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\begin{document}

\title{Parameters controlling the eruption frequency of long-lived felsic
magmatic systems: an example from the Milos volcanic field (Greece).}



\author[1]{Xiaolong Zhou}%
\author[2]{Klaudia F. Kuiper}%
\author[3]{Jan R. Wijbrans}%
\author[2]{Pieter Vroon}%
\affil[1]{Vrije Universiteit Amsterdam}%
\affil[2]{Vrije Universiteit}%
\affil[3]{VU University Amsterdam}%


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  \date{June 15, 2024}


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\begin{abstract}
The observation that individual volcanic centres have their own eruption
frequencies has been known for a long time but is as yet poorly
understood. The key to a better understanding of the mechanisms
controlling the eruption frequency comes from integrating accurate
geochronology and geochemical data with numerical models. In many
silicic volcanic systems, the eruption frequency is studied for short
timescales of \textless{}1 Ma. Here, we combine two published numerical
models to improve our understanding of the eruption frequency in a
long-lived (\textgreater{}3 Ma) felsic magmatic system, the Milos
volcanic field. From these two models, we interpret the time intervals
between magma pulses into the subvolcanic reservoir
(t\textsubscript{i}), the rates of magma supply (Q\textsubscript{av})
and chamber growth rates (G\textsubscript{mc}) as the key parameters
controlling the eruption frequency. During the time intervals of
1.5-1.04 Ma and 0.97-0.63 Ma the t\textsubscript{i} is longer than 500
years and the volcanic quiescence periods are longer than 350 ka.
Furthermore, these periods are characterized by low values for
Q\textsubscript{av} ([?] 0.001
km\textsuperscript{3}\selectlanguage{ngerman}·yr\textsuperscript{-1}) and for
G\textsubscript{mc} (\textless{}0.0008
km\textsuperscript{3}·yr\textsuperscript{-1}). In contrast, during the
time intervals of 3.3-1.5 Ma and 0.60-0.06 Ma, the t\textsubscript{i} is
shorter (\textless{}0.5 ka) and the values for Q\textsubscript{av}
(\textgreater{} 0.001 km\textsuperscript{3}·yr\textsuperscript{-1}) and
for G\textsubscript{mc} (\textgreater{} 0.001
km\textsuperscript{3}·yr\textsuperscript{-1}) are higher corresponding
to frequent eruptions. The parameters t\textsubscript{i},
Q\textsubscript{av}, and G\textsubscript{mc} appear to determine the
eruption frequency of a volcanic system. Changes in one or more of these
three parameters of the Milos volcanic field correlate with changes in
the tectonic stress field.%
\end{abstract}\selectlanguage{ngerman}%



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