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《Earth Science Frontiers》 2011-02
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Petrogenesis and geodynamic setting of Jiandeng potassic granite at the end of the Neoarchean in Zanhuang Complex,North China Craton.

Yang Chonghui1,Du Lilin1,Ren Liudong1,Song Huixia1,Wan Yusheng1,2,Xie Hangqiang1,2,Liu Zengxiao3 1.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China 2.Beijing SHRIMP Center,Beijing 100037,China 3.Hebei Institute of Geology and Mineral Resources,Langfang 065000,China  
Jiandeng granite in the Zanhuang Complex is located in the northwestern Lincheng County,Hebei Province.The pluton consists mainly of K-feldspar granite and monzo-granite with few quartz diorite enclaves.SHRIMP dating of zircon from the granite yielded an age of(2490±13)Ma.The rocks have high contents of SiO2(74.3%—75.4%),K2O(5.76%—9.37%) and alkali with K2O+Na2O=6.16%—9.51%,and low contents of CaO(0.14%—0.81%),TiO2(0.04%—0.15%),MgO(0.02%—0.49%) and total FeO(0.26%—1.05%),belonging to shoshonitic series with slightly peraluminous feature.They have lower REE contents((12.07—160.38)×10-6),with relative enrichment of the LREE and variational Eu anomaly(Eu/Eu*=0.46—1.97).The rocks are rich in large-ion lithophile elements(LILE) Rb,Ba and Th,and poor in Sr,Zr,Nb,Y and Yb,with high Rb/Sr and Rb/Ba ratios.They have positive ε Nd(t) value ranging from 2.85 to 3.66,with TDM2 ages between 2.55 and 2.64 Ga.SHRIMP dating of zircon from the quartz diorite enclave yielded an age of(2506±13)Ma.The quartz diorite is high in Al2O3(17.16%),Na2O(4.47%),CaO(4.34%) and TFeO(5.26%),and shows higher total REE content of 212.82×10-6,with a small Eu anomaly(Eu/Eu*=0.83).This rock is rich in Rb,Sr and Zr,and has an εNd(t) value of 3.05 and a TDM2 age of 2.63 Ga.The geochemical data show that the Jiandeng granite is similar to the S-type granite formed by anatexis of the juvenile crust in a tectonic transition setting from compression to extension,and the quartz diorite may represent a residue of the source rock.The formation of Jiandeng granite marks a tectono-magmatic event resulting in stabilization of the North China Craton at the end of the Neoarchean.
【Fund】: 中国地质调查局地质调查项目(1212010611802 1212010711815);; 中国地质科学院地质研究所基本科研业务费项目(J0907)
【CateGory Index】: P588.121
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