Initiation of melting beneath the Oslo rift: a melt inclusion perspective. Pagina's 221-236

L.A. Kirstein; L. Dunworth; I. Nikogosian; J.L.R. Touret; W. Luistenhower

doi:10.1016/S0009-2541(01)00379-5

Initiation of melting beneath the Oslo rift: a melt inclusion perspective. Pagina's 221-236

L.A. Kirstein, L. Dunworth, I. Nikogosian, J.L.R. Touret, W. Luistenhower

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Abstract

This study of the most primitive magmas in the Permo-Carboniferous Oslo magmatic system aims at understanding the initial phases of magmatism in a rift-related environment. Primary melt inclusions are investigated from two compositional types of pyroxene: Cr-diopside and Ti-augite, found within the alkaline Skien basalts, southern Norway. Data from the analyses of melt inclusions in this tectonic setting indicate that the melting process is complex. In both types of pyroxene, two groups of melt inclusions can be identified, together with rare CO

Original language	English
Pages (from-to)	221-236
Journal	Chemical Geology
Volume	183
Issue number	1-3
DOIs	https://doi.org/10.1016/S0009-2541(01)00379-5
Publication status	Published - 2002

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10.1016/S0009-2541(01)00379-5

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abstract = "This study of the most primitive magmas in the Permo-Carboniferous Oslo magmatic system aims at understanding the initial phases of magmatism in a rift-related environment. Primary melt inclusions are investigated from two compositional types of pyroxene: Cr-diopside and Ti-augite, found within the alkaline Skien basalts, southern Norway. Data from the analyses of melt inclusions in this tectonic setting indicate that the melting process is complex. In both types of pyroxene, two groups of melt inclusions can be identified, together with rare CO",

author = "L.A. Kirstein and L. Dunworth and I. Nikogosian and J.L.R. Touret and W. Luistenhower",

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AU - Nikogosian, I.

AU - Touret, J.L.R.

AU - Luistenhower, W.

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AB - This study of the most primitive magmas in the Permo-Carboniferous Oslo magmatic system aims at understanding the initial phases of magmatism in a rift-related environment. Primary melt inclusions are investigated from two compositional types of pyroxene: Cr-diopside and Ti-augite, found within the alkaline Skien basalts, southern Norway. Data from the analyses of melt inclusions in this tectonic setting indicate that the melting process is complex. In both types of pyroxene, two groups of melt inclusions can be identified, together with rare CO

U2 - 10.1016/S0009-2541(01)00379-5

DO - 10.1016/S0009-2541(01)00379-5

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ER -

Initiation of melting beneath the Oslo rift: a melt inclusion perspective. Pagina's 221-236

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