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Sedimentary and structural characteristics of the Triassic Nanpanjiang Basin (Southwest China). New insights on the regional tectonic evolution

Author: Wenjing XiaYan Chen, professeur).Quanren YanMichel FaureUniversité d'Orléans.All authors
Publisher: 2018.
Dissertation: Thèse de doctorat : Sciences de la Terre : Orléans : 2018.
Thèse de doctorat : Sciences de la Terre : University of Chinese academy of sciences : 2018.
Edition/Format:   Computer file : Document : Thesis/dissertation : English
Summary:
En tant qu'un des plus grands bassins sédimentaires du bloc de Chine du Sud, le bassin de Nanpanjiang a attiré une grande attention de la communauté géologique depuis de longtemps. Après plusieurs années de recherche, il reste encore de grand débats sur i) la provenance du bassin, ii) l'âge du changement de régime extension à compression, iii) le type de bassin et son contexte géodynamique. Dans cette
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Genre/Form: Thèses et écrits académiques
Material Type: Document, Thesis/dissertation, Internet resource
Document Type: Internet Resource, Computer File
All Authors / Contributors: Wenjing Xia; Yan Chen, professeur).; Quanren Yan; Michel Faure; Université d'Orléans.; University of Chinese academy of sciences.; École doctorale Énergie, Matériaux, Sciences de la Terre et de l'Univers (Centre-Val de Loire).; Institut des sciences de la terre d'Orléans (2010-).; School of Earth Sciences and Engineering, Nanjing University.
OCLC Number: 1105202050
Notes: Thèse soutenue en co-tutelle.
Titre provenant de l'écran-titre.
Description: 1 online resource
Responsibility: Wenjing Xia ; sous la direction de Yan Chen et de Quanren Yan et de Michel Faure.

Abstract:

En tant qu'un des plus grands bassins sédimentaires du bloc de Chine du Sud, le bassin de Nanpanjiang a attiré une grande attention de la communauté géologique depuis de longtemps. Après plusieurs années de recherche, il reste encore de grand débats sur i) la provenance du bassin, ii) l'âge du changement de régime extension à compression, iii) le type de bassin et son contexte géodynamique. Dans cette thèse, nous avons conduit une étude pluri-disciplinaire incluant l'analyse des faciès sédimentaires et leur distribution géographique, paléocourants, spectres des minéraux lourds et leur geochimie, la géochronologie U-Pb sur zircon et baddeléyite, et le magnétisme des roches pour reconstrurier l'evolution de ce bassin. Les résultats indiquent un trois-étapes évolution. i) durant la période du Permien supérieur au début du Trias, la diabase mise en place 269Ma annonce l'ouverture du bassin, l'environnement sédimentaire est devenu plus profond. ii) durant la période du stade tardif du Trias inférieur (~ 245 Ma) au Trias moyen, à cause des influences de l'orogène Xuefengshan et de l'orogène d'Indochine situées à l'est et au sud du bassin, le bassin a évolué en bassin d'avant-pays. La diabase arrête sa mise en place durant cette période. Les analyses de détritus et de paléo-courants indiquent que durant cette période, les provenances de la partie est et de la partie sud du bassin étaient respectivement l'orogène Xuefengshan et l'orogène Indochinois. iii) la fin du Tirassique, la profondeur de l'environnement sédimentaire a fortement diminué, indiquant que le bassin a commencé à se rétrécir sous l'effet de la compression de l'orogène Xuefengshan et de l'orogène d'Indochine.

Ranks as the largest sedimentary basin in the South China during the Triassic, The Nanpanjiang basin attracts a large attention of the geology community for a long time. After many years study, there still exist several debates on i) the provenance of the sedimentary detritus, ii) the time of the change of the tectonic regime from extension to compression, iii) the type of the basin and its geodynamic background. In this thesis, a multidisciplinary study including analysis of sedimentary facies, paleo-current, frame work detritus mode, heavy mineral combinations and their geochemistry feature, rock magnetism and Zircon-baddeleyite isotopic dating on diabase was conducted to rebuild the evolution of the basin.The results show a three-stage evolution, i) during the Late Permian to the Early Triassic, the 269Ma diabase intruding into the basin announces the opening of the basin, the sedimentary environment became deeper. ii) During the late stage of the Early Triassic (~245 Ma) to the Middle Triassic, owing to the influences of the Xuefengshan orogen and the Indochina orogen which are located to the east and south of the basin, the basin evolved into a foreland basin. The diabase ceased emplacement in this period. The detritus and paleo-current analysis indicate that during this stage, the provenances of the East part and the South part of the basin were Xuefengshan Orogen and Indochina Orogen respectively. iii) During the Late Tirassic, the depth of the sedimentary environment decrease drasticly, indicating that the basin began to shrink owing to the compression of the Xuefengshan Orogen and the Indochina Orogen.

