首站-论文投稿智能助手
典型文献
Pure forsterite in Nyiragongo lavas:evidence for subsolidus oxidation of volcanic rocks
文献摘要:
Some volcanic rocks from Nyiragongo volcano in the Democratic Republic of Congo contain highly oxi-dized olivine crystals.These olivines crystals are made of two phases,dark olivine on backscattered electron images of pure forsterite composition and grey Mg-poor areas made of olivine and iron-rich oxides.Calculation of the initial composition confirms that they are primary olivine with late separation of two different olivine compositions.Pure forsterite is enriched in SiO2 but contains lower amounts of CaO than Fe-rich areas,in agreement with expected partitioning of these elements related to the composition of the olivine.Iron-rich oxides formed around or inside the olivine crystals during the separation process and confirm a highly oxidized environment during their evolution.We propose that this separation occurred during subsolidus recrystallization under high fO2 conditions of the olivine crystals after cooling of the volcanic rocks.It provides evidences for circulation of iron-rich fluids or gas inducing deuteritic processes occurring in the large vol-canic cone of the Nyiragongo,in relation with the presence of a shallow magma chamber connected to a large and permanent lava lake.
文献关键词:
作者姓名:
Innocent Badriyo Agama;Gilles Chazot;Pierre Kamgang
作者机构:
Département Des Sciences de la Terre,Faculté Des Sciences,Université de Yaoundé I,B.P.812,Yaoundé,Cameroon;Observatoire Volcanologique de Goma,B.P.484,Goma,Nord-Kivu,Democratic Republic of the Congo;Laboratoire Géosciences Océan,Institut Universitaire Européen de la Mer,Université de Brest (UBO),UMR 6538,Place Copernic,29280 Plouzané,France
引用格式:
[1]Innocent Badriyo Agama;Gilles Chazot;Pierre Kamgang-.Pure forsterite in Nyiragongo lavas:evidence for subsolidus oxidation of volcanic rocks)[J].地球化学学报(英文版),2022(01):12-23
A类:
forsterite,Nyiragongo,olivines,deuteritic,canic
B类:
Pure,lavas,subsolidus,oxidation,volcanic,rocks,Some,from,volcano,Democratic,Republic,Congo,highly,crystals,These,made,two,phases,dark,backscattered,electron,images,pure,grey,Mg,poor,areas,oxides,Calculation,initial,confirms,that,they,primary,separation,different,compositions,enriched,SiO2,but,contains,lower,amounts,CaO,than,agreement,expected,partitioning,these,elements,related,Iron,formed,around,inside,during,oxidized,environment,their,evolution,We,propose,this,occurred,recrystallization,under,fO2,conditions,after,cooling,It,provides,evidences,circulation,fluids,gas,inducing,processes,occurring,large,cone,relation,presence,shallow,magma,chamber,connected,permanent,lake
AB值:
0.492938
相似文献
Deserpentinization and high-pressure (eclogite-facies) metamorphic features in the Eoarchean ultramafic body from Isua,Greenland
Juan Miguel Guotana;Tomoaki Morishita;Ikuya Nishio;Akihiro Tamura;Tomoyuki Mizukami;Kenichiro Tani;Yumiko Harigane;Kristoffer Szilas;D.Graham Pearson-Graduate School of Natural Science & Technology,Kanazawa University,Japan;School of Environmental Science and Management,University of the Philippines Los Ba(n)os,Laguna,Philippines;Lamont-Doherty Earth Observatory,Columbia University,Palisades,NY 10964,USA;Volcanoes and Earth's Interior Research Center,Japan Agency for Marine-Earth Science and Technology,2-15 Natsushima,Kanagawa 237-0061,Japan;National Museum of Nature and Science,4-1-1,Amakubo,Tsukuba-shi,Ibaraki 305-0005,Japan;Institute of Geology and Geoinformation Geological Survey of Japan/AIST,Central 7,1-1-1 Higashi,Tsukuba,Ibaraki 305-8567,Japan;Department of Geosciences and Natural Resource Management,University of Copenhagen,?ster Voldgade 10,1350 Copenhagen,Denmark;Department of Earth & Atmospheric Sciences,University of Alberta,Edmonton,AB,Canada
The generation and evolution of the Archean continental crust:The granitoid story in southeastern Brazil
Rodrigo S.Marimon;Chris J.Hawkesworth;Elton L.Dantas;Rudolph A.J.Trouw;Wilson Teixeira;Peter C.Hackspacher;Allen Fetter;Ciro A.ávila;Silvia Volante;Atlas V.Corrêa Neto;Everton M.Bongiolo;Rodrigo Vinagre;Maurício Simon-Depto.de Geologia,IGEO,Universidade Federal do Rio de Janeiro,UFRJ,Rio de Janeiro,RJ,Brazil;School of Earth Sciences,University of Bristol,Bristol,United Kingdom;Instituto de Geociências,Universidade de Brasília,UnB,Brasília,DF,Brazil;Instituto de Geociências,Universidade de S?o Paulo,USP,S?o Paulo,SP,Brazil;Instituto de Geociências e Ciências Exatas,Universidade Estadual Paulista,Rio Claro,SP,Brazil;Institute of Geology,Mineralogy and Geophysics,Ruhr-Universit?t Bochum,Universit?tsstra?e 150,44801 Bochum,Germany;ISOTOPIA Lab,School of Earth,Atmosphere and Environment,Monash University,Wellington Rd,Clayton,VIC 3800,Australia;Programa de Pós-Gradua??o em Geociências,IG,Universidade Federal do Rio Grande do Sul,UFRGS,Porto Alegre,RS,Brazil
