大兴安岭北部漠河地区早奥陶世A型花岗岩锆石U-Pb年代学、地球化学及Hf同位素研究
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摘要
大兴安岭北部漠河地区黑云母二长花岗岩中锆石自形程度较好,主要为长柱状,具有较为清晰的韵律环带结构,表明锆石岩浆成因。锆石LA-ICP-MS U-Pb年代学研究显示岩石形成时代为早奥陶世(481±5Ma)。岩石地球化学研究显示,岩石属于钙碱性、弱过铝质系列花岗岩,高硅(SiO_2=71.42%～72.57%)、富碱(ALK=8.11%～8.76%)、贫镁(MgO=0.52%～0.54%)。10000Ga/Al值为2.73～2.85,Zr+Nb+Ce+Y含量374×10~(-6)～495×10~(-6),岩浆形成温度801～897℃,判断岩石为A型花岗岩。岩石有中等的负Eu异常(δEu=0.24～0.35),Rb/Sr值为1.18～1.38、Ba/La值为8.7～12.4、Mg~#值为23.3～30.3,及低Ni(1.51×10~(-6)～5.59×10~(-6))、Cr(6.60×10~(-6)～13.4×10~(-6))、V(20.0×10~(-6)～21.6×10~(-6))含量。岩石的ε_(Hf)(t)值为-2.22～5.57,二阶段模式年龄(t_(DM2))变化于1021～1453Ma之间,主要源于中新元古代增生地壳。结合区域构造演化及构造判别,认为岩石形成于额尔古纳地块与西伯利亚板块拼合造山后的伸展背景。
Zircons from the granites in the Mohe region,northeastern Da Hinggan Mountains are euhedral in shape and display oscillatory zoning in CL image,implying their magmatic origin.LA-ICP-MS zircon U-Pb dating results indicate that these rocks were formed in the Early Ordovician(481 ± 5 Ma).Lithogeochemcial analysis shows that these rocks belong to the calc-alkaline,slightly peraluminous series granitoids,characterized by high SiO_2 contents(71.42% ～72.57%),high alkali contents(8.11% ～8.76%)but low MgO contents(0.52%～0.54%).The 10000 Ga/Al ratios in these rocks vary from 2.73 to 2.85,Zr+Nb+Ce+Y contents 374～495×10~(-6),and the temperature of magma formed is 801～897℃,all these characteristics indicate the rocks belong to aluminous A-type granite.The granites are characterized by the low Sr(150×10~(-6)～205×10~(-6))and low Yb(0.89×10~(-6)～1.07×10~(-6))andδEu values(0.24～0.35).The rocks have Rb/Sr ratios(1.18～1.38),Ba/La rations(8.7～12.4),Mg#rations(23.3～30.3)and low contents Ni(1.51×10~(-6)～5.59×10~(-6)),Cr(6.6×10~(-6)～13.4×10~(-6)),V(20.0×10~(-6)～21.6×10~(-6)).The in situ zircon ε_(Hf)(t)value varies from -2.22 to 5.57 and the two-stage model age(T_(DM2))varies from 1021 to 1453 Ma,suggesting that the primary magma was derived from partial melting of juvenile crustal materials.It can be concluded from regional tectonic evolution and discrimination diagram of tectonic setting that the granites formed in the post-orogenic extension setting due to agglomeration of Siberia block and Erguna Massif.
Zircons from the granites in the Mohe region,northeastern Da Hinggan Mountains are euhedral in shape and display oscillatory zoning in CL image,implying their magmatic origin.LA-ICP-MS zircon U-Pb dating results indicate that these rocks were formed in the Early Ordovician(481 ± 5 Ma).Lithogeochemcial analysis shows that these rocks belong to the calc-alkaline,slightly peraluminous series granitoids,characterized by high SiO_2 contents(71.42% ～72.57%),high alkali contents(8.11% ～8.76%)but low MgO contents(0.52%～0.54%).The 10000 Ga/Al ratios in these rocks vary from 2.73 to 2.85,Zr+Nb+Ce+Y contents 374～495×10~(-6),and the temperature of magma formed is 801～897℃,all these characteristics indicate the rocks belong to aluminous A-type granite.The granites are characterized by the low Sr(150×10~(-6)～205×10~(-6))and low Yb(0.89×10~(-6)～1.07×10~(-6))andδEu values(0.24～0.35).The rocks have Rb/Sr ratios(1.18～1.38),Ba/La rations(8.7～12.4),Mg#rations(23.3～30.3)and low contents Ni(1.51×10~(-6)～5.59×10~(-6)),Cr(6.6×10~(-6)～13.4×10~(-6)),V(20.0×10~(-6)～21.6×10~(-6)).The in situ zircon ε_(Hf)(t)value varies from -2.22 to 5.57 and the two-stage model age(T_(DM2))varies from 1021 to 1453 Ma,suggesting that the primary magma was derived from partial melting of juvenile crustal materials.It can be concluded from regional tectonic evolution and discrimination diagram of tectonic setting that the granites formed in the post-orogenic extension setting due to agglomeration of Siberia block and Erguna Massif.
引文
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