Constraints on the origin of sub-effusive nodules from the Sarno (Pomici di Base) eruption of Mt. Somma-Vesuvius (Italy) based on compositions of silicate-melt inclusions and clinopyroxene
Author:
Publisher
Mineralogical Society of America
Subject
Geochemistry and Petrology,Geophysics
Cited by 7 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. New views on Somma Vesuvius subvolcanic system and on mechanism that could increase eruption explosivity by a review and immiscibility in melt inclusions;Journal of Geochemical Exploration;2024-01
2. Mechanism of carbonate assimilation by intraplate basaltic magma and liquid immiscibility: example of Wangtian’e volcano (Changbaishan volcanic area, NE China);Frontiers in Earth Science;2023-12-19
3. Constraining the volatile evolution of mafic melts at Mt. Somma–Vesuvius, Italy, based on the composition of reheated melt inclusions and their olivine hosts;European Journal of Mineralogy;2023-11-09
4. Magmatic stoping during the caldera-forming Pomici di Base eruption (Somma-Vesuvius, Italy) as a fuel of eruption explosivity;Lithos;2020-10
5. Magmatism of the Phlegrean Volcanic Fields as revealed by melt inclusions;Vesuvius, Campi Flegrei, and Campanian Volcanism;2020
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