Matches in SemOpenAlex for { <https://semopenalex.org/work/W4281771507> ?p ?o ?g. }
- W4281771507 endingPage "104610" @default.
- W4281771507 startingPage "104610" @default.
- W4281771507 abstract "Metasandstones from early Cambrian to early Carboniferous stratigraphic successions were sampled in the Rehamna massif of the Western Meseta in Morocco. The early Cambrian sample shows a single Paleoproterozoic population at ca. 2 Ga suggesting a local basement source. The Ordovician sample is largely dominated by a Cryogenian-Ediacaran population and minor Paleoproterozoic peaks. The Devonian sample reveals age populations similar to North-West African Cambrian to Devonian age spectra indicating that the southern-derived West Gondwana source essentially pertained up to the Devonian. The two early Carboniferous samples show more heterogeneous zircon age spectra with a marked Ediacaran peak accompanied by Paleoproterozoic and Mesoproterozoic sub-peaks indicating important re-organization of the drainage systems. One sample also shows presence of Upper Devonian to early Carboniferous zircon grains, which suggests local magmatic sources associated to the formation of intracontinental extensional basins. The comparison of detrital zircon spectra with paleogeographic reconstructions indicate that the early Carboniferous change in detrital zircon sources can be interpreted in the framework of the opening of the Paleotethys ocean with coeval erosion of orogenic topographies linked to the emplacement of a Mid-Variscan Allochthon, and/or collision of an Avalonian indenter to the north." @default.
- W4281771507 created "2022-06-13" @default.
- W4281771507 creator A5000413232 @default.
- W4281771507 creator A5021087347 @default.
- W4281771507 creator A5031543307 @default.
- W4281771507 creator A5049688961 @default.
- W4281771507 creator A5053029204 @default.
- W4281771507 creator A5081299120 @default.
- W4281771507 creator A5083005320 @default.
- W4281771507 date "2022-10-01" @default.
- W4281771507 modified "2023-09-27" @default.
- W4281771507 title "U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif" @default.
- W4281771507 cites W1428601112 @default.
- W4281771507 cites W1580835259 @default.
- W4281771507 cites W1829099766 @default.
- W4281771507 cites W1978105167 @default.
- W4281771507 cites W1981036127 @default.
- W4281771507 cites W1983675476 @default.
- W4281771507 cites W1989286012 @default.
- W4281771507 cites W1993302664 @default.
- W4281771507 cites W1996228785 @default.
- W4281771507 cites W1996920988 @default.
- W4281771507 cites W2016082826 @default.
- W4281771507 cites W2018021159 @default.
- W4281771507 cites W2020139762 @default.
- W4281771507 cites W2020973699 @default.
- W4281771507 cites W2028904790 @default.
- W4281771507 cites W2036622817 @default.
- W4281771507 cites W2039872199 @default.
- W4281771507 cites W2049653977 @default.
- W4281771507 cites W2056041163 @default.
- W4281771507 cites W2080931112 @default.
- W4281771507 cites W2091067705 @default.
- W4281771507 cites W2092901514 @default.
- W4281771507 cites W2095016071 @default.
- W4281771507 cites W2105652317 @default.
- W4281771507 cites W2109694953 @default.
- W4281771507 cites W2139096563 @default.
- W4281771507 cites W2139326036 @default.
- W4281771507 cites W2169766597 @default.
- W4281771507 cites W2195287487 @default.
- W4281771507 cites W2515560417 @default.
- W4281771507 cites W2527875242 @default.
- W4281771507 cites W2547433798 @default.
- W4281771507 cites W2594320557 @default.
- W4281771507 cites W2767699940 @default.
- W4281771507 cites W2772693715 @default.
- W4281771507 cites W2776513136 @default.
- W4281771507 cites W2780464171 @default.
- W4281771507 cites W2796600848 @default.
- W4281771507 cites W2808123073 @default.
- W4281771507 cites W2883898733 @default.
- W4281771507 cites W2884441216 @default.
- W4281771507 cites W2890971385 @default.
- W4281771507 cites W2900075580 @default.
- W4281771507 cites W2938881728 @default.
- W4281771507 cites W2940226022 @default.
- W4281771507 cites W3016310266 @default.
- W4281771507 cites W3017211746 @default.
- W4281771507 cites W3047607448 @default.
- W4281771507 cites W3126288227 @default.
- W4281771507 cites W3170538944 @default.
- W4281771507 cites W3177834491 @default.
- W4281771507 cites W3200466102 @default.
- W4281771507 cites W4245429158 @default.
- W4281771507 doi "https://doi.org/10.1016/j.jafrearsci.2022.104610" @default.
- W4281771507 hasPublicationYear "2022" @default.
- W4281771507 type Work @default.
- W4281771507 citedByCount "2" @default.
- W4281771507 countsByYear W42817715072022 @default.
- W4281771507 countsByYear W42817715072023 @default.
- W4281771507 crossrefType "journal-article" @default.
- W4281771507 hasAuthorship W4281771507A5000413232 @default.
- W4281771507 hasAuthorship W4281771507A5021087347 @default.
- W4281771507 hasAuthorship W4281771507A5031543307 @default.
- W4281771507 hasAuthorship W4281771507A5049688961 @default.
- W4281771507 hasAuthorship W4281771507A5053029204 @default.
- W4281771507 hasAuthorship W4281771507A5081299120 @default.
- W4281771507 hasAuthorship W4281771507A5083005320 @default.
- W4281771507 hasBestOaLocation W42817715072 @default.
- W4281771507 hasConcept C107832698 @default.
- W4281771507 hasConcept C109007969 @default.
- W4281771507 hasConcept C127313418 @default.
- W4281771507 hasConcept C127413603 @default.
- W4281771507 hasConcept C13106087 @default.
- W4281771507 hasConcept C147176958 @default.
- W4281771507 hasConcept C149918038 @default.
- W4281771507 hasConcept C151730666 @default.
- W4281771507 hasConcept C160776313 @default.
- W4281771507 hasConcept C17409809 @default.
- W4281771507 hasConcept C181727316 @default.
- W4281771507 hasConcept C202746551 @default.
- W4281771507 hasConcept C2778849375 @default.
- W4281771507 hasConcept C2780049196 @default.
- W4281771507 hasConcept C2781148125 @default.
- W4281771507 hasConcept C2781297371 @default.
- W4281771507 hasConceptScore W4281771507C107832698 @default.
- W4281771507 hasConceptScore W4281771507C109007969 @default.