Skip to main content

Research Repository

Advanced Search

Petrography and Mineral Chemistry of Monte Epomeo Green Tuff, Ischia Island, South Italy: Constraints for Identification of the Y-7 Tephrostratigraphic Marker in Distal Sequences of the Central Mediterranean

D'Antonio, Massimo; Arienzo, Ilenia; Brown, Richard J.; Petrosino, Paola; Pelullo, Carlo; Giaccio, Biagio

Petrography and Mineral Chemistry of Monte Epomeo Green Tuff, Ischia Island, South Italy: Constraints for Identification of the Y-7 Tephrostratigraphic Marker in Distal Sequences of the Central Mediterranean Thumbnail


Authors

Massimo D'Antonio

Ilenia Arienzo

Paola Petrosino

Carlo Pelullo

Biagio Giaccio



Abstract

The 56 ka Monte Epomeo Green Tuff (MEGT) resulted from the largest volume explosive eruption from Ischia island (south Italy). Its tephra is one of the main stratigraphic markers of the central Mediterranean area. Despite its importance, a detailed characterisation of the petrography and mineral chemistry of MEGT is lacking. To fill this gap, we present detailed petrographic description and electron microprobe mineral chemistry data on samples collected on-land from the MEGT. Juvenile clasts include pumice, scoria, and obsidian fragments with porphyritic/glomeroporphyritic, vitrophyric, and fragmental textures. The porphyritic index is 13–40 vol.%, and phenocryst phases include alkali-feldspar, plagioclase, clinopyroxene, ferrian phlogopite, and titano-magnetite, in order of decreasing abundance; accessory phases include sphene, hydroxy-fluor-apatite, and rare edenite. Plagioclase varies from predominant andesine to subordinate oligoclase, whereas alkali-feldspar is more variable from sanidine to anorthoclase; quasi-pure sanidine commonly occurs as either rim or recrystallisation overgrowth of large phenocrysts due to hydrothermal alteration. Secondary minerals include veins and patches of carbonate minerals, Fe-Mn oxyhydroxides, clay minerals, and zeolites. Clinopyroxene is ferroan diopside (En45–29Fs7–27) and never reaches Na-rich compositions. This feature allows the discrimination of MEGT from aegirine-bearing, distal tephra layers erroneously attributed to MEGT, with implications for the areal distribution of Ischia explosive deposits.

Citation

D'Antonio, M., Arienzo, I., Brown, R. J., Petrosino, P., Pelullo, C., & Giaccio, B. (2021). Petrography and Mineral Chemistry of Monte Epomeo Green Tuff, Ischia Island, South Italy: Constraints for Identification of the Y-7 Tephrostratigraphic Marker in Distal Sequences of the Central Mediterranean. Minerals, 11(9), Article 955. https://doi.org/10.3390/min11090955

Journal Article Type Article
Acceptance Date Aug 29, 2021
Online Publication Date Aug 31, 2021
Publication Date 2021-09
Deposit Date Nov 1, 2021
Publicly Available Date Jan 24, 2022
Journal Minerals
Electronic ISSN 2075-163X
Publisher MDPI
Peer Reviewed Peer Reviewed
Volume 11
Issue 9
Article Number 955
DOI https://doi.org/10.3390/min11090955
Public URL https://durham-repository.worktribe.com/output/1223967

Files

Published Journal Article (5.3 Mb)
PDF

Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/

Copyright Statement
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.






You might also like



Downloadable Citations