The effect of degassing and volatile exsolution on the composition of a trachybasaltic melt decompressed at slow and fast rates

Download statistics - Document (COUNTER):

Mollo, S.; Vetere, F.; Beherens, H.; Tecchiato, V.; Langone, A.; Scarlato, P.; Perugini, D.: The effect of degassing and volatile exsolution on the composition of a trachybasaltic melt decompressed at slow and fast rates. In: Periodico di Mineralogia 86 (2017), Nr. 2, S. 185-197. DOI:

Repository version

To cite the version in the repository, please use this identifier:

Selected time period:


Sum total of downloads: 354

It is widely accepted that, for the correct interpretation of bulk rock compositions, degassing process controlling both loss of magmatic volatiles and significant changes in the contents of volatile chemical species must be considered. The continuous degassing experiments presented in this study attempt to determine the absolute and relative change in abundances of volatile components in the melt at shallow levels, simulating what might occur during slow and fast ascent of magma from depth without crystallization. We performed disequilibrium decompression experiments using as starting melt a bubble-free but volatile-bearing trachybasalt. The charges were isothermally decompressed at 1, 150 °C from 400 MPa down to 50 MPa at rates of 0.01 MPa/s and 1 MPa/s. Results demonstrate that degassing of 1 wt% H2O of initial volatile content in the melt is not enough to induce melt compositional changes as well as H2O supersaturation in the trachybasaltic melt. In contrast, the minimum H2O threshold to observe Cl, B, and Li devolatilization corresponds to 3 wt% H2O and volatile supersaturation is attained at the fast decompression rate of 1 MPa/s. An increase of CO2 up to 0.3 wt% do not change the partitioning behaviour of these chemical species between vapor and trachybasaltic melt. Moreover, CO2 degassing is less efficient with respect to H2O transfer from the melt into the vapor phase. As a consequence, the trachybasaltic melt is preferentially supersaturated in CO2 with decreasing pressure. Disequilibrium degassing does not change the bulk oxidation state of the melt.
License of this version: CC BY 4.0 Unported
Document Type: article
Publishing status: publishedVersion
Issue Date: 2017
Appears in Collections:Fakultät für Bauingenieurwesen und Geodäsie

distribution of downloads over the selected time period:

downloads by country:

pos. country downloads
total perc.
1 image of flag of Germany Germany 203 57.34%
2 image of flag of Italy Italy 35 9.89%
3 image of flag of United States United States 28 7.91%
4 image of flag of United Kingdom United Kingdom 15 4.24%
5 image of flag of Japan Japan 13 3.67%
6 image of flag of China China 9 2.54%
7 image of flag of France France 6 1.69%
8 image of flag of India India 5 1.41%
9 image of flag of Switzerland Switzerland 5 1.41%
10 image of flag of New Zealand New Zealand 3 0.85%
    other countries 32 9.04%

Further download figures and rankings:


Zur Erhebung der Downloadstatistiken kommen entsprechend dem „COUNTER Code of Practice for e-Resources“ international anerkannte Regeln und Normen zur Anwendung. COUNTER ist eine internationale Non-Profit-Organisation, in der Bibliotheksverbände, Datenbankanbieter und Verlage gemeinsam an Standards zur Erhebung, Speicherung und Verarbeitung von Nutzungsdaten elektronischer Ressourcen arbeiten, welche so Objektivität und Vergleichbarkeit gewährleisten sollen. Es werden hierbei ausschließlich Zugriffe auf die entsprechenden Volltexte ausgewertet, keine Aufrufe der Website an sich.

Search the repository