Very low-grade secondary minerals as indicators of palaeo-hydrothermal systems in the Upper Cretaceous volcanic succession of Hannah Point, Livingston Island, Antarctica
Published inApplied Clay Science, vol. 134, p. 246-256
Publication date2016
Abstract
Research group
Citation (ISO format)
BASTIAS SILVA, Miguel Joaquin et al. Very low-grade secondary minerals as indicators of palaeo-hydrothermal systems in the Upper Cretaceous volcanic succession of Hannah Point, Livingston Island, Antarctica. In: Applied Clay Science, 2016, vol. 134, p. 246–256. doi: 10.1016/j.clay.2016.07.025
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Identifiers
- PID : unige:109546
- DOI : 10.1016/j.clay.2016.07.025
ISSN of the journal0169-1317