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首页|期刊导航|地质学报|滇中老街子Pb-Ag多金属矿床的成矿时代及成矿动力学背景探讨:来自硫化物Re-Os同位素证据

滇中老街子Pb-Ag多金属矿床的成矿时代及成矿动力学背景探讨:来自硫化物Re-Os同位素证据

江小均 严清高 李文昌 李超 吴鹏 管申进 余海军 李金龙

地质学报2018,Vol.92Issue(6):1280-1296,17.
地质学报2018,Vol.92Issue(6):1280-1296,17.

滇中老街子Pb-Ag多金属矿床的成矿时代及成矿动力学背景探讨:来自硫化物Re-Os同位素证据

The Metallogenic Age and Geodynamic Setting of the Laojiezi Pb-Ag Polymetallic Deposit, Central Yunnan Province:Evidence from Re-Os Isotope of Sulfides

江小均 1严清高 1李文昌 1李超 2吴鹏 3管申进 1余海军 1李金龙4

作者信息

  • 1. 昆明理工大学国土资源工程学院地球科学系,昆明,650093
  • 2. 中国地质调查局成都地质调查中心,成都,610081
  • 3. 国家地质实验测试中心,北京,10037
  • 4. 云南省地质调查局,昆明,650051
  • 折叠

摘要

Abstract

The Laojiezi Pb-Ag deposit,located in the middle section of the Cenozoic Red River-Ailaoshan alkali-rich porphyry belt,is the typical alkali-rich volcanic-magmatic hydrothermal deposit in central Yunnan province.A 70-m-wide syenite porphyry and molybdenite-pyrite vein with high Cu-Mo abnormal pyritization was firstly discovered in the deep part of the deposits (3 # vein of 2073 level).It is believed that obvious alkali-rich porphyry and magmatic-hydrothermal Cu-Mo superimposed mineralization occurs at depth of the deposit.This study conducted Re-Os isotopic analysis for molybdenite-pyrite samples from molybdenite-pyrite veins,pyrite-galena veins and high Cu-Mo syenite porphyry from deep adits in the Laojiezi Pb-Ag deposits.An isochron age of 33.71 ± 0.29Ma and a weighted average age of 33.99 ± 0.22Ma were obtained for molybdenite,indicating that the mineralization of the Pb-Ag polymetallic deposit took place in Oligocene,which is consistent with the diagenetic age of the syenite porphyry.The initial Os value of 0.3049 ~ 1.5549 and the γOs value of 140.5 ~ 1126 suggest that the metallogenic material was derived from partial melting of the crust-mantle transition layer.The metallogenic age of the Laojiezi porphyry Pb-Ag polymetallic deposit is roughly the same as that (30 ~ 40 Ma) of regional alkali-rich porphyry and magmatic hydrothermal polymetallic deposits.It shows that,after the collision between the India plate and Eurasia plate,the change of tectonic stress field resulted in large-scale strike-slip faulting system,which induced partial melting of crust-mantle transition zone within the stable cratons,forming alkali-rich intrusive rocks and metallogenic fluids,and the fluid formed alkali-rich porphyry and magmatic-hydrothermal polymetallic deposits along the weak structures.

关键词

滇中/老街子Pb-Ag多金属矿床/Re-Os同位素/成矿动力学

Key words

Central Yunnan/Laojiezi Pb-Ag deposits/Re-Os isotope/metallogenic geodynamic

引用本文复制引用

江小均,严清高,李文昌,李超,吴鹏,管申进,余海军,李金龙..滇中老街子Pb-Ag多金属矿床的成矿时代及成矿动力学背景探讨:来自硫化物Re-Os同位素证据[J].地质学报,2018,92(6):1280-1296,17.

基金项目

本文为北京离子探针中心开放基金(DDC15-016)、国家重点基础研究发展计划(973计划)(编号:2015CB452605)、云南省应用基础研究计划青年(2016DF031)和云南省科技领军人才培养计划(编号:2013HA001)等项目联合资助. (DDC15-016)

地质学报

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