@article{gledocs_11858_10802,
author = {Kleest, Christin and Webb, Sharon L. and Fanara, Sara},
title = {Rheology of melts from the colli albani volcanic district (Italy): a case study},
year = {2020-08-14},
volume = {175},
number = {9},
publisher = {Springer Berlin Heidelberg},
publisher = {},

abstract = {In this study the first viscosity measurements in the glass transition range of melts from highly explosive large-volume eruptions from the Colli Albani Volcanic District (CAVD) are presented. The magmas are ultrapotassic, rich in iron and CaO and characterised by a low silica content (< 45 wt%). Melt compositions range from tephri-phonolitic to foiditic. The Colli Albani eruptions appear anomalous since they produced a large volume of erupted material in spite of their silica undersaturated compositions. The viscosity of the Colli Albani melt changes as the melt composition evolves from the original melt to a country-rock contaminated melt to a crystal-bearing melt with a permanent decrease in liquid viscosity. Conventional estimations of viscosities assume these magmas to have a low viscosity. The presented data show that the melt viscosities are higher than expected. Taking into account further chemical or rheological features of a melt, the investigated CAVD melts are not that striking as assumed in comparison with other large-volume eruptions. Consequently, considering the alkaline-earth to alkaline ratio together with the SiO2 content could provide an alternative when comparing large volume eruptions.},
note = { \url {http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10802}},
}