Stable Isotope (δ18O, δD) Composition of Magmatic Fluids Exsolved from an Active Alkaline Magma Cham...
Stable Isotope (δ18O, δD) Composition of Magmatic Fluids Exsolved from an Active Alkaline Magma Chamber—The Case of the AD 79 Magma Chamber of Vesuvius
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Basel: MDPI AG
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English
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Basel: MDPI AG
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This work documents, for the first time, the calculated oxygen and hydrogen isotope composition of the brines exsolved from the peripheral margin of the active magma alkaline chamber that fed the AD 79 (“Pompei”) eruption of Vesuvius. The exsolved hydrosaline fluids had a constant δ18O composition and a variable δD composition, showing a general lo...
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Stable Isotope (δ18O, δD) Composition of Magmatic Fluids Exsolved from an Active Alkaline Magma Chamber—The Case of the AD 79 Magma Chamber of Vesuvius
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TN_cdi_proquest_journals_2843097577
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2843097577
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ISSN
2075-163X
E-ISSN
2075-163X
DOI
10.3390/min13070913
