| 北淮阳新元古代基性侵入岩年代学初步研究 |
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| 引用本文： | 谢智,陈江峰,张巽,李惠民,周泰禧,杨刚.北淮阳新元古代基性侵入岩年代学初步研究[J].地球学报,2002,23(6):517-520. |
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| 作者姓名： | 谢智 陈江峰 张巽 李惠民 周泰禧 杨刚 |
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| 作者单位： | 中国科学技术大学地球和空间科学学院，化学地球动力学研究实验室，安徽合肥，230026;中国科学技术大学地球和空间科学学院，化学地球动力学研究实验室，安徽合肥，230026;中国科学技术大学地球和空间科学学院，化学地球动力学研究实验室，安徽合肥，230026;中国地质调查局同位素年代学中心，天津，300170;中国科学技术大学地球和空间科学学院，化学地球动力学研究实验室，安徽合肥，230026;中国科学技术大学地球和空间科学学院，化学地球动力学研究实验室，安徽合肥，230026 |
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| 基金项目： | 国家自然科学基金（49573172和49794042）；中国科学院重点项目（KZ951-A1-401-5） |
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| 摘 要： | 大别造山带北部北淮阳褶皱带中分布少量变质变形基性侵入体,错石U-Pb研究的初步结果表明,它们的形成时代是新元古代（78±18Ma）,与北大别杂岩带中TTG片麻岩的形成时代一致。它们不仅形成时代与北大别杂岩带中基性-超基性岩不同,而且表现出与北大别杂岩带中基性侵入体不一致的主量元素地球化学信息。
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| 关 键 词： | 北淮阳 锆石U-Pb年龄 基性侵入岩 新元古代 |
Geochronology of Neoproterozoic Mafic Intrusions in North Huaiyang Area |
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| XIE Zhi,CHEN Jiang-feng,ZHANG Xun,LI Hui-min,ZHOU Tai-xi and YANG Gang.Geochronology of Neoproterozoic Mafic Intrusions in North Huaiyang Area[J].Acta Geoscientia Sinica,2002,23(6):517-520. |
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| Authors: | XIE Zhi CHEN Jiang-feng ZHANG Xun LI Hui-min ZHOU Tai-xi and YANG Gang |
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| Institution: | Laboratory for Chemical Geodynamics, Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026;Laboratory for Chemical Geodynamics, Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026;Laboratory for Chemical Geodynamics, Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026;Isotopic Geochronoiogy Center, CGU, Tianjin, 300170;Laboratory for Chemical Geodynamics, Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026;Laboratory for Chemical Geodynamics, Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, 230026 |
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| Abstract: | There are a few metamorphosed and deformed mafic intrusions in North Huaiyang area, the northernmost part of Dabie orogen. The U-Pb data presented in this paper show that they were formed in Neoprterozoic Era (784 ±18 Ma) , similar to the formation time of TTG gneisses in North Dabie terrain. Major elements in the intrusions are different from those in the mafic-ultramafic intrusions of North Dabie terrain. |
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| Keywords: | North Huaiyang metamorphic belt zircon U-Pb dating mafic intrusions Neoproterozoic |
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