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冈底斯斑岩铜矿带冲江及驱龙含矿斑岩体锆石ELA-ICP-MS及SHRIMP定年对比研究

COMPARISON OF ELA-ICP-MS AND SHRIMP U-PB ZIRCON AGES OF THE CHONGJIANG AND QULONG ORE-BEARING PORPHYRIES IN THE GANGDESE PORPHYRY COPPER BELT

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【作者】 莫济海梁华英喻亨祥谢应雯张玉泉

【Author】 MO Jihai 1,2 , LIANG Huaying1, YU Hengxiang3, XIE Yingwen1 and ZHANG Yuquan1 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Graduate School, Chinese Academy of Sciences, Beijing 100039, China; 3. Guilin Institute of Technology, Guilin, GX 541004, China)

【机构】 中国科学院广州地球化学研究所中国科学院研究生院 北京100039桂林工学院广东广州510640广西桂林541004

【摘要】 利用ELA-ICP-MS分析技术对冈底斯斑岩铜矿带冲江及驱龙含矿斑岩体进行锆石U-Pb年龄测定,所得到的年龄分别为14.0±0.2Ma和17.0±0.2Ma。两个含矿岩体锆石ELA-ICP-MSU-Pb年龄和SHRIMP年龄在误差范围内基本一致。冲江含矿斑岩体成岩成矿可分为两期,每期成岩成矿时间跨度约1Ma;驱龙含矿斑岩体成岩成矿时间跨度约为1Ma。

【Abstract】 New zircon U-Pb ages of the Chongjiang and the Qulong ore-bearing porphyries in the Gangdese porphyry copper belt are analyzed by using ELA-ICP-MS dating technique. The ages for the early stages of both Chongjiang and the Qulong ore-bearing porphyries are 14.0±0.2 Ma and 17.0±0.2 Ma, respectively. Here the zircon ELA-ICP-MS U-Pb ages are similar to the SHRIMP U-Pb ages within error, suggesting that the ELA-ICP-MS method can be used to precisely date the ages of young zircon grains. The data also imply that the Chongjiang ore-bearing porphyry may undergo two stages of magma-ore-forming processes and the lifespan of each stage lasts about 1 Ma, and that the lifespan of the Qulong magmatic ore-formation system lasts about 1 Ma.

【基金】 国家自然科学基金项目(40472049);中国科学院广州地球化学研究所创新项目(GIG-CX-040-03)资助.
  • 【文献出处】 大地构造与成矿学 ,Geotectonica Et Metallogenia , 编辑部邮箱 ,2006年04期
  • 【分类号】P597.3
  • 【被引频次】50
  • 【下载频次】708
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