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- W2020143030 abstract "The history of the Amsinassène-Téfedest Block, in the central Hoggar domain, is characterized by a polycyclic evolution. The unreliable 1970 Ma age obtained on the Arechchoum gneisses, known to be Suggarian-Eburnean, might represent the effect of the Eburnean orogeny. A RbSr whole-rock age on the leucocratic fractions of gneisses point to a kibaran migmatization. This age confirms the existence of a Kibaran orogeny shown in the Aleksod area. The Pharusian-Pan African cycle, in this domain, is characterized by the emplacement of huge granitic bodies during two distinct magmatic phases: one of Late Proterozoic age (670 Ma) or Imezzarian phase, the other of Cambrian age as shown by the 546 and 515 Ma RbSr whole-rock ages obtained on late kinematic granitic plutons, Iskelian phase. The younger mineral ages (470430 Ma) indicate late vertical uplift of the central Hoggar." @default.
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- W2020143030 date "1979-08-01" @default.
- W2020143030 modified "2023-09-25" @default.
- W2020143030 title "Geochronological data on the Amsinassene-Tefedest Block (Central Hoggar, Algerian Sahara) and evidence for its polycyclic evolution" @default.
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- W2020143030 doi "https://doi.org/10.1016/0301-9268(79)90005-6" @default.
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