Mass Transfer during Hematitization and Implications for Uranium Mineralization in the Zoujiashan Deposit, Xiangshan Volcanic Basin
Teng Deng;Guoxiang Chi;Xiongjie Zhang;Zenghua Li;Deru Xu;Shengmiao Li;Pengfei Du;Pei Shang;Shaohao Zou;Wanpeng Zhou;Ke Xu;Hai Yan;Ma Wen;Zhengpeng Ding-State Key Laboratory of Nuclear Resources and Environment,East China University of Technology,Nanchang 330013,China;Key Laboratory of Uranium Geology,China Geological Survey,Tianjin 300170,China;School of Earth Sciences,East China University of Technology,Nanchang 330013,China;Department of Geology,University of Regina,Regina S4S 0A2,Canada;Engineering Research Center of Nuclear Technology Application,Ministry of Education,East China University of Technology,Nanchang 330013,China;Jiangxi Engineering Laboratory on Radioactive Geoscience and Big Data Technology,East China University of Technology,Nanchang,330013,China;Geological Bureau of Hunan Province,Changsha 410014,China;Geologic Party No.208,China National Nuclear Corporation,Baotou 410014,China
Under the surface:Pressure-induced planetary-scale waves,volcanic lightning,and gaseous clouds caused by the submarine eruption of Hunga Tonga-Hunga Ha'apai volcano
David A.Yuen;Melissa A.Scruggs;Frank J.Spera;Yingcai Zheng;Hao Hu;Stephen R.McNutt;Glenn Thompson;Kyle Mandli;Barry R.Keller;Songqiao Shawn Wei;Zhigang Peng;Zili Zhou;Francesco Mulargia;Yuichiro Tanioka-Columbia University,Dept.of Applied Physics and Applied Mathematics,New York,NY,10027,USA;Ocean University of China,School of Computer Science and Marine Geosciences,Qingdao,266100,China;University of California,Santa Barbara,Dept.of Earth Science,1006 Webb Hall,University of California,Santa Barbara,CA,93106,USA;University of Houston,Dept of Earth and Atmospheric Sciences,Science&Research Bldg.1,3507 Cullen Boulevard,#312,Houston,TX,77004,USA;University of South Florida,School of Geosciences,Tampa,FL,USA;Mission Beach,CA,USA;Michigan State University,Dept.of Earth and Environmental Sciences,288 Farm Ln Bldg,Room 207,East Lansing MI,48824,USA;Georgia Institute of Technology,School of Atmospheric and Earth Sciences,North Avenue,Atlanta,GA,30332,USA;University of Southern California,Sonny Astani Dept.of Civil&Environmental Engineering Kaprielian Hall,Los Angeles,CA,90089-2531,USA;University of Bologna,Dept.of Geological Sciences,Via Zamboni,33,40126,Bologna,Italy;Hokkaido University,Division of Earth System Science,N10W5,Sapporo,Hokkaido,060-0810,Japan
Mapping the spatial distribution of fossil geothermal manifestations and assessment of geothermal potential of the Tangyin rift,Southeast of Taihang Mountain in China
MAHWA Joshua;LI Da-jiang;PING Jian-hua;LENG Wei;TANG Jia-bo;SHAO Dong-yun-School of Water Conservancy and Engineering,Zhengzhou University,Zhengzhou 450001,China;Department of Geology,College of Earth Science,University of Dodoma,Box 11090,Dodoma,Tanzania;Power China Henan Engineering CO.,LTD,No.30 Changchun Road,High and New Technology Industries Development Zone,Zhengzhou 450001,China;Geothermal and Ecological Geology Research Centre,Zhengzhou University,Zhengzhou 450001,China;College of Ecology and Environment,Zhengzhou University,Zhengzhou 450001,China;Power China Geothermal Development CO.,LTD,No.30 Changchun Road,High and New Technology Industries Development Zone,Zhengzhou 450001,China
Surface microstructures of lunar soil returned by Chang'e-5 mission reveal an intermediate stage in space weathering process
Jian-Gang Guo;Tianping Ying;Hanbin Gao;Xu Chen;Yanpeng Song;Ting Lin;Qinghua Zhang;Qiang Zheng;Chunlai Li;Yigang Xu;Xiaolong Chen-Beijing National Laboratory for Condensed Matter Physics,Institute of Physics,Chinese Academy of Sciences(CAS),Beijing 100190,China;Songshan Lake Materials Laboratory,Dongguan 523808,China;CAS Key Laboratory of Standardization and Measurement for Nanotechnology,CAS Center for Excellence in Nanoscience,National Centre for Nanoscience and Technology,Beijing 100190,China;University of Chinese Academy of Sciences,Beijing 100049,China;Key Laboratory of Lunar and Deep Space Exploration,National Astronomical Observatories,Chinese Academy of Sciences,Beijing 100012,China;State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China
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。