FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2040377046> ?p ?o ?g. }

• W2040377046 endingPage "279" @default.
• W2040377046 startingPage "258" @default.
• W2040377046 abstract "Mapping and documentation of lithological varieties and their corresponding geochemistry at the Kitongo uranium mineralization were concerned. The Kitongo U occurrence is hosted by granitic rocks that include interleaved sequences of metasedimentary and metavolcanic rocks of the collectively termed Poli Group. U-mineralization and Na-metasomatism are related and structurally controlled. The most promising uraniferous bodies are intimately related to intersections between the ductile ENE-trending faults and the brittle conjugate R' faults postdating the shearing event. The con- centration of uranium at fault intersections rather than along individual faults suggests that these zones that are dilatational in nature were also highly permeable and therefore the hydrothermal fluids ponded there could readily precipitate U therein. A two-stage albitization has altered the foliated granitic host rock and the second albitization that has over-printed the first one is more effective at fault intersections. Whole rock geochemistry was performed by using ICP-MS and ICP-AES respectively for major oxides, trace and REE. The U-bearing rock suite exhibits restricted range in SiO2 concentration (62.89% - 70.91%) and Al2O3 (13.16% - 18.59%) and it is poor in MgO (0.02% - 1.03%), CaO (0.24% - 1.88%) and K2O (0.08% - 5.32%). The mineralized rocks are however comparatively richer in Na2O (4.33% - 10.92%) compared to their barren counterparts. The host granite and associated granodioritic rocks in the area are weakly metaluminous, peralkaline, and are calc-alkaline. They are moderately to strongly fractionated and have tholeiitic and shoshonitic affinities with moderate to high HFSE (high field strength elements) and LILE (large ion lithophile elements) enrichment. The Rb/Sr, Rb/Ba and Sr/Ba ratios are 0.31, 0.14 and 1.48, respectively. U content in the mineralized granite is up to 651 ppm while the non-mineralized rock has only 2.4 ppm U. The REE patterns of the granite show LREE enrichment and strong Eu negative anomalies (Eu/Eu* = 0.03 to 0.48). The main mineralization stage characterized by local U, Na, Pb, Zn, Ga, Hf, Sr, Fe, Al, P and Zr enrichments is related to the second albitization event and could probably be associated in time with the calcite-uranium stage. The identification of fault segments favorable for uranium mineralization in northern Cameroon (Poli area) is important for understanding the genesis of hydrothermal ore deposits within continental strike-slip faults and therefore has great implications for exploration strategies." @default.
• W2040377046 created "2016-06-24" @default.
• W2040377046 creator A5016318750 @default.
• W2040377046 creator A5027635612 @default.
• W2040377046 creator A5069718401 @default.
• W2040377046 creator A5072785810 @default.
• W2040377046 date "2012-01-01" @default.
• W2040377046 modified "2023-10-14" @default.
• W2040377046 title "Na-Metasomatism and Uranium Mineralization during a Two-Stage Albitization at Kitongo, Northern Cameroon: Structural and Geochemical Evidence" @default.
• W2040377046 cites W1965894220 @default.
• W2040377046 cites W1971685925 @default.
• W2040377046 cites W1973342441 @default.
• W2040377046 cites W1975126732 @default.
• W2040377046 cites W1986275976 @default.
• W2040377046 cites W1990767147 @default.
• W2040377046 cites W1994721714 @default.
• W2040377046 cites W1995202272 @default.
• W2040377046 cites W1995657303 @default.
• W2040377046 cites W2000249710 @default.
• W2040377046 cites W2007695812 @default.
• W2040377046 cites W2010560924 @default.
• W2040377046 cites W2011885262 @default.
• W2040377046 cites W2013377619 @default.
• W2040377046 cites W2019409833 @default.
• W2040377046 cites W2019872605 @default.
• W2040377046 cites W2021726465 @default.
• W2040377046 cites W2021987309 @default.
• W2040377046 cites W2025031866 @default.
• W2040377046 cites W2029923666 @default.
• W2040377046 cites W2032077846 @default.
