Zobrazeno 1 - 4
of 4
pro vyhledávání: '"El-Hocine Fettous"'
Autor:
Fabrício de Andrade Caxito, Lauro Cézar Montefalco de Lira Santos, Carlos Eduardo Ganade, Abderrahmane Bendaoud, El-Hocine Fettous, Merlain Houketchang Bouyo
Publikováno v:
Brazilian Journal of Geology, Vol 50, Iss 2 (2020)
Abstract Both the Borborema Province of NE Brazil and the geological provinces of NW Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and the Central African Orogen of Cameroon, Chad, and Central African Republic)
Externí odkaz:
https://doaj.org/article/7d2517599d454cc19c7eba41595b6efd
Autor:
Merlain Houketchang Bouyo, Fabrício de Andrade Caxito, Carlos E. Ganade, Lauro Cézar Montefalco de Lira Santos, Abderrahmane Bendaoud, El-Hocine Fettous
Publikováno v:
Brazilian Journal of Geology, Vol 50, Iss 2 (2020)
Brazilian Journal of Geology v.50 n.2 2020
Brazilian Journal of Geology
Sociedade Brasileira de Geologia (SBGEO)
instacron:SBGEO
Brazilian Journal of Geology v.50 n.2 2020
Brazilian Journal of Geology
Sociedade Brasileira de Geologia (SBGEO)
instacron:SBGEO
Both the Borborema Province of NE Brazil and the geological provinces of NW Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and the Central African Orogen of Cameroon, Chad, and Central African Republic) are compl
Autor:
Sonia Ouadahi, Abderrahmane Bendaoud, Jean-Louis Bodinier, Jean-Marie Dautria, Alain Vauchez, El-Hocine Fettous, Olivier Alard
Publikováno v:
Precambrian Research
Precambrian Research, Elsevier, 2022, 369, pp.106505. ⟨10.1016/j.precamres.2021.106505⟩
Precambrian Research, Elsevier, 2022, 369, pp.106505. ⟨10.1016/j.precamres.2021.106505⟩
International audience; The assembly of West Gondwana supercontinent involved several complex processes that led to the formation of the Hoggar shield during the Panafrican-Brasiliano event. We present the first petro-geochemical, geochronological an
Publikováno v:
Precambrian Research. 368:106484
The vast Tin Begane batholith (5000 km2) is located in the Laouni terrane, LATEA metacraton, Central Hoggar and emplaced in the middle crust (c. 4.2 kbar). High-K calc-alkaline, metaluminous and magnesian as a whole, it comprises two distinct groups: