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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-17T12:17:56Z</responseDate> <request identifier=oai:HAL:hal-01667217v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01667217v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-PSUD</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:GEOPS</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> <setSpec>collection:UNIV-PSUD-SACLAY</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:UNIV-PARIS-SACLAY</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>The 2.1 Ga-old injectite network of the Franceville Basin, Gabon: Architecture, origin and implications on manganese mineralization</title> <creator>DUBOIS, Manon</creator> <creator>LOPEZ, Michel</creator> <creator>Orberger, Beate</creator> <creator>GAY, Aurelien</creator> <creator>Moussavou, Mathieu</creator> <creator>Pambo, Florent</creator> <creator>Rodrigues, Sophie</creator> <contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Géosciences Paris Sud (GEOPS) ; Université Paris-Sud - Paris 11 (UP11) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Université des sciences et techniques de Masuku, Franceville</contributor> <contributor>COMILOG SA, Moanda</contributor> <source>ISSN: 0301-9268</source> <source>Precambrian Research</source> <publisher>Elsevier</publisher> <identifier>hal-01667217</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01667217</identifier> <source>https://hal.archives-ouvertes.fr/hal-01667217</source> <source>Precambrian Research, Elsevier, 2017, 302, pp.255-278. 〈10.1016/j.precamres.2017.09.022〉</source> <identifier>DOI : 10.1016/j.precamres.2017.09.022</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.precamres.2017.09.022</relation> <language>en</language> <subject lang=en>Injectites</subject> <subject lang=en>Paleoproterozoic</subject> <subject lang=en>Franceville bassin</subject> <subject lang=en>Mn-carbonate</subject> <subject lang=en>Black mudstones</subject> <subject lang=en>turbidites</subject> <subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>Detailed sedimentological investigations on numerous outcrops and drill-core sections in the 2.1-Ga-old Franceville basin, Gabon, provide evidence for a large-scale injectite network. The injectites were formed by the injection of sands through a thickness of about 150 m of the FB1 Member, and now cover a minimum area of 70 km2 corresponding to the Bangombé plateau, but are also recognized close to Franceville 35 km farther south-east. The injectite lithology corresponds to a mud- or carbonate-supported sandstone characterized by a loose and uncompacted fabric contrasting with the host-rock. Because the injectites are often parallel to subparallel to the stratification, they were misinterpreted as depositional beds by previous authors. At outcrop, the injectite bodies exhibit sill, dyke, wing and protrusive geometries emplaced during early burial within poorly compacted material, with partial wall erosion and dissociation. The source of the sand material is attributed to a channel-levee turbidite depositional system located in the lower part of the FB1 Member. These deposits were buried by a thick biochemical muddy cap deposited during a starvation phase, which increased the seal capacity of the system. This type of architecture has a high potential to develop compaction disequilibrium during burial. Moreover, in the case of the Francevillian injectites, the abundance of microbial organic matter favoured early methane degassing and lateral charging of the sand reservoir. The overpressure in the channels was periodically released during early burial, through the effect of rapid sedimentary and tectonic loading, and possible seismic activity. The fluidized sand was injected according to a symmetrical wing pattern. Thus, the injected masses caused a local decrease in the grade of the lateritic manganese ore deposit of the Bangombé plateau.</description> <date>2017-11</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>