The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example
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摘要: 在全球岩浆活动静寂期，人们在华北克拉通内相继识别出大量~2.3 Ga的地质体，对探讨华北克拉通古元古代地质演化过程具有十分重要的意义.选择中条山地区横岭关二长花岗岩进行了地球化学、锆石U-Pb年代学和Hf同位素研究.横岭关二长花岗岩LA-ICPMS锆石U-Pb年龄结果为2 308±12 Ma，代表岩体的形成时代.横岭关二长花岗岩高硅、高钾、高铝、富碱，贫钙、低钠和低钛，A/CNK主要集中在1.0~1.1之间，为高钾钙碱性偏铝－过铝质花岗岩系列.岩石的稀土元素含量相对高，轻重稀土元素分异强烈，并具有明显的Eu负异常.高场强元素Nb、Ta、Zr、Hf、U和大离子亲石元素Rb等相对富集，亏损V、Cr、Co、Ni等相容元素，具有I型花岗岩的特征.横岭关二长花岗岩锆石εHf（t）为0.52~6.24，平均值为2.06，单阶段和两阶段模式年龄分别为2 419~2 642 Ma和2 438~2 738 Ma.横岭关二长花岗岩具有同碰撞花岗岩的特征，推测来源于~2.5 Ga古老地壳岩石在挤压碰撞环境下的部分熔融，揭示了华北克拉通在古元古代全球岩浆静寂期并不静寂.Abstract: A large number of ~2.3 Ga geologic bodies have been identified in the North China Craton (NCC) in global magmatic quiescence, which is vital for unveiling the Paleoproterozoic geological evolution on the NCC. This paper presents the whole rock geochemical data, zircon U-Pb ages and Hf isotopes of the Henglingguan monzogranite in Zhongtiao mountains area. LA-ICPMS dating of zircon from the Henglingguan monzogranite yields an age of 2 308±12 Ma. The Henglingguan monzogranite is high in SiO2, K2O, Al2O3 and alkali, and low in CaO, NaO and TiO2, with A/CNK concentrated between 1.0 and 1.1, which belongs to high-K calc-alkaline and metaluminous-peraluminous series. The monzogranite is high in total REE contents, showing strong fractionation of LREE and HREE and obvious negative Eu anomaly. As to the trace elements, the monzogranite shows enrichment in Nb, Ta, Zr, Hf, U and Rb, and depletion in V, Cr, Co and Ni, which is consistent with characteristics of I-type granite. Zircons in the Henglingguan monzogranite have εHf(t) values ranging from 0.52 to 6.24, with an average of 2.06, and Hf model TDM1 age of 2 419-2 642 Ma and TDM2 age of 2 438-2 738 Ma. The Henglingguan monzogranite shows the features of syn-collision granites originated from partial melting of the ~2.5 Ga ancient crust in collision environment, which shows the NCC was not quiet during the Paleoproterozoic global magmatic quiescence.
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图 1 华北克拉通~2.3 Ga地质体分布
底图据Zhao et al.（2005）、Zhai and Santosh（2011）；~2.3 Ga年龄数据见附表1文献.图中简写含义：AL.阿拉善; CD.承德; DF.登封; EH.冀东; ES.胶东; FP.阜平; GY.固阳; HA.怀安; HL.贺兰山; HS.恒山; JN.集宁; LL.吕梁; MY.密云; NH.冀北; QL.千里山; NL.辽北; SJ.吉南; SL.辽南; TH.太华; WD.乌拉山-大青山; WH.五河; WL.辽西; WS.鲁西; WT.五台; XH.宣化; ZT.中条
Fig. 1. The distribution map of ~2.3 Ga geologic bodies in the North China Craton
图 2 华北克拉通中条山地区地质简图(据白瑾等，1997；刘树文等, 2007)
Fig. 2. Geological sketch map of Zhongtiao mountains in the North China Craton (after Bai et al., 1997; Liu et al., 2007)
图 3 横岭关二长花岗岩的野外及显微镜下照片（矿物缩写据沈其韩，2009）
a.二长花岗质片麻岩的野外特征；b.二长花岗质片麻岩的显微镜下特征，单偏光；c.绢云石英片岩的野外特征；d.绢云石英片岩的显微镜下特征，单偏光
Fig. 3. Field and microscopic photographs of the Henglingguan monzogranite (abbreviation of minerals after Shen, 2009)
图 4 横岭关二长花岗岩锆石U⁃Pb年龄谐和图（a）和锆石年龄与εHf(t)关系图（b）
球粒陨石（CHUR）根据Blichert⁃Toft and Albereade（1997）; 亏损地幔（DM）根据Griffin et al.（2000）; 长英质上地壳的计算根据Vervoort et al.（2000）
Fig. 4. U⁃Pb Concordia diagram of zircons from the Henglingguan adamellite (a) and zircon ages vs. εHf(t) (b)
图 5 横岭关二长花岗岩SiO2-K2O（a）和A/CNK-A/NK（b）关系图解
图a据Peccerillo and Taylor（1976）、Middlemost（1985）；图b中A/CNK=Al2O3/(CaO+Na2O+K2O), A/NK=Al2O3/(Na2O+K2O)
Fig. 5. Geochemical diagram of SiO2 vs. K2O (a) and A/CNK vs. A/NK (b) for the Henglingguan monzogranit
图 6 横岭关二长花岗岩球粒陨石标准化稀土元素配分图（a）和原始地幔标准化微量元素蛛网图解（b）（标准化值根据Sun McDonough, 1989）
Fig. 6. Chondrite-normalized REEs (a) and PM-normalized trace elements (b) patterns for the Henglingguan monzogranite (normalization values after Sun McDonough, 1989)
图 7 横岭关二长花岗岩10 000 Ga/Al-TFeO/MgO（a）和SiO2-P2O5（b）判别图
Fig. 7. 10 000 Ga/Al vs. TFeO/MgO (a) and SiO2 vs P2O5 (b) diagram of the Henglingguan monzogranite
图 8 横岭关二长花岗岩Nb-Y（a）和Rb-（Y+Yb）（b）图解（底图据Pearce et al., 1984）
Syn⁃COLG.同碰撞花岗岩; VAG.火山弧花岗岩; WPG.板内花岗岩; ORG.洋脊花岗岩
Fig. 8. Nb vs. Y (a) and Rb vs. (Y+Yb) (b) diagrams of the Henglingguan monzogranite (after Pearce et al., 1984)
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