• W2040377046 cites W2048294410 @default.
• W2040377046 cites W2075666634 @default.
• W2040377046 cites W2078846635 @default.
• W2040377046 cites W2079242815 @default.
• W2040377046 cites W2081673195 @default.
• W2040377046 cites W2084448379 @default.
• W2040377046 cites W2086162992 @default.
• W2040377046 cites W2087177400 @default.
• W2040377046 cites W2092720542 @default.
• W2040377046 cites W2127546698 @default.
• W2040377046 cites W2133107978 @default.
• W2040377046 cites W2144329035 @default.
• W2040377046 doi "https://doi.org/10.4236/ijg.2012.31028" @default.
• W2040377046 hasPublicationYear "2012" @default.
• W2040377046 type Work @default.
• W2040377046 sameAs 2040377046 @default.
• W2040377046 citedByCount "32" @default.
• W2040377046 countsByYear W20403770462013 @default.
• W2040377046 countsByYear W20403770462014 @default.
• W2040377046 countsByYear W20403770462015 @default.
• W2040377046 countsByYear W20403770462016 @default.
• W2040377046 countsByYear W20403770462017 @default.
• W2040377046 countsByYear W20403770462018 @default.
• W2040377046 countsByYear W20403770462019 @default.
• W2040377046 countsByYear W20403770462020 @default.
• W2040377046 countsByYear W20403770462021 @default.
• W2040377046 countsByYear W20403770462022 @default.
• W2040377046 countsByYear W20403770462023 @default.
• W2040377046 crossrefType "journal-article" @default.
• W2040377046 hasAuthorship W2040377046A5016318750 @default.
• W2040377046 hasAuthorship W2040377046A5027635612 @default.
• W2040377046 hasAuthorship W2040377046A5069718401 @default.
• W2040377046 hasAuthorship W2040377046A5072785810 @default.
• W2040377046 hasBestOaLocation W20403770461 @default.
• W2040377046 hasConcept C111696902 @default.
• W2040377046 hasConcept C120806208 @default.
• W2040377046 hasConcept C127313418 @default.
• W2040377046 hasConcept C147645078 @default.
• W2040377046 hasConcept C151730666 @default.
• W2040377046 hasConcept C156622251 @default.
• W2040377046 hasConcept C159390177 @default.
• W2040377046 hasConcept C159750122 @default.
• W2040377046 hasConcept C167919410 @default.
• W2040377046 hasConcept C17409809 @default.
• W2040377046 hasConcept C191897082 @default.
• W2040377046 hasConcept C192562407 @default.
• W2040377046 hasConcept C195843664 @default.
• W2040377046 hasConcept C2776152364 @default.
• W2040377046 hasConcept C2778849375 @default.
• W2040377046 hasConcept C555451288 @default.
• W2040377046 hasConcept C67236022 @default.
• W2040377046 hasConceptScore W2040377046C111696902 @default.
• W2040377046 hasConceptScore W2040377046C120806208 @default.
• W2040377046 hasConceptScore W2040377046C127313418 @default.
• W2040377046 hasConceptScore W2040377046C147645078 @default.
• W2040377046 hasConceptScore W2040377046C151730666 @default.
• W2040377046 hasConceptScore W2040377046C156622251 @default.
• W2040377046 hasConceptScore W2040377046C159390177 @default.
• W2040377046 hasConceptScore W2040377046C159750122 @default.
• W2040377046 hasConceptScore W2040377046C167919410 @default.
• W2040377046 hasConceptScore W2040377046C17409809 @default.
• W2040377046 hasConceptScore W2040377046C191897082 @default.
• W2040377046 hasConceptScore W2040377046C192562407 @default.
• W2040377046 hasConceptScore W2040377046C195843664 @default.
• W2040377046 hasConceptScore W2040377046C2776152364 @default.
• W2040377046 hasConceptScore W2040377046C2778849375 @default.
• W2040377046 hasConceptScore W2040377046C555451288 @default.
• W2040377046 hasConceptScore W2040377046C67236022 @default.

• next