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<http:\/\/www.worldcat.org\/oclc\/1105202050<\/a>> # Sedimentary and structural characteristics of the Triassic Nanpanjiang Basin (Southwest China). New insights on the regional tectonic evolution<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nbgn:ComputerFile<\/a>, schema:CreativeWork<\/a>, schema:MediaObject<\/a>, bgn:Thesis<\/a> ;\u00A0\u00A0\u00A0\nbgn:inSupportOf<\/a> \"Th\u00E8se de doctorat : Sciences de la Terre : Orl\u00E9ans : 2018.<\/span>\" ;\u00A0\u00A0\u00A0\nbgn:inSupportOf<\/a> \"Th\u00E8se de doctorat : Sciences de la Terre : University of Chinese academy of sciences : 2018.<\/span>\" ;\u00A0\u00A0\u00A0\nlibrary:oclcnum<\/a> \"1105202050<\/span>\" ;\u00A0\u00A0\u00A0\nlibrary:placeOfPublication<\/a> <http:\/\/id.loc.gov\/vocabulary\/countries\/fr<\/a>> ;\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Topic\/sedimentologie_chine_sud_ouest<\/a>> ; # S\u00E9dimentologie--Chine (sud-ouest)<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/dewey.info\/class\/551.82\/<\/a>> ;\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/trias<\/a>> ; # Trias<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Topic\/orogenese_chine_sud_ouest<\/a>> ; # Orogen\u00E8se--Chine (sud-ouest)<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Place\/nanpanjiang_basin_china<\/a>> ; # Nanpanjiang Basin (China)<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/orogenese_indosinienne<\/a>> ; # Orogen\u00E8se Indosinienne<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/bloc_de_chine_du_sud<\/a>> ; # Bloc de Chine du Sud<\/span>\n\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/bassin_de_nanpanjiang<\/a>> ; # Bassin de Nanpanjiang<\/span>\n\u00A0\u00A0\u00A0\nschema:author<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/xia_wenjing_1989<\/a>> ; # Wenjing Xia<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/school_of_earth_sciences_and_engineering_nanjing_university<\/a>> ; # School of Earth Sciences and Engineering, Nanjing University.<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/chen_yan_19_professeur<\/a>> ; # professeur). Yan Chen<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/yan_quanren<\/a>> ; # Quanren Yan<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/institut_des_sciences_de_la_terre_d_orleans_2010<\/a>> ; # Institut des sciences de la terre d\'Orl\u00E9ans (2010-).<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/universite_d_orleans<\/a>> ; # Universit\u00E9 d\'Orl\u00E9ans.<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/faure_michel<\/a>> ; # Michel Faure<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/ecole_doctorale_energie_materiaux_sciences_de_la_terre_et_de_l_univers_centre_val_de_loire<\/a>> ; # \u00C9cole doctorale \u00C9nergie, Mat\u00E9riaux, Sciences de la Terre et de l\'Univers (Centre-Val de Loire).<\/span>\n\u00A0\u00A0\u00A0\nschema:contributor<\/a> <http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/university_of_chinese_academy_of_sciences<\/a>> ; # University of Chinese academy of sciences.<\/span>\n\u00A0\u00A0\u00A0\nschema:datePublished<\/a> \"2018<\/span>\" ;\u00A0\u00A0\u00A0\nschema:description<\/a> \"Ranks as the largest sedimentary basin in the South China during the Triassic, The Nanpanjiang basin attracts a large attention of the geology community for a long time. After many years study, there still exist several debates on i) the provenance of the sedimentary detritus, ii) the time of the change of the tectonic regime from extension to compression, iii) the type of the basin and its geodynamic background. In this thesis, a multidisciplinary study including analysis of sedimentary facies, paleo-current, frame work detritus mode, heavy mineral combinations and their geochemistry feature, rock magnetism and Zircon-baddeleyite isotopic dating on diabase was conducted to rebuild the evolution of the basin.The results show a three-stage evolution, i) during the Late Permian to the Early