SUO QingYu, LI ChangHao, SHEN Ping, ZHAO JunKang, CHU XiangKai
{"title":"黑龙江多宝山铜(钼)矿床的叠加成矿作用:辉钼矿Re-Os同位素测年和硫同位素组成指示","authors":"SUO QingYu, LI ChangHao, SHEN Ping, ZHAO JunKang, CHU XiangKai","doi":"10.18654/1000-0569/2023.11.16","DOIUrl":null,"url":null,"abstract":"斑岩型矿床易受后期岩浆、构造、变质等地质作用影响,使得矿床自身发生改造变形。后期的热事件不仅可以将原有矿体再活化,还能够带来新的成矿物质,进而发生新一期成矿作用。不同地质时期的成矿作用在同一空间互相叠加,会形成与斑岩矿床矿化特征截然不同的矿床,称为叠加改造型斑岩矿床。多宝山铜(钼)矿床位于中亚造山带东段,兴蒙造山带内。该矿床在成矿构造地质、矿石组构和成矿期次等方面表现出多期改造与叠加成矿的特征。本次根据野外观察和成矿年代学研究,推测多宝山铜矿至少存在两期成矿作用。对采自矿坑340平台10件叠加矿化类型的辉钼矿样品进行Re-Os同位素分析,获得辉钼矿的模式年龄介于435.6±10.5Ma~446.1±7.1Ma之间,等时线年龄为440.1±4.5Ma (MSWD=0.56)。结合前人获得的年龄资料,确认多宝山叠加成矿与晚奥陶世玄武安山岩应形成于统一的成岩成矿地质事件。不同矿化期次的黄铜矿和黄铁矿原位硫同位素结果显示:典型斑岩型矿脉中黄铜矿<i>δ</i><sup>34</sup>S平均值为-2.12‰;叠加矿化黄铜矿<i>δ</i><sup>34</sup>S平均值为-1.78‰,黄铁矿<i>δ</i><sup>34</sup>S平均值为-1.03‰,均落入幔源硫范围,表明硫主要来自岩浆。而前人在叠加期形成的黄铜矿中,测试到较低的<i>δ</i><sup>34</sup>S值(-12.9‰~-5.6‰),这是后期流体易携带轻硫<sup>32</sup>S发生迁移并在应力较低的区域内重新沉淀的结果。同位素组成指示叠加成矿期的矿化元素即来源于新的岩浆活动,又继承了先前存在的岩(矿)体。","PeriodicalId":7075,"journal":{"name":"岩石学报","volume":"15 1","pages":"0"},"PeriodicalIF":1.7000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Superimposed mineralization of the Duobaoshan Cu(Mo) deposit in Heilongjiang Province: Indicated by the molybdenite Re-Os isotopic dating and sulfur isotope composition\",\"authors\":\"SUO QingYu, LI ChangHao, SHEN Ping, ZHAO JunKang, CHU XiangKai\",\"doi\":\"10.18654/1000-0569/2023.11.16\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"斑岩型矿床易受后期岩浆、构造、变质等地质作用影响,使得矿床自身发生改造变形。后期的热事件不仅可以将原有矿体再活化,还能够带来新的成矿物质,进而发生新一期成矿作用。不同地质时期的成矿作用在同一空间互相叠加,会形成与斑岩矿床矿化特征截然不同的矿床,称为叠加改造型斑岩矿床。多宝山铜(钼)矿床位于中亚造山带东段,兴蒙造山带内。该矿床在成矿构造地质、矿石组构和成矿期次等方面表现出多期改造与叠加成矿的特征。本次根据野外观察和成矿年代学研究,推测多宝山铜矿至少存在两期成矿作用。对采自矿坑340平台10件叠加矿化类型的辉钼矿样品进行Re-Os同位素分析,获得辉钼矿的模式年龄介于435.6±10.5Ma~446.1±7.1Ma之间,等时线年龄为440.1±4.5Ma (MSWD=0.56)。结合前人获得的年龄资料,确认多宝山叠加成矿与晚奥陶世玄武安山岩应形成于统一的成岩成矿地质事件。不同矿化期次的黄铜矿和黄铁矿原位硫同位素结果显示:典型斑岩型矿脉中黄铜矿<i>δ</i><sup>34</sup>S平均值为-2.12‰;叠加矿化黄铜矿<i>δ</i><sup>34</sup>S平均值为-1.78‰,黄铁矿<i>δ</i><sup>34</sup>S平均值为-1.03‰,均落入幔源硫范围,表明硫主要来自岩浆。而前人在叠加期形成的黄铜矿中,测试到较低的<i>δ</i><sup>34</sup>S值(-12.9‰~-5.6‰),这是后期流体易携带轻硫<sup>32</sup>S发生迁移并在应力较低的区域内重新沉淀的结果。同位素组成指示叠加成矿期的矿化元素即来源于新的岩浆活动,又继承了先前存在的岩(矿)体。\",\"PeriodicalId\":7075,\"journal\":{\"name\":\"岩石学报\",\"volume\":\"15 1\",\"pages\":\"0\"},\"PeriodicalIF\":1.7000,\"publicationDate\":\"2023-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"岩石学报\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18654/1000-0569/2023.11.16\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"岩石学报","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18654/1000-0569/2023.11.16","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOLOGY","Score":null,"Total":0}
Superimposed mineralization of the Duobaoshan Cu(Mo) deposit in Heilongjiang Province: Indicated by the molybdenite Re-Os isotopic dating and sulfur isotope composition
岩石学报Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
3.60
自引率
22.20%
发文量
5997
审稿时长
6 months
期刊介绍：
Acta Petrologica Sinica is an academic journal under the supervision of the Chinese Academy of Sciences and sponsored by the Chinese Society of Mineralogy, Petrology and Geochemistry and the Institute of Geology and Geophysics of the Chinese Academy of Sciences. The journal's publishing policy is to adhere to innovation, comprehensiveness, cutting-edge and orientation, advocate diversity and multi-school, rely on and unite the vast number of geoscientists across the country, explore the mysteries of nature, carry out extensive and in-depth basic theoretical research, promote the research and development of the field of earth science in my country, publish high-level scientific research results, and cultivate and train a large number of geoscientific research talents for my country.
Acta Petrologica Sinica mainly reports on various disciplines related to the basic theory of petrology, including important basic theories and applied research results in magmatic petrology, metamorphic petrology, sedimentary petrology, petrology geotectonics, rock isotope chronology and isotope geochemistry, rock mineralization, and rock-forming mineralogy. At the same time, the journal also publishes review articles, problem discussions, academic trends and book reviews.
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
