西大别山早白垩世谭冲和陈冲花岗岩体U-Pb年龄、地球化学和Sr-Nd-Hf同位素特征:对岩石成因和下地壳拆沉时限的约束
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摘要
谭冲和陈冲岩体出露于西大别造山带新县岩基北缘,主要岩性分别为二长花岗岩和花岗斑岩。为理解其岩石成因和构造属性,对两个岩体开展了激光等离子质谱(LA-ICP-MS)锆石U-Pb测年、元素地球化学和Sr-Nd-Hf同位素研究。结果表明,谭冲和陈冲岩体锆石U-Pb年龄分别为133.5±1.1Ma(MSDW=0.63)和132.9±1.1Ma(MSDW=1.30),暗示其形成于早白垩世。岩石均具有较高的SiO_2(69.40%～77.82%)、Al_2O_3(11.72%～15.26%)和总碱(Na_2O+K_2O=6.40%～8.70%)含量,K_2O/Na_2O比值大于1,过铝质(A/CNK=1.14～1.66,一个样品值0.97除外)等特点,总体归为高钾钙碱性系列。岩石富集轻稀土((La/Yb)_N=22.98～28.64),负Eu异常不明显,亏损Ba、Nb、Ta、P、Ti和Y元素。岩石锶同位素初始比值I_(Sr)为0.707220～0.707557,钕同位素ε_(Nd)(t)值为-17.7～-18.1,两阶段Nd模式年龄T_(DM2)=2.36～2.40Ga。锆石ε_(Hf)(t)值集中于-21.4～-25.8,两阶段Hf模式年龄T_(DM2)=2.24～2.48Ga。详细的矿物组成、岩石地球化学和Sr-Nd-Hf同位素分析揭示,两个岩体成因类型均为分异的I型花岗岩,起源于残留相含有石榴子石的部分熔融岩浆。岩浆房形成压力和深度较大,可能是在加厚下地壳环境扬子陆块北缘古老陆壳物质重熔的产物。结合区域同期岩浆岩对比研究认为,西大别地区与东大别地区加厚下地壳拆沉时限基本一致,发生在133Ma左右。
The Tanchong and Chenchong granitic stocks are situated in the northern margin of Xinxian batholith within the western Dabie orogen. They consist of monzogranite and granite porphyry, respectively. Elemental, whole-rock Sr-Nd and zircon U-Pb-Hf isotopic analyses have been carried out in this study, in order to understand their petrogenesis and tectonic significance. LA-ICP-MS zircon dating yields U-Pb ages of 133.5±1.1 Ma and 132.9±1.1 Ma for the Tanchong and Chenchong granites, respectively, indicating they formed in the early Cretaceous. These granites are characterized by high SiO_2 of 69.40% to 77.82%, Al_2O_3 of 11.72% to 15.26%, a total alkali of Na_2O+K_2O=6.40% to 8.70% with K_2O/Na_2O>1 and A/CNK=1.14 to 1.66, and belong to the high-K calc-alkaline series. They are enriched in LREE with(La/Yb)_N=22.98 to 28.64 and unapparent Eu anomaly, and depleted in Ba, Nb, Ta, P, Ti and Y. They have moderate I_(Sr) values(0.707220 to 0.707557) and negative ε_(Nd)(t) values(-17.7 to-18.1), with two-stage Nd model ages of 2.36 to 2.40 Ga. Zircon ε_(Hf)(t) values are negative(-21.4 to-25.8) with an calculated two-stage Hf model ages of 2.24 to 2.48 Ga. Their petrographic and geochemical data suggest that the Tanchong and Chenchong granites are fractionated I-type granites, which are derived from partial melting of ancient crust of the Yangtze Block. Their equilibrated residues are probably garnet-bearing. We infer that the magmas of Tanchong and Chenchong stocks were formed in a thickened continental setting. Combining regional synchronous magmatic rocks, we propose that tectonic collapse of the western Dabie orogen probably started at about 133 Ma, which is consistent with the eastern Dabie orogen.
The Tanchong and Chenchong granitic stocks are situated in the northern margin of Xinxian batholith within the western Dabie orogen. They consist of monzogranite and granite porphyry, respectively. Elemental, whole-rock Sr-Nd and zircon U-Pb-Hf isotopic analyses have been carried out in this study, in order to understand their petrogenesis and tectonic significance. LA-ICP-MS zircon dating yields U-Pb ages of 133.5±1.1 Ma and 132.9±1.1 Ma for the Tanchong and Chenchong granites, respectively, indicating they formed in the early Cretaceous. These granites are characterized by high SiO_2 of 69.40% to 77.82%, Al_2O_3 of 11.72% to 15.26%, a total alkali of Na_2O+K_2O=6.40% to 8.70% with K_2O/Na_2O>1 and A/CNK=1.14 to 1.66, and belong to the high-K calc-alkaline series. They are enriched in LREE with(La/Yb)_N=22.98 to 28.64 and unapparent Eu anomaly, and depleted in Ba, Nb, Ta, P, Ti and Y. They have moderate I_(Sr) values(0.707220 to 0.707557) and negative ε_(Nd)(t) values(-17.7 to-18.1), with two-stage Nd model ages of 2.36 to 2.40 Ga. Zircon ε_(Hf)(t) values are negative(-21.4 to-25.8) with an calculated two-stage Hf model ages of 2.24 to 2.48 Ga. Their petrographic and geochemical data suggest that the Tanchong and Chenchong granites are fractionated I-type granites, which are derived from partial melting of ancient crust of the Yangtze Block. Their equilibrated residues are probably garnet-bearing. We infer that the magmas of Tanchong and Chenchong stocks were formed in a thickened continental setting. Combining regional synchronous magmatic rocks, we propose that tectonic collapse of the western Dabie orogen probably started at about 133 Ma, which is consistent with the eastern Dabie orogen.
引文
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