Hong, W., Xu, X. and Zou, H. (2013) Petrogenesis of Coexisting High-Silica Aluminous and Peralkaline Rhyolites from Yunshan (Yongtai), Southeastern China. Journal of Asian Earth Sciences, 74, 316-329.
https://doi.org/10.1016/j.jseaes.2013.01.005

has been cited by the following article:

• TITLE: Petrology of Metaluminous A-Type Rhyolite Discovered from Hadjer el Hamis Volcanoes (Lake Chad Basin)

  AUTHORS: Claudial Amane Lagmet, Fadimatou Ngounouno Yamgouot, Mama Ntoumbe, Abdou Aziz Youpougam, Ismaïla Ngounouno

  KEYWORDS: Metaluminous, Rhyolites, Lake Chad, Petrology, Hadjer el Hamis

  JOURNAL NAME: Open Journal of Geology, Vol.8 No.9, August 20, 2018

  ABSTRACT: Metaluminous (P.I. > 1) rhyolite from Hadjer el Hamis consisted of quartz, alkali feldspar, clinopyroxene (hedenbergite), amphibole (F-arfvedsonite) and oxides-hydroxides (ilmenite, magnetite, limonite) phenocrysts is characterized by the negative Eu, Ba, P, Sr and Ti anomalies. This metaluminous rhyolite and the early discovered peralkaline rhyolites in Hadjer el Hamis volcanoes derive likely from the same source, according to their coexistence on the same sector and their similar Zr/Nb ratios. The causes of magma heterogeneity are likely linked to varying amounts of extraction of an earlier melt phase or tectonic juxtaposition or a sudden increasing of fO2 in silicic magmas, triggered from a hydrothermal process, associated with F- and alkali-bearing fluids influx, which promoted the enrichment of Na in the hedenbergite rims and the crystallization of arfvedsonite.