首站-论文投稿智能助手
典型文献
Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction:Radiogenic Ca and Nd Isotopic Constraints
文献摘要:
The Early Cretaceous aluminous A-type granites in the Lower Yangtze River belt(LYRB)can provide important insights into the Mesozoic magmatism in eastern China,but their origin remains highly controversial.In this study,radiogenic Ca-Nd isotopic analysis was performed for sy-enite porphyry and alkali-feldspar granite porphyry of the Yangshan pluton,a typical aluminous A-type granitic intrusion in the LYRB,to constrain its source and geodynamic setting.The results show that εCa(126 Ma),εNd(126 Ma)and K/Casource of the syenite porphyry range from-0.24 to+0.96,-7.2 to-6.0,and 0.31 to 1.26,respectively.The corresponding values for the alkali-feldspar granite porphyry range from 0.26 to 0.84,-8.0 to-6.1,and 0.79 to 1.08,respectively.Binary mixing modeling indicates that they were originated from the same sources with different proportion,namely,a mixing of 50%to 75%Neoproterozoic crust and 50%to 25%asthenospheric mantle.Together with previous works,we propose that the Early Cretaceous subduction of the ridge between the Pacific and Izanagi plates was responsible for the formation of the aluminous A-type granites in the LYRB.
文献关键词:
作者姓名:
Jianghao Bai;Mingxing Ling;Xiaoyong Yang;Fang Liu;Huangling Gu;Zebin Luo;Xiaoyan Jiang;Zhaofeng Zhang
作者机构:
State Key Laboratoty of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;CAS Center for Excellence in Deep Earth Science,Guangzhou 510640,China;University of Chinese Academy of Sciences,Beijing 100049,China;State Key Laboratory of Nuclear Resources and Environment,East China University of Technology,Nanchang 330013,China;Key Laboratory of Crust-Mantle Materials and Environments,School of Earth and Space Sciences,University of Science and Technology of China,Hefei 230026,China;International Research Center for Planetary Science,College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;School of City and Environment,Hunan University of Technology,Zhuzhou 412007,China;State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550081,China
引用格式:
[1]Jianghao Bai;Mingxing Ling;Xiaoyong Yang;Fang Liu;Huangling Gu;Zebin Luo;Xiaoyan Jiang;Zhaofeng Zhang-.Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction:Radiogenic Ca and Nd Isotopic Constraints)[J].地球科学学刊(英文版),2022(03):581-590
A类:
Yangshan,Radiogenic,aluminous,LYRB,radiogenic,enite,Casource,Izanagi
B类:
Type,Granites,Lower,Yangtze,River,Belt,Formed,by,Ridge,Subduction,Nd,Isotopic,Constraints,Early,Cretaceous,type,granites,belt,can,provide,important,insights,into,Mesozoic,magmatism,eastern,China,but,their,remains,highly,controversial,In,this,study,isotopic,analysis,was,performed,porphyry,alkali,feldspar,pluton,typical,granitic,intrusion,constrain,its,geodynamic,setting,results,show,that,Ma,syenite,range,from,to+0,respectively,corresponding,values,Binary,mixing,modeling,indicates,they,were,originated,same,sources,different,proportion,namely,Neoproterozoic,crust,asthenospheric,mantle,Together,previous,works,propose,subduction,ridge,between,Pacific,plates,responsible,formation
AB值:
0.542651
相似文献
Paleozoic post-collisional magmatism and high-temperature granulite-facies metamorphism coupling with lithospheric delamination of the East Kunlun Orogenic Belt,NW China
Qian Wang;Jiao Zhao;Chuanlin Zhang;Shengyao Yu;Xiantao Ye;Xiaoqiang Liu-College of Earth Science and Engineering,Shandong University of Science and Technology,Qingdao 266590,China;Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;State Key Laboratory of Nuclear Resources and Environment,East China University of Technology,Nanchang 330013,China;College of Oceanography,Hohai University,Nanjing 210098,China;Key Lab of Submarine Geosciences and Prospecting Techniques,MOE,Institute for Advanced Ocean Study,College of Marine Geosciences,Ocean University of China,Qingdao 266100,China
A continental back-arc setting for the Namaqua belt:Evidence from the Kakamas Domain
P.H.Macey;R.J.Thomas;A.F.M.Kisters;J.F.A.Diener;M.Angombe;S.Doggart;C.A.Groenewald;C.W.Lambert;J.A.Miller;H.Minnaar;H.Smith;H.F.G.Moen;E.Muvangua;A.Nguno;G.Shifotoka;J.Indongo;D.Frei;C.Spencer;P.le Roux;R.A.Armstrong;C.Tinguely-Council for Geoscience,P.O.Box 572,Bellville,South Africa;Department of Geology,University of Stellenbosch,South Africa;Department of Geological Sciences,University of Cape Town,South Africa;Geological Survey of Namibia,Windhoek,Namibia;Department of Geology,University of Free State,South Africa;Department of Earth Sciences,University of the Western Cape,South Africa;The Institute of Geoscience Research,Dept.Applied Geology,Curtin University,Perth,Australia;Department of Geological Sciences and Geological Engineering,Queen's University,Kingston,Canada;Geochronology and Tracers Facility,British Geological Survey,Nottingham NG12 5GG,UK;RSES,Australian National,University,Canberra,ACT,Australia
机标中图分类号,由域田数据科技根据网络公开资料自动分析生成,仅供学习研究参考。