Bimodal zircon ages from Natash volcanics (southeast Egypt) and the link between eruption mechanisms and Late Cretaceous tectonics
|Author(s)||Abu El-Rus Mohamed Ali1, Paquette Jean-Louis2, Chazot Gilles3, Vannucci Riccardo4|
|Affiliation(s)||1 : Assiut Univ, Dept Geol, Fac Sci, Asyut 71516, Egypt.
2 : Univ Clermont Auvergne, Lab Magmas & Volcans, CNRS, IRD,OPGC, F-63000 Clermont Ferrand, France.
3 : Univ Brest UBO, IUEM, Geosci Ocean, UMR 6538, Pl Copernic, F-29280 Plouzane, France.
4 : Univ Pavia, Dipartimento Sci Terra & Ambiente, Via Ferrata 1, I-27100 Pavia, Italy.
|Source||Arabian Journal Of Geosciences (1866-7511) (Springer Heidelberg), 2019-05 , Vol. 12 , N. 9 , P. 291 (?p.)|
|WOS© Times Cited||3|
|Keyword(s)||Eastern Desert Egypt, Cretaceous volcanism, Natash volcanics, Trachyte plugs, U-Pb zircon ages|
Trachyte plugs from the Natash volcanic field have been precisely dated using in situ U-Pb geochronology on zircon grains at similar to 93Ma. Available zircon ages thus suggest that the overall volcanic history at Natash was probably shorter than previously estimated based on Rb-Sr and K-Ar ages, which are more sensitive to element mobility. Basaltic flows and trachyte plugs were produced by a largely synchronous, Upper Cretaceous volcanic activity that occurred in the Natash area at the onset of the extensional fracturing that preceded and accompanied the doming of the Afro-Arabian Shield. Extraction and eruption of volumetrically dominant basalts from deeper lithospheric levels were ruled by major NW-SE strike-slip faults, whereas both major and subordinate fault systems activated by successive tectonic pulses favoured the ascent of more evolved melts (i.e. trachytes and rhyolites) from shallow-level magma chambers. The study revealed also the presence of zircon xenocrysts in some trachyte plugs associated or not to magmatic zircon. These xenocrysts have pre-Cambrian ages (similar to 681Ma) matching those of zircons from basement rocks in the area (similar to 700Ma) and were most probably incorporated during the emplacement of trachyte plugs at shallow depths. The strictly bimodal ages recorded by zircons suggest a very large time gap (>500Ma) between the end of the Pan-African Orogeny and the onset of new tectono-magmatic activity in the Natash area.