文章摘要
龙灵利,王京彬,王玉往,毛启贵,邓小华,赵路通,孙志远,孙燕,高一涵.东天山卡拉塔格矿集区赋矿火山岩地层时代探讨——SHRIMP锆石U-Pb年龄证据[J].矿产勘查,2016,7(1):31-37
东天山卡拉塔格矿集区赋矿火山岩地层时代探讨——SHRIMP锆石U-Pb年龄证据
Discussion on the age of ore-host volcanic strata in the Kalatage ore concentration area, eastern Tianshan:Evidence from SHRIMP zircon U-Pb dating
投稿时间:2015-09-07  
DOI:
中文关键词: 新疆  东天山  卡拉塔格  火山岩  闪长玢岩  锆石U-Pb年代学
英文关键词: volcanic rock, diorite porphyrite, zircon U-Pb age, eastern Tianshan, Xinjiang, Kalatage
基金项目:国家重点基础发展研究计划项目(编号:2014CB440803)、国家自然科学基金(编号:41202064、41372102、41572077)和中国地调局项目(编号:12120114081701)联合资助。 
作者单位
龙灵利 北京矿产地质研究院,北京 100012 
王京彬 北京矿产地质研究院,北京 100012 
王玉往 北京矿产地质研究院,北京 100012 
毛启贵 北京矿产地质研究院,北京 100012 
邓小华 北京矿产地质研究院,北京 100012 
赵路通 北京矿产地质研究院,北京 100012 
孙志远 北京矿产地质研究院,北京 100012 
孙燕 北京矿产地质研究院,北京 100012 
高一涵 北京矿产地质研究院,北京 100012 
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中文摘要:
      新疆东天山卡拉塔格矿集区内发育有红海(—黄土坡)大型VMS型铜锌矿床、红石—梅岭热液脉状铜矿床、玉带斑岩型铜矿床等,其赋矿围岩均为一套多旋回火山—沉积岩系。文章获得侵入该岩系下部岩性段中闪长玢岩SHRIMP锆石U-Pb年龄为(442.6±5.3)Ma和(437.1±3.8)Ma,其精确限定了该岩性段形成时代上限为晚奥陶世,表明这套含矿岩系最早可能形成于奥陶纪。
英文摘要:
      The large sized Honghai (-Huangtupo) VMS type Cu-Zn deposit, Hongshi-Meiling hydrothermal vein type copper deposit and Yudai porphyry type copper deposit occur in the Kalatage ore concentration area, eastern Tianshan district, Xinjiang. The area possesses various genetic types of deposits,such as the ore-host rocks consist of series of volcanic-sedimentary rocks with complex volcanic cycles. The U-Pb age measurement results by the high precise SHRIMP method of zircon samples collected from diorite porphyrite which intruded into the bottom of the ore-host rocks in the Kalatage ore concentration area, are(442.6±5.3) Ma and(437.1±3.8) Ma respectively, which precisely defined the upper limit of the age of the lower section of the ore-host volcanic rocks is late Ordovician, it indicates the ore- host volcanic rocks were formed in the earlier Ordovician period.
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