Triassic, the 269Ma diabase intruding into the basin announces the opening of the basin, the sedimentary environment became deeper. ii) During the late stage of the Early Triassic (~245 Ma) to the Middle Triassic, owing to the influences of the Xuefengshan orogen and the Indochina orogen which are located to the east and south of the basin, the basin evolved into a foreland basin. The diabase ceased emplacement in this period. The detritus and paleo-current analysis indicate that during this stage, the provenances of the East part and the South part of the basin were Xuefengshan Orogen and Indochina Orogen respectively. iii) During the Late Tirassic, the depth of the sedimentary environment decrease drasticly, indicating that the basin began to shrink owing to the compression of the Xuefengshan Orogen and the Indochina Orogen.<\/span>\" ;\u00A0\u00A0\u00A0\nschema:description<\/a> \"En tant qu\'un des plus grands bassins s\u00E9dimentaires du bloc de Chine du Sud, le bassin de Nanpanjiang a attir\u00E9 une grande attention de la communaut\u00E9 g\u00E9ologique depuis de longtemps. Apr\u00E8s plusieurs ann\u00E9es de recherche, il reste encore de grand d\u00E9bats sur i) la provenance du bassin, ii) l\'\u00E2ge du changement de r\u00E9gime extension \u00E0 compression, iii) le type de bassin et son contexte g\u00E9odynamique. Dans cette th\u00E8se, nous avons conduit une \u00E9tude pluri-disciplinaire incluant l\'analyse des faci\u00E8s s\u00E9dimentaires et leur distribution g\u00E9ographique, pal\u00E9ocourants, spectres des min\u00E9raux lourds et leur geochimie, la g\u00E9ochronologie U-Pb sur zircon et baddel\u00E9yite, et le magn\u00E9tisme des roches pour reconstrurier l\'evolution de ce bassin. Les r\u00E9sultats indiquent un trois-\u00E9tapes \u00E9volution. i) durant la p\u00E9riode du Permien sup\u00E9rieur au d\u00E9but du Trias, la diabase mise en place 269Ma annonce l\'ouverture du bassin, l\'environnement s\u00E9dimentaire est devenu plus profond. ii) durant la p\u00E9riode du stade tardif du Trias inf\u00E9rieur (~ 245 Ma) au Trias moyen, \u00E0 cause des influences de l\'orog\u00E8ne Xuefengshan et de l\'orog\u00E8ne d\'Indochine situ\u00E9es \u00E0 l\'est et au sud du bassin, le bassin a \u00E9volu\u00E9 en bassin d\'avant-pays. La diabase arr\u00EAte sa mise en place durant cette p\u00E9riode. Les analyses de d\u00E9tritus et de pal\u00E9o-courants indiquent que durant cette p\u00E9riode, les provenances de la partie est et de la partie sud du bassin \u00E9taient respectivement l\'orog\u00E8ne Xuefengshan et l\'orog\u00E8ne Indochinois. iii) la fin du Tirassique, la profondeur de l\'environnement s\u00E9dimentaire a fortement diminu\u00E9, indiquant que le bassin a commenc\u00E9 \u00E0 se r\u00E9tr\u00E9cir sous l\'effet de la compression de l\'orog\u00E8ne Xuefengshan et de l\'orog\u00E8ne d\'Indochine.<\/span>\" ;\u00A0\u00A0\u00A0\nschema:exampleOfWork<\/a> <http:\/\/worldcat.org\/entity\/work\/id\/9348185321<\/a>> ;\u00A0\u00A0\u00A0\nschema:genre<\/a> \"Th\u00E8ses et \u00E9crits acad\u00E9miques<\/span>\" ;\u00A0\u00A0\u00A0\nschema:inLanguage<\/a> \"en<\/span>\" ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Sedimentary and structural characteristics of the Triassic Nanpanjiang Basin (Southwest China). 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<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/institut_des_sciences_de_la_terre_d_orleans_2010<\/a>> # Institut des sciences de la terre d\'Orl\u00E9ans (2010-).<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Organization<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Institut des sciences de la terre d\'Orl\u00E9ans (2010-).<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Organization\/school_of_earth_sciences_and_engineering_nanjing_university<\/a>> # School of Earth Sciences and Engineering, Nanjing University.<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Organization<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"School of Earth Sciences and Engineering, Nanjing University.<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
