|Table of Contents|

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

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

Issue:
2023年第05期
Page:
1149-1161
Research Field:
庆贺汤中立院士从事地质工作七十周年专辑
Publishing date:

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
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)
Keywords:
metallogenic chronology;  polymetallic sulfide;  Rb-Sr isochron age;  subvolcanic complex;  provenance;  tectonic evolution;  Shandong
PACS:
P597; P611
DOI:
10.19814/j.jese.2022.12062
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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