A volcanic sublimate or fumarolic sublimate is a mineral which forms directly from volcanic gas, by the process of deposition, during an eruption or discharge from a volcanic vent or fumarole. Native sulfur is a common sublimate mineral and various halides, sulfides and sulfates occur in this environment associated with fumaroles and eruptions.
- Manahan, Stanley E. Environmental Chemistry, CRC Press, 2004, Eighth Edition, p. 408 ISBN 978-1566706339
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