首站-论文投稿智能助手
典型文献
Hydrous plumes in the Archean and the origin of continents
文献摘要:
The origin of continents,which is fundamentally important in understanding the evolution of Earth and its habitability,remains a highly debatable issue.The dominant rock types of Archean cra-tons are tonalite-trondhjemite-granodiorite(TTG)plutons.Exten-sive evidence suggests that Archean TTG rocks were formed from a hydrous mafic source[1-3].Subduction has been considered to be the only effective means of transporting a great amount of water to the mantle,leading to partial melting to generate a hydrous mafic crust,which can be regarded as the most possible source of the Archean TTG rocks.Hence,Arndt[2]argued that subduction zones are probably the sole setting in Earth to provide the three main ingredients of the Archean TTG,namely,basalt,water,and heat.In such a model,the collision of the island arcs above the subduc-tion zones forms the continents[2].
文献关键词:
作者姓名:
Zhongqing Wu;Guochun Zhao
作者机构:
Deep Space Exploration Laboratory/School of Earth and Space Sciences,University of Science and Technology of China,Hefei 230026,China;CAS Center for Excellence in Comparative Planetology,University of Science and Technology of China,Hefei 230026,China;National Geophysical Observatory at Mengcheng,University of Science and Technology of China,Mengcheng 253500,China;Department of Earth Sciences,the University of Hong Kong,Hong Kong,China;Department of Geology,State Key Laboratory of Continental Dynamics,Northwest University,Xi'an 710029,China
引用格式:
[1]Zhongqing Wu;Guochun Zhao-.Hydrous plumes in the Archean and the origin of continents)[J].科学通报(英文版),2022(20):2023-2025
A类:
habitability,Arndt,subduc
B类:
Hydrous,plumes,Archean,origin,continents,which,fundamentally,important,understanding,evolution,Earth,its,remains,highly,debatable,issue,dominant,types,cra,are,tonalite,trondhjemite,granodiorite,TTG,plutons,Exten,sive,evidence,suggests,that,rocks,were,formed,from,hydrous,mafic,source,Subduction,has,been,considered,only,effective,means,transporting,great,amount,water,mantle,leading,partial,melting,generate,crust,can,regarded,most,possible,Hence,argued,subduction,zones,probably,sole,setting,provide,three,ingredients,namely,basalt,heat,In,such,model,collision,island,arcs,above,forms
AB值:
0.618777
相似文献
Continuous chemical redistribution following amorphous-to-crystalline structural ordering in a Zr-Cu-Al bulk metallic glass
Xuelian Wu;Si Lan;Xiyang Li;Ming Yang;Zhenduo Wu;Xiaoya Wei;Haiyan He;Muhammad Naeem;Jie Zhou;Zhaoping Lu;Elliot Paul Gilbert;Dong Ma;Xun-Li Wang-Department of Physics,City University of Hong Kong,Hong Kong,China;Herbert Gleiter Institute of Nanoscience,School of Materials Science and Engineering,Nanjing University of Science and Technology,Nanjing 210094,China;Beijing National Laboratory for Condensed Matter Physics,Institute of Physics,Chinese Academy of Sciences,Beijing 100190,China;Quantum Matter Institute,University of British Columbia,Vancouver,British Columbia V6T 1Z4,Canada;Neutron Sciences Platform,Songshan Lake Materials Laboratory,Dongguan 523808,China;Center for Neutron Scattering and Applied Physics,City University of Hong Kong Dongguan Research Institute,Dongguan 523000,China;State Key Laboratory for Advanced Metals and Materials,University of Science and Technology Beijing,Beijing 100083,China;Australian Centre for Neutron Scattering,Australian Nuclear Science and Technology Organisation,Lucas Heights,New South Wales 2234,Australia;City University of Hong Kong Shenzhen Research Institute,Shenzhen 518057,China
The onset of deep recycling of supracrustal materials at the Paleo-Mesoarchean boundary
Xiaolei Wang;Ming Tang;Jeff Moyen;Di Wang;Alfred Kr?ner;Chris Hawkesworth;Xiaoping Xia;Hangqiang Xie;Carl Anhaeusser;Axel Hofmann;Junyong Li;Linsen Li-State Key Laboratory for Mineral Deposits Research,School of Earth Sciences and Engineering,Nanjing University,Nanjing 210023,China;School of Earth and Space Sciences,Peking University,Beijing 100871,China;Laboratoire Magmas et Volcans UMR6524,Université de Lyon,UJM-UCA-CNRS-IRD,Saint Etienne 42023,France;Institut für Geowissenschaften,Universit?t Mainz,Mainz 55099,Germany;Department of Earth Sciences,University of Bristol,Bristol BS8 1RJ,UK;State Key Laboratory of lsotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;SHRIMP Center,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;Economic Geology Research Unit,University of the Witwatersrand,Johannesburg 2050,South Africa;Department of Geology,University of Johannesburg,Johannesburg 2006,South Africa
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。