, the Baiyinnuoer Pb-Zn deposit is a typical skarn deposit. In order to determine the mineralization age of the deposit, LA-ICP-MS U-Pb dating of zircons in the granodiorite porphyry and rhyolite porphyry associated with the mineralization was studied. The results suggest that the granodiorite and rhyolite porphyry were crystallized in (253.4±0.9) Ma and (133.6±0.7) Ma. The rock geochemistry indicates that the granodiorite is quasi-aluminous,and the rhyolite porphyry is excessive-aluminous. Both of them are characterized by fractionation of HREE and LREE, enrichment of large ion lithophile elements (LILE) and relative depletion of high field strength elements (HFSE). Combined with the geological characteristics and the previous research in this region, we conclude that two mineralization events occurred in the deposit with the early mineralization at about 253.4 Ma and the late one at about 133.6 Ma. The early mineralization may be related to the closure of the Paleo-Asian Ocean and the late mineralization was influenced by the subduction of the Mongolia-Okhotsk Ocean. The Baiyinnuoer Pb-Zn deposit was formed in the post-collisional extension.

Key words: skarn deposit, LA-ICP-MS zircon U-Pb chronology, intrusive rock, geochemistry, Baiyinnuoer Pb-Zn deposit, Inner Mongolia

中图分类号:

P618.4

杨帆, 汪岩, 那幅超, 付俊彧, 张广宇, 孙巍, 庞雪娇, 陈井胜, 刘淼, 李斌. 内蒙古白音诺尔铅锌矿床成矿时代及其地质意义——来自侵入岩地球化学及年代学的制约[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1696-1710.

Yang Fan, Wang Yan, Na Fuchao, Fu Junyu, Zhang Guangyu, Sun Wei, Pang Xuejiao, Chen Jingsheng, Liu Miao, Li Bin. Geological Significance and Metallogenic Epoch of the Baiyinnuoer Pb-Zn Deposit in Inner Mongolia: Constraints from Geochemistry and Chronology of Intrusive Rocks[J]. Journal of Jilin University(Earth Science Edition), 2018, 48(6): 1696-1710.

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内蒙古白音诺尔铅锌矿床成矿时代及其地质意义——来自侵入岩地球化学及年代学的制约

Geological Significance and Metallogenic Epoch of the Baiyinnuoer Pb-Zn Deposit in Inner Mongolia: Constraints from Geochemistry and Chronology of Intrusive Rocks

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