首站-论文投稿智能助手
典型文献
Chemical-Abrasion U-Pb zircon geochronology reveals 150 Myr of partial melting events in the Archean crust of the S?o Francisco Craton
文献摘要:
Field observations and CA-LA-ICP-MS U-Pb zircon ages and Hf isotope compositions obtained from mig-matitic orthogneisses and granitoids from the Belo Horizonte Complex,southern S?o Francisco Craton,indicate a major period of partial melting and production of felsic rocks in the Neoarchean.Our observa-tions show that the complex is an important site for studying partial melting processes of Archean crys-talline crust.Much of the complex exposes fine-grained stromatic migmatites that are intruded by multiple leucogranitic veins and sheeted dikes.Both migmatites and leucogranite sheets are crosscut by several phases of granitoid batholiths and small granitic bodies;both of which are closely associated with the host banded gneisses.Chemical abrasion followed by detailed cathodoluminescence imaging revealed a wide variety of zircon textures that are consistent with a long-lived period of partial melting and crustal remobilization.Results of U-Pb and Hf isotopes disclose the complex as part of a much wider crustal segment,encompassing the entire southern part of the S?o Francisco Craton.Compilation of avail-able U-Pb ages suggests that this crustal segment was consolidated sometime between 3000 Ma and 2900 Ma and that it experienced three main episodes of partial melting before stabilization at 2600 Ma.The partial melting episodes took place between 2750 Ma and 2600 Ma as a result of tectonic accretion and peeling off the lithospheric mantle and lower crust.This process is likely responsible for the emplacement of voluminous potassic granitoids across the entire S?o Francisco Craton.We believe that the partial melting of Meso-Archean crystalline crust and production of potassic granitoids are linked to a fundamental shift in the tectonics of the craton,which was also responsible for the widespread intrusion of large syenitic bodies in the northern part of the craton,and the construction of layered mafic-ultra-mafic intrusions to the south of the BHC.
文献关键词:
作者姓名:
Lorena Martins;Cristiano Lana;Ariela Mazoz;Tiago Novo
作者机构:
Applied Isotope Research Group,Departamento de Geologia,Escola de Minas,Universidade Federal de Ouro Preto,Morro do Cruzeiro,Ouro Preto,MG,35400-000,Brazil;Universidade Federal de Minas Gerais,Programa de Pós-Gradua??o em Geologia,IGC-CPMTC,Campus Pampulha,Av.Ant?nio Carlos 6627,Belo Horizonte,MG,31270-901,Brazil
引用格式:
[1]Lorena Martins;Cristiano Lana;Ariela Mazoz;Tiago Novo-.Chemical-Abrasion U-Pb zircon geochronology reveals 150 Myr of partial melting events in the Archean crust of the S?o Francisco Craton)[J].地学前缘(英文版),2022(05):169-189
A类:
Abrasion,mig,matitic,Belo,Horizonte,stromatic,migmatites,leucogranitic,sheeted,leucogranite,crosscut,batholiths,syenitic
B类:
Chemical,Pb,zircon,geochronology,reveals,Myr,partial,melting,events,Archean,Francisco,Craton,Field,observations,CA,LA,ICP,ages,Hf,compositions,obtained,from,orthogneisses,granitoids,Complex,southern,indicate,major,period,production,felsic,rocks,Neoarchean,Our,show,that,complex,important,site,studying,processes,Much,exposes,fine,grained,are,intruded,by,multiple,veins,dikes,Both,sheets,several,phases,small,bodies,both,which,closely,associated,host,banded,abrasion,followed,detailed,cathodoluminescence,imaging,revealed,variety,textures,consistent,long,lived,crustal,remobilization,Results,isotopes,disclose,much,wider,segment,encompassing,entire,Compilation,avail,able,suggests,this,was,consolidated,sometime,between,Ma,experienced,three,main,episodes,before,stabilization,took,result,accretion,peeling,off,lithospheric,mantle,lower,This,likely,responsible,emplacement,voluminous,potassic,across,We,believe,Meso,crystalline,linked,fundamental,shift,tectonics,craton,also,widespread,large,northern,construction,layered,mafic,ultra,intrusions,BHC
AB值:
0.490273
相似文献
Genesis of High Ba-Sr Yashan Intrusion from the Jiaodong Peninsula,Eastern China:Implications for the Destruction of the North China Craton
Guozhi Xie;Lipeng Zhang;Jie Li;Zhongyi Bao;Kun Wang;Qian Chen;Li Wang;Jingwei Wang-Center of Deep Sea Research,Institute of Oceanology,Center for Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071,China;School of Marine Sciences,University of Chinese Academy of Sciences,Beijing 100049,China;Laboratory for Marine Mineral Resources,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266237,China;School of Resources,Hebei GEO University,Shijiazhuang 050031,China;Shandong Provincial No.6 Exploration Institute of Geology and Mineral Resources,Weihai 264209,China;Rizhao Natural Resources and Planning Bureau,Rizhao 276800,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。