Tracking chalcophile elements from source to vent at Kilauea Volcano, Hawaii

Add to your list(s) Download to your calendar using vCal

• Penny Wieser, University of Cambridge
• Wednesday 08 May 2019, 12:10-13:00
• Harker 2, Department of Earth Sciences, Downing Street.

If you have a question about this talk, please contact Emily Mason.

Kilauea Volcano emits globally significant quantities of S and sulfur loving (Chalcophile) elements into the atmosphere. These emissions have serious implications for respiratory health and agricultural productivity across the island. Yet, the processes controlling the concentration of these elements in erupted melts are enigmatic. Using high precision major and trace element measurements in melt inclusions and matrix glasses, we demonstrate that chalcophile element systematics at Kilauea are controlled by a number of processes, including the presence of sulfide in the mantle source, sulfide-liquid immiscibility during fractionation, sulfide resorption upon eruption, and the degassing of traditionally “refractory” chalcophile elements (e.g. Se). Our conclusions differ substantially from those of previous work, largely because in the literature, chalcophile elements have only been investigated in lava lakes (where the behaviour of S is anomalous due to syn-eruptive degassing).

This talk is part of the Cambridge Volcanology Seminar series.

This talk is included in these lists:

• Harker 2, Department of Earth Sciences, Downing Street
• AUB_Cambridge Seminars
• Cambridge Volcanology Seminar
• Department of Earth Sciences seminars
• Department of Geography
• ld636

Note that ex-directory lists are not shown.