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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第46卷

期数:

2024年第05期

页码:

606-635

栏目:

基础地质与矿床地质

出版日期:

2024-09-30

文章信息/Info

Title:

Sedimentary Provenance and Geochronology of Jianshan Formation in Bayan Obo Ore District, the Northern Margin of North China Craton and Their Geological Significance

文章编号:

1672-6561(2024)05-0606-30

作者:

杨建军¹; 王东升^2*; 佘宏全²; 李以科²; 杨月后¹; 柯昌辉²; 张 丽³; 赵 剑⁴; 赵 阳⁴; 郭 宾³

(1. 内蒙古自治区地质调查研究院 内蒙古自治区岩浆活动成矿与找矿重点实验室,内蒙古 呼和浩特 010020; 2. 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; 3. 包钢(集团)公司白云鄂博铁矿,内蒙古 包头 014080; 4. 内蒙古包钢钢联股份有限公司巴润矿业分公司,内蒙古 包头 014080)

Author(s):

YANG Jian-jun¹;  WANG Dong-sheng^2*;  SHE Hong-quan²;  LI Yi-ke²;  YANG Yue-hou¹;  KE Chang-hui²;  ZHANG Li³;  ZHAO Jian⁴;  ZHAO Yang⁴;  GUO Bin³

(1. Inner Mongolia Key Laboratory of Magmatic Mineralization and Ore-prospecting, Inner Mongolia Geological Survey Institute, Hohhot 010020, Inner Mongolia, China; 2. MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 3. Bayan Obo Iron Mine, Baotou Iron and Steel Company, Baotou 014080, Inner Mongolia, China; 4. Barun Mining Co. of Steel Union Co. Ltd. of Baotou Steel(Group)Corp., Baotou 014080, Inner Mongolia, China)

关键词:

变沉积岩;  锆石U-Pb年龄;  太古代—元古代;  沉积源区;  热液改造;  尖山组;  华北克拉通

Keywords:

meta-sedimentary rock;  zircon U-Pb age;  Archean-Proterozoic;  sedimentary provenance;  hydrothermal alteration;  Jianshan Formation;  North China Craton

分类号:

P548

DOI:

10.19814/j.jese.2024.03004

文献标志码:

A

摘要:

白云鄂博矿床位于华北克拉通北缘,其围岩尖山组为一套绿片岩相硅质碎屑岩组合,尖山组的形成时代及物源研究对于理解区域大地构造演化和成矿过程具有重要意义。采用LA-ICP-MS方法对矿区尖山组的变质砂岩及变质细砂岩进行了锆石U-Pb年代学研究。变质细砂岩样品Z5246的锆石年龄为2 645～1 147 Ma,包含两个主峰值年龄,分别为2 510和1 390 Ma; 变质砂岩样品By23281锆石年龄为2 722～1 847 Ma,包含3个主峰值年龄,分别为2 487、1 925和1 859 Ma。结合锆石稀土元素特征,认为变质砂岩样品By23281中2 722～1 847 Ma的锆石属于未受热液改造的碎屑锆石,尖山组的形成时代应晚于1 847 Ma; 而结合野外特征、锆石形貌及稀土元素特征,认为变质细砂岩样品Z5246中1 761～1 147 Ma的年龄反映了后期热液改造的过程,也进一步佐证了白云石碳酸岩的岩浆成因。结合矿区及周边已有的年代学数据,认为矿区尖山组物源主要来自华北克拉通北缘太古宙基底和古元古代晚期的变质岩,最终形成于中元古代,之后受到白云石碳酸岩岩浆期热液的明显改造。矿区尖山组碎屑岩的年龄数据记录了华北克拉通北缘太古代—元古代的陆壳增生、碰撞及裂解事件,为研究太古代—元古代区域构造演化提供了有力证据。

Abstract:

The Bayan Obo ore deposit is located in the northern margin of North China Craton, and its country rock, Jianshan Formation, is a set of greenschist facies rocks formed by regional metamorphism. The study on its formation age and provenance is of great significance for understanding the regional tectonic evolution. LA-ICP-MS zircon U-Pb geochronology was conducted on the metasandstone and metamorphic fine sandstone within Jianshan Formation. The zircon ages from metamorphic fine sandstone range from 2 645 Ma to 1 147 Ma, including two main peak ages of 2 510 Ma and 1 390 Ma, respectively. The zircon ages from metasandstone range from 2 722 Ma to 1 847 Ma, including three main peak ages of 2 487 Ma, 1 925 Ma, and 1 859 Ma, respectively. Based on the REE characteristics of zircons, it is believed that zircons of sample By23281 displaying ages from 2 722 Ma to 1 847 Ma belong to typical detrital zircons and the formation age of Jianshan Formation should be later than 1 847 Ma. Based on the field characteristics, REE and morphology of zircons, the 1 761-1 147 Ma age of sample Z5246 represents the process of subsequent hydrothermal alteration, further confirming the magmatic origin of dolomitic carbonate. Based on the previous chronological data in the ore district and its periphery, it is advocated that Jianshan Formation is ultimately formed in the Mesoproterozoic, with its material sources coming from the Archean basement on the northern margin of North China Craton and metamorphic rocks from the Late Paleoproterozoic. In the Mesoproterozoic, Jianshan Formation is significantly altered by post-magmatic hydrothermal alteration of dolomitic carbonate. The ages of the clastic rocks in Bayan Obo ore district record the crustal accretion, collision and break-up events at the northern margin of North China Craton, providing powerful evidence for the study on the regional tectonic evolution during Archean-Proterozoic.

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备注/Memo

备注/Memo:

收稿日期:2024-03-03; 修回日期:2024-06-22
基金项目:国家重点研发计划项目(2022YFC2905301); 内蒙古自治区自然资源厅项目(150000235053210000203); 国家自然科学基金项目(42072114); 中国地质科学院矿产资源研究所科技成果转化项目(HE2224,HE2228,HE2313,HE2333)
*通信作者:王东升(1988-),男,河南濮阳人,副研究员,理学博士,E-mail:wangdsyzy@126.com。

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