Djerossem F. auteur aut IRD Berger J. auteur aut IRD Vanderhaeghe O. auteur aut IRD Isseini M. auteur aut IRD Ganne Jérôme auteur aut IRD Zeh A. auteur aut IRD text journalArticle eng text/pdf reformatted digital access This paper presents new petrological, geochemical, isotopic (Nd) and geochronological data on magmatic rocks from the poorly known southern Ouaddai massif, located at the southern edge of the so-called Saharan metacraton. This area is made of greenschist to amphibolite facies metasediments intruded by large pre- to syn-tectonic batholiths of leucogranites and an association of monzonite, granodiorite and biotite granite forming a late tectonic high-K calc-alkaline suite. U-Pb zircon dating yields ages of 635 +/- 3 Ma and 613 +/- 8 Ma on a peraluminous biotite-leucogranite (containing numerous inherited Archean and Paleoproterozoic zircon cores) and a muscovite-leucogranite, respectively. Geochemical fingerprints are very similar to some evolved Himalayan leucogranites suggesting their parental magmas were formed after muscovite and biotite dehydration melting of metasedimentary rocks. A biotite-granite sample belonging to the late tectonic high-K to shoshonitic suite contains zircon rims that yield an age of 540 +/- 5 Ma with concordant inherited cores crystallized around 1050 Ma. Given the high-Mg# (59) andesitic composition of the intermediate pyroxene-monzonite, the very similar trace-element signature between the different rock types and the unradiogenic isotopic signature for Nd, the late-kinematic high-K to shoshonitic rocks formed after melting of the enriched mantle and further differentiation in the crust. These data indicate that the southern Ouaddai was part of the Pan-African belt. It is proposed that it represents a continental back-arc basin characterized by a high-geothermal gradient during Early Ediacaran leading to anatexis of middle to lower crustal levels. After tectonic inversion during the main Pan-African phase, late kinematic high-K to shoshonitic plutons emplaced during the final post-collisional stage. specialized Central Africa Orogenic Belt Pan-African Saharan Metacraton peraluminous granites shoshonitic magmatism TCHAD SAHARA 064 066 191 34 [22 ] 2020 0037-9409 https://www.documentation.ird.fr/hor/fdi:010080427 0037-9409 [F B010080427] https://www.documentation.ird.fr/hor/fdi:010080427 https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers20-12/010080427.pdf IRD - Base Horizon / Pleins textes 2021-01-14 2021-04-05 fdi:010080427 fre