Arc magmatism in the Nkoula granitoid suites, Central African Fold belt in Cameroon: evidence of a metasomatized high oxidized S- and I- type magma-Reference-Cited by-同舟云学术

Arc magmatism in the Nkoula granitoid suites, Central African Fold belt in Cameroon: evidence of a metasomatized high oxidized S- and I- type magma

Published:2022-03-07 Issue:4 Volume:111 Page:1223-1250
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Ntieche Benjamin^ORCID,Wokwenmendam Nguet Pauline,Moundi Amidou,Mekala Ram Mohan,Mounjouohou Mahomed Aziz,Atsalang Chimene Grace Staelle,Nchouwet Zakari

Funder

The Academy of Sciences for the Developing World

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s00531-022-02175-4.pdf

Reference115 articles.

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2. Abdel-Rahman AM (1994) Nature of biotites from alkaline, calc-alkaline, and peraluminous magmas. J Petrol 35:525–541

3. Anderson JL, Smith DR (1995) The effects of temperature and fO2 on the Al-in hornblende barometer. Am Miner 80:549–559

4. Atherton MP, Petford N (1993) Generation of sodium–rich magmas from newly Underplated basaltic crust. Nature 362(6416):144–146

5. Barbarin B (1999) A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos 46:605–626. https://doi.org/10.1016/S0024-4937(98)00085-1

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