Zirzon U-Pb age and petrogenisis of plagiogranite porphyry in Changlingzi, Hexigten Banner, Inner Mongolia and its collision orogeny
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摘要:
内蒙古克什克腾旗长岭子斜长花岗斑岩位于大兴安岭锡林浩特增生杂岩带内。本文对长岭子斜长花岗斑岩进行了主微量元素地球化学以及锆石U-Pb年代学和Lu-Hf同位素研究。长岭子斜长花岗斑岩锆石206Pb/238U加权平均年龄为（248.1±4.7）Ma，是早三叠世岩浆活动的产物；继承锆石除外，样品中锆石具有正的εHf（t）值（5.78~12.41），二阶段模式年龄TDM2分别为914~488 Ma。长岭子斜长花岗斑岩具有较高的SiO2、Na2O和Al2O3含量以及较低的Fe2O3、MgO和CaO含量，属于偏铝质-过铝质的低钾-钙碱性系列I型花岗岩，富集Rb、K、U、Th、Pb、Sr等大离子亲石元素，亏损Nd、Ta、Ti等高场强元素。同时，斜长花岗斑岩具有高Sr低Y以及高Sr/Y比等特点，具有典型的埃达克质岩石特征，形成于加厚下地壳的部分熔融。综合上述地球化学特征，本文认为长岭子斜长花岗斑岩来源于加厚新生下地壳的部分熔融，表明早三叠世兴蒙地区并非岛弧的环境，而是处于碰撞造山环境，古亚洲洋在该时期已经闭合。
Abstract:The Changlingzi plagiogranite porphyry is located in the Xilinhot Late Paleozoic Accretion Complex within the Da Hinggan Mountains. This study is focused on the zircon U -Pb isotopic geochronology, Hf isotopic composition analysis and geochemistry of the Changlingzi plagiogranite porphyry. Zircon crystals from the plagiogranite porphyry yielded weighted average 206Pb/238U age of (248.1±4.7)Ma. The zircons from this porphyry have positive εHf(t) values from 5.78 to 12.41, with TDM2(Hf) ages from 914 to 488Ma. The plagiogranite porphyry has high content of SiO2, Na2O and Al2O3, and low content of TiO2, MgO and CaO, showing a metaluminous-peraluminouslow-K to calc-alkaline affinity, with LREE enrichment and HREE depletion, suggesting I-type granite. In addition, the plagiogranite porphyry has high Sr and low Y values as well as high Sr/Y ratios (74.5~103.4), indicating that the plagiogranite porphyry belongs to adakite. It is suggested that the plagiogranite porphyry was formed by partial melting of the thickened newborn lower crust. And in Early Triassic, Xing' an-Mongolian orogenic belt was in a collisionorogeny tectonic setting, indicating that the Paleo-Asian Ocean had been closed in this period.
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图 1 中国东北大地构造简图（a，据陈衍景等, 2012; Chen et al., 2016修改）及黄岗—甘珠尔庙地区地质简图（b，据芮宗瑶等, 1994修改）
Figure 1.
图 4 长岭子斜长花岗斑岩SiO2-(Na2O + K2O)图解（a，据Le Maitre, 2002）、A/CNK-A/NK图解（b，据Maniar and Piccoli, 1989）和SiO2-K2O图解（c，据Rickwood, 1989）
Figure 4.
图 5 长岭子研究区斜长花岗斑岩球粒陨石标准化稀土元素配分曲线（a）和原始地幔标准化微量元素蛛网图（b）（球粒陨石标准化值和原始地幔标准化值据Sun and McDonough, 1989）
Figure 5.
图 7 长岭子斜长花岗斑岩K2O-Na2O图解（据Collins et al., 1982）
Figure 7.
图 9 长岭子斜长花岗斑岩Sr/Y-Y图解（a, 据Martin, 1999）和（La/Yb）N-YbN图解（b, 据Defant et al., 1990）
Figure 9.
图 10 长岭子斜长花岗斑岩SiO2-Mg#（a）图解和SiO2-MgO图解（b）（据Wang et al., 2006）
Figure 10.
图 11 长岭子斜长花岗斑岩Nb−Y（a）, Ta−Yb（b）, Rb−(Y+Nb)（c）和Rb−(Yb+Ta)（d）图解（据Pearce et al., 1984, 1996；）
Figure 11.
表 1 长岭子斜长花岗斑岩全岩主量元素（%）和微量元素（10−6）分析结果
Table 1. Major (%) and trace(10−6) elements compositions of the plagiogranite porphyries in Changlingzi area
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表 2 长岭子斜长花岗斑岩锆石LA−ICP−MS U−Pb定年分析结果
Table 2. LA−ICP−MS Zircon U−Pb analysis for the plagiogranite porphyry in Changlingzi area
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表 3 长岭子研究区斜长花岗斑岩锆石Lu−Hf同位素分析结果
Table 3. Zircon Lu−Hf isotope analysis for the plagiogranite porphyry in Changlingzi area
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