“…This could be justified by the fact that, if more fine powder of reactive mineral is added, the reactive phase also increases. The changes in microstructure observed in SEM images are in line with the findings of other authors [32,33,44] who used a secondary aluminosilicate source as alumina, metakaolin, pumice and feldspars to improve the physico-chemical properties of geopolymer binder from volcanic scoria and metakaolin, respectively. They concluded that, with the more reactive additive mineral included into these systems, a higher dissolution extent of raw materials in alkaline media has been observed, the amorphous binder phase increased with Si/Al ratio in the range of 1-2, resulting in the development of higher strength.…”