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<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/faure_michel<\/a>> # Michel Faure<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Person<\/a> ;\u00A0\u00A0\u00A0\nschema:familyName<\/a> \"Faure<\/span>\" ;\u00A0\u00A0\u00A0\nschema:givenName<\/a> \"Michel<\/span>\" ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Michel Faure<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/xia_wenjing_1989<\/a>> # Wenjing Xia<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Person<\/a> ;\u00A0\u00A0\u00A0\nschema:birthDate<\/a> \"1989<\/span>\" ;\u00A0\u00A0\u00A0\nschema:deathDate<\/a> \"\" ;\u00A0\u00A0\u00A0\nschema:familyName<\/a> \"Xia<\/span>\" ;\u00A0\u00A0\u00A0\nschema:givenName<\/a> \"Wenjing<\/span>\" ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Wenjing Xia<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Person\/yan_quanren<\/a>> # Quanren Yan<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Person<\/a> ;\u00A0\u00A0\u00A0\nschema:familyName<\/a> \"Yan<\/span>\" ;\u00A0\u00A0\u00A0\nschema:givenName<\/a> \"Quanren<\/span>\" ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Quanren Yan<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Place\/nanpanjiang_basin_china<\/a>> # Nanpanjiang Basin (China)<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Place<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Nanpanjiang Basin (China)<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/bassin_de_nanpanjiang<\/a>> # Bassin de Nanpanjiang<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Thing<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Bassin de Nanpanjiang<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
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<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/orogenese_indosinienne<\/a>> # Orogen\u00E8se Indosinienne<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Thing<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Orogen\u00E8se Indosinienne<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Thing\/trias<\/a>> # Trias<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Thing<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Trias<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Topic\/orogenese_chine_sud_ouest<\/a>> # Orogen\u00E8se--Chine (sud-ouest)<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Intangible<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"Orogen\u00E8se--Chine (sud-ouest)<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/experiment.worldcat.org\/entity\/work\/data\/9348185321#Topic\/sedimentologie_chine_sud_ouest<\/a>> # S\u00E9dimentologie--Chine (sud-ouest)<\/span>\n\u00A0\u00A0\u00A0\u00A0a \nschema:Intangible<\/a> ;\u00A0\u00A0\u00A0\nschema:name<\/a> \"S\u00E9dimentologie--Chine (sud-ouest)<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/id.loc.gov\/vocabulary\/countries\/fr<\/a>>\u00A0\u00A0\u00A0\u00A0a \nschema:Place<\/a> ;\u00A0\u00A0\u00A0\ndcterms:identifier<\/a> \"fr<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/www.theses.fr\/2018ORLE2040\/document<\/a>>\u00A0\u00A0\u00A0\nrdfs:comment<\/a> \"Acc\u00E8s au texte int\u00E9gral<\/span>\" ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n
<http:\/\/www.worldcat.org\/title\/-\/oclc\/1105202050<\/a>>\u00A0\u00A0\u00A0\u00A0a \ngenont:InformationResource<\/a>, genont:ContentTypeGenericResource<\/a> ;\u00A0\u00A0\u00A0\nschema:about<\/a> <http:\/\/www.worldcat.org\/oclc\/1105202050<\/a>> ; # Sedimentary and structural characteristics of the Triassic Nanpanjiang Basin (Southwest China). New insights on the regional tectonic evolution<\/span>\n\u00A0\u00A0\u00A0\nschema:dateModified<\/a> \"2020-10-11<\/span>\" ;\u00A0\u00A0\u00A0\nvoid:inDataset<\/a> <http:\/\/purl.oclc.org\/dataset\/WorldCat<\/a>> ;\u00A0\u00A0\u00A0\u00A0.\n\n\n<\/div>\n\n

Content-negotiable representations<\/p>\n