Silica-rich melts in quartz xenoliths from Vulcano Island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, Southern Italy

M.L. Frezzotti; A. Peccerillo; V. Zavon; I. Nikogosian

doi:10.1093/petrology/egg080

Silica-rich melts in quartz xenoliths from Vulcano Island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, Southern Italy

M.L. Frezzotti, A. Peccerillo, V. Zavon, I. Nikogosian

Research output: Contribution to Journal › Article › Academic › peer-review

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Original language	English
Pages (from-to)	3-26
Journal	Journal of Petrology
Volume	45
Issue number	1
DOIs	https://doi.org/10.1093/petrology/egg080
Publication status	Published - 2004

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10.1093/petrology/egg080

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title = "Silica-rich melts in quartz xenoliths from Vulcano Island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, Southern Italy",

author = "M.L. Frezzotti and A. Peccerillo and V. Zavon and I. Nikogosian",

year = "2004",

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language = "English",

volume = "45",

pages = "3--26",

journal = "Journal of Petrology",

issn = "0022-3530",

publisher = "Oxford University Press",

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Silica-rich melts in quartz xenoliths from Vulcano Island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, Southern Italy. / Frezzotti, M.L.; Peccerillo, A.; Zavon, V.; Nikogosian, I.

In: Journal of Petrology, Vol. 45, No. 1, 2004, p. 3-26.

Research output: Contribution to Journal › Article › Academic › peer-review

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T1 - Silica-rich melts in quartz xenoliths from Vulcano Island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, Southern Italy

AU - Frezzotti, M.L.

AU - Peccerillo, A.

AU - Zavon, V.

AU - Nikogosian, I.

PY - 2004

Y1 - 2004

U2 - 10.1093/petrology/egg080

DO - 10.1093/petrology/egg080

M3 - Article

VL - 45

SP - 3

EP - 26

JO - Journal of Petrology

JF - Journal of Petrology

SN - 0022-3530

IS - 1

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