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

卷:

第45卷

期数:

2023年第05期

页码:

1149-1161

栏目:

庆贺汤中立院士从事地质工作七十周年专辑

出版日期:

2023-09-15

文章信息/Info

Title:

Rb-Sr Age of Sulfides of Qibaoshan Polymetallic Deposit in Wulian Area, the Southern Margin of Jiaolai Basin, China and Its Geological Significance

文章编号:

1672-6561(2023)05-1149-13

作者:

李双飞¹; 2; 陈 建¹; 2; 唐名鹰¹; 2; 3*; 朱 伟¹; 2; 丁正江³; 4; 黄 鹂¹; 2; 邹占春¹; 2; 孙丽莎¹; 2; 彭永和¹; 2; 丁文洁¹; 2

(1. 山东省第八地质矿产勘查院,山东 日照 276826; 2. 山东省地质矿产勘查开发局有色金属找矿与资源评价重点实验室,山东 日照 276826; 3. 山东省深部金矿探测大数据应用开发工程实验室,山东 威海 264209; 4. 山东省第六地质矿产勘查院,山东 威海 264209)

Author(s):

LI Shuang-fei¹; 2;  CHEN Jian¹; 2;  TANG Ming-ying¹; 2; 3*;  ZHU Wei¹; 2;  DING Zheng-jiang³; 4;  HUANG Li¹; 2;  ZOU Zhan-chun¹; 2;  SUN Li-sha¹; 2;  PENG Yong-he¹; 2;  DING W

(1. No.8 Institute of Geology and Mineral Resources Exploration of Shandong Province, Rizhao 276826, Shandong, China; 2. Key Laboratory of Nonferrous Metal Ore Exploration and Resource Evaluation, Shandong Provincial Bureau of Geology & Mineral Resources, Rizhao 276826, Shandong, China; 3. Shandong Provincial Engineering Laboratory of Application and Development of Big Data for Deep Gold Exploration, Weihai 264209, Shandong, China; 4. No.6 Institute of Geology and Mineral Resources Exploration of Shandong Province, Weihai 264209, Shandong, China)

关键词:

成矿年代学;  多金属硫化物;  Rb-Sr等时线年龄;  次火山杂岩体;  物源;  构造演化;  山东

Keywords:

metallogenic chronology;  polymetallic sulfide;  Rb-Sr isochron age;  subvolcanic complex;  provenance;  tectonic evolution;  Shandong

分类号:

P597; P611

DOI:

10.19814/j.jese.2022.12062

文献标志码:

A

摘要:

胶莱盆地南缘五莲地区七宝山多金属矿床赋存于七宝山火山机构,围岩为早白垩世七宝山次火山杂岩体。因缺乏精确的成矿年代学研究,该矿床的成因争议较大。选取了7件硫化物样品进行Rb-Sr等时线年龄的测定,分析该矿床形成时代。结果表明:方铅矿、闪锌矿、黄铁矿的⁸⁷Rb/⁸⁶Sr值和⁸⁷Sr/⁸⁶Sr值分别为0.114 5～3.602 0和0.711 231～0.716 895,两者具线性关系,获得良好线性关系的Rb-Sr等时线年龄为(113.9±2.1)Ma,成矿年龄略晚于最晚期侵入体石英闪长玢岩的年龄(124.1 Ma),说明七宝山多金属矿床的形成与石英闪长玢岩有关; 硫化物初始Sr同位素比值介于0.710 98～0.711 15,处于地壳(>0.719 0)与地幔(<0.704 0)之间,指示成矿物质来源于壳幔混合。结合前人对胶东中生代地球动力学背景的研究,七宝山次火山杂岩体及赋存其中的七宝山多金属矿床应为华北东部中生代晚期构造体制转折和岩石圈大规模破坏、拆沉作用的产物。

Abstract:

Qibaoshan polymetallic deposit in Wulian area, the southern margin of Jiaolai Basin, occurs in Qibaoshan volcanic structure, and the surrounding rock is Early Cretaceous Qibaoshan subvolcanic complex. However, the genesis of the deposit is controversial because of the lack of accurate metallogenic geochronology. In order to determine the accurate age of the deposit, 7 sulphide samples were selected for Rb-Sr age determination. The results show that the ratios of ⁸⁷Rb/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr are 0.114 5-3.602 0 and 0.711 231-0.716 895, respectively; the Rr-Sr isochronal age of galena, sphalerite and pyrite with good linear relationship is(113.9 ± 2.1)Ma, which is slightly later than that of quartz diorite porphyrite(124.1 Ma), indicating that Qibaoshan polymetallic deposit is related to quartz diorite porphyrite. The initial Sr isotope ratios of sulfide are 0.710 98-0.711 15, between the values of crust(>0.719 0)and mantle(>0.704 0), indicating that the ore-forming material comes from crust-mantle mixture. The mineralization age of Qibaoshan polymetallic deposit is consistent with that of Qibaoshan subvolcanic complex, indicating that the diagenesis and mineralization of Qibaoshan subvolcanic complex occur simultaneously, which is the product of volcanic activity. Based on previous studies on Mesozoic geodynamics in the eastern Shandong, it is concluded that Qibaoshan subvolcanic complex and Qibaoshan polymetallic deposit in it are the products of the tectonic system transition and the large-scale destruction and subsidence of the lithosphere in the eastern North China during Late Mesozoic.

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备注/Memo

备注/Memo:

收稿日期:2022-12-27; 修回日期:2023-04-09投稿网址:http:∥jese.chd.edu.cn/
基金项目:山东省自然资源厅项目(鲁勘字[2020]18号); 山东省地质矿产勘查开发局项目(KY202213)
作者简介:李双飞(1987-),男,山东省第八地质矿产勘查院高级工程师,E-mail:251853543@qq.com。
*通讯作者:唐名鹰(1990-),男,山东省第八地质矿产勘查院工程师,E-mail:353635085@qq.com。

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