江南造山带东段陈蔡地区新元古代高硅埃达克质花岗闪长岩的发现及其构造启示
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摘要
华南由扬子板块与华夏板块在新元古代拼合而成,其拼合时间与演化模式一直广受争议。江南造山带是其重要的拼合带,带内保留一系列新元古代沉积作用-岩浆活动记录,是研究扬子板块与华夏板块拼贴碰撞时间与演化机制的理想场所。本文针对江南造山带东段陈蔡地区花岗闪长岩,开展了LA-ICP-MS锆石U-Pb年代学、全岩主微量元素及Sr-Nd同位素地球化学研究。代表性样品的~(206)Pb/~(238)U加权平均年龄为838±5Ma和836±4Ma,为花岗闪长岩的原岩结晶年龄。样品K_2O含量为1.30%～2.57%,铝饱和指数(A/CNK)为1.01～1.54,为钙碱性过铝质花岗闪长岩。样品高Si O_2(63.38%～68.97%)、Al_2O_3(15.30%～16.70%)、Na_2O(3.89%～6.24%)、Sr(306×10~(-6)～628×10~(-6))、Sr/Y(26～80)和低Mg O含量(0.64%～1.99%)、K_2O/Na_2O(0.17～0.64)、低Y含量(3.38×10~(-6)～16.10×10~(-6))和Yb含量(0.42×10~(-6)～1.67×10~(-6)),δEu异常不明显,相对富集轻稀土和大离子亲石元素、强烈亏损重稀土和高场强元素、低~(87)Sr/~(86)Sr初始值(0.7015～0.7022)和高ε_(Nd)(t)值(+4.10～+6.13),具有与高硅埃达克岩相似的特征。结合区域构造演化背景,认为陈蔡花岗闪长岩是扬子板块与华夏板块之间的古洋壳向双溪坞陆弧地体俯冲的过程中,俯冲板片熔体被少量地幔楔橄榄岩同化和交代的产物,暗示838～836Ma时江南造山带东段仍处于俯冲消减阶段,扬子与华夏尚未完成最终拼合。综合现有证据,认为扬子与华夏在江南造山带各区段于ca.825～820Ma完成拼合。
The South China Block is commonly considered as the result of the amalgamation of the Yangtze Block to the northwest and Cathaysia Block to the southeast along the Jiangnan Orogen during the Neoproterozoic period.However,the mechanism of final amalgamation between the Yangtze Block and Cathaysia block is still controversial.The Jiangnan orogenic belt is an important assemblage zone,and a series of Neoproterozoic sedimentary sequences-magmatic activity records are preserved in the belt,which is an ideal place for studying the collision time and evolution mechanism of the Yangtze Block and Cathaysia Block.In this study,systematic LA-ICP-MS zircon U-Pb geochronological and geochemical data are presented for granodiorites from the Chencai Group in eastern Jiangnan Orogen,China.LA-ICP-MS zircon U-Pb dating of representative samples yield~(206)Pb/~(238)U weight average ages of 838±5Ma and 836±4Ma respectively,indicating the formation age of the granodiorites.The samples show K_2O contents and A/CNK=molar(Al_2O_3/(Ca O+Na_2O+K_2O))values ranging from 1.30%～2.57%and 1.01～1.54,respectively,which demonstrate that they belong to cale-alkaline,peraluminous series.They have similar characteristics to those of high-SiO_2adakite,such as high Si O_2(63.38%～68.97%),Al_2O_3(15.30%～16.70%),Na_2O(3.89%～6.24%),Sr(306×10~(-6)～628×10~(-6)),and Sr/Y(26～80),but low MgO(0.64%～1.99%),K_2O/Na_2O,Y(3.38×10~(-6)～16.10×10~(-6))and Yb(0.42×10~(-6)～1.67×10~(-6)).They are relatively enriched in light rare earth elements(LREEs)and large ion lithophile elements(LILEs),and strongly depleted in heavy rare earth elements(HREEs)and high field strength elements(HFSEs),with a slightlyδEu anomaly and low values of(~(87)Sr/~(86)Sr)_(i )andε_(Nd)(t)of 0.7015～0.7022 and 4.10～6.13,respectively.Along with the geochemistry characteristics and regional tectonic background,it is inferred that the Chencai meta-granodirites is the product of sab melt assimilation and metasomatism of the mantle wedge peridotite during the subduction of the ancient oceanic crust between the Yangtze Block and Cathaysia Block to the Shuangxiwu continental arc,suggesting that the eastern Jiangnan Orogen was still on the stage of subduction in the period from 838Ma to 836Ma,and the Yangtze Block and Cathaysia Block had not completed the final assemblage.In conjunction with previous geochronological and geological evidence,it is proposed that the final amalgamation of the Yangtze Block and Cathaysia Block in the Jiangnan Orogen,which is composed of the eastern,central and western parts,most likely occurred at ca.825～820Ma.
The South China Block is commonly considered as the result of the amalgamation of the Yangtze Block to the northwest and Cathaysia Block to the southeast along the Jiangnan Orogen during the Neoproterozoic period.However,the mechanism of final amalgamation between the Yangtze Block and Cathaysia block is still controversial.The Jiangnan orogenic belt is an important assemblage zone,and a series of Neoproterozoic sedimentary sequences-magmatic activity records are preserved in the belt,which is an ideal place for studying the collision time and evolution mechanism of the Yangtze Block and Cathaysia Block.In this study,systematic LA-ICP-MS zircon U-Pb geochronological and geochemical data are presented for granodiorites from the Chencai Group in eastern Jiangnan Orogen,China.LA-ICP-MS zircon U-Pb dating of representative samples yield~(206)Pb/~(238)U weight average ages of 838±5Ma and 836±4Ma respectively,indicating the formation age of the granodiorites.The samples show K_2O contents and A/CNK=molar(Al_2O_3/(Ca O+Na_2O+K_2O))values ranging from 1.30%～2.57%and 1.01～1.54,respectively,which demonstrate that they belong to cale-alkaline,peraluminous series.They have similar characteristics to those of high-SiO_2adakite,such as high Si O_2(63.38%～68.97%),Al_2O_3(15.30%～16.70%),Na_2O(3.89%～6.24%),Sr(306×10~(-6)～628×10~(-6)),and Sr/Y(26～80),but low MgO(0.64%～1.99%),K_2O/Na_2O,Y(3.38×10~(-6)～16.10×10~(-6))and Yb(0.42×10~(-6)～1.67×10~(-6)).They are relatively enriched in light rare earth elements(LREEs)and large ion lithophile elements(LILEs),and strongly depleted in heavy rare earth elements(HREEs)and high field strength elements(HFSEs),with a slightlyδEu anomaly and low values of(~(87)Sr/~(86)Sr)_(i )andε_(Nd)(t)of 0.7015～0.7022 and 4.10～6.13,respectively.Along with the geochemistry characteristics and regional tectonic background,it is inferred that the Chencai meta-granodirites is the product of sab melt assimilation and metasomatism of the mantle wedge peridotite during the subduction of the ancient oceanic crust between the Yangtze Block and Cathaysia Block to the Shuangxiwu continental arc,suggesting that the eastern Jiangnan Orogen was still on the stage of subduction in the period from 838Ma to 836Ma,and the Yangtze Block and Cathaysia Block had not completed the final assemblage.In conjunction with previous geochronological and geological evidence,it is proposed that the final amalgamation of the Yangtze Block and Cathaysia Block in the Jiangnan Orogen,which is composed of the eastern,central and western parts,most likely occurred at ca.825～820Ma.
引文
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