Origin by fractional crystallization of transitional basalt for the Asela-Ziway pantellerites. Crustal control in the genesis of Plio-Quaternary bimodal magmatism of the Main Ethiopian Rift (MER): geochemical and isotopic (Sr, Nd, Pb) evidence by Trua et al. (1999)-Reference-Cited by-同舟云学术

Origin by fractional crystallization of transitional basalt for the Asela-Ziway pantellerites. Crustal control in the genesis of Plio-Quaternary bimodal magmatism of the Main Ethiopian Rift (MER): geochemical and isotopic (Sr, Nd, Pb) evidence by Trua et al. (1999)

Published:2000-07 Issue:1-2 Volume:168 Page:1-3
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Ayalew Dereje

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference14 articles.

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2. Chemical variations in a bimodal mamga system: the Plio-Quaternary volcanism in the Dera Nazret area (Main Ethiopian Rift, Ethiopia);Boccaletti;Afr. Geosci. Rev.,1995

3. Genesis of silicic peralkaline volcanic rocks in an ocean island setting by crustal melting and open-system processes: Socorro island, Mexico;Bohrson;J. Petrol.,1997

4. The geochemistry of volcanic rocks from Pantelleria Island, Sicily Channel: petrogenesis and characteristics of the mantle source region;Civetta;J. Petrol.,1998

5. The Ethiopian Rift Valley (between 7 and 8.40′ Lat. North);Dipaola;Bull. Volcanol.,1972

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