Eleanor S. Jennings
University of Bayreuth
24 Papers
40 Citations
Eleanor S. Jennings is an academic researcher from University of Bayreuth. The author has contributed to research in topics: Mantle (geology) & Olivine. The author has an hindex of 10, co-authored 17 publications. Previous affiliations of Eleanor S. Jennings include Paul Scherrer Institute & University of Cambridge.
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Papers
A Simple Thermodynamic Model for Melting of Peridotite in the System NCFMASOCr
Eleanor S. Jennings,Tim Holland +1 more
TL;DR: In this article, a thermodynamic model is presented for calculating phase relations in peridotite, from 0·001 to 60'kbar and from 800°C to liquidus temperatures, in the system NCFMASOCr.
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Characterization of magma from inclusions in zircon: Apatite and biotite work well, feldspar less so
TL;DR: In this paper, mineral inclusions in zircon grains from selected plutonic rocks from Dronning Maud Land, Antarctica, contain inclusions of apatite, biotite, amphibole and pyroxenes that accurately reflect the chemical compositions of the equivalent phases in the host-rock matrix, and the compositions of whole rocks.
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Deep mixing of mantle melts beneath continental flood basalt provinces: Constraints from olivine-hosted melt inclusions in primitive magmas
TL;DR: In this article, major and trace element compositions of 154 rehomogenised olivine-hosted melt inclusions found in primitive rocks (picrites and ferropicrites) from the Mesozoic Parana-Etendeka and Karoo Continental Flood Basalt (CFB) provinces are presented.
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Hot primary melts and mantle source for the Paraná-Etendeka flood basalt province: new constraints from Al-in-olivine thermometry
TL;DR: In this article, the authors applied the Al-in-olivine thermometer to olivine-spinel pairs from picrites and ferropicrites to calculate the potential temperature of the Parana-Etendeka CFB.
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Stability of Coronene at High Temperature and Pressure
TL;DR: Coronene has previously been shown to survive atmospheric entry during Earth accretion; this can now be extended to include survival through geological processes such as subduction and silicate melting of the rock cycle, opening the possibility of extraterrestrial coronene predating terrestrial accretion existing on Earth.
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