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Accessory mineral constraints on crustal evolution: elemental fingerprints for magma discrimination
E. Bruand, M. Fowler, C. Storey O. Laurent, C. Antoine, M. Guitreau, E. Heilimo, O. Nebel 13 2006 27 August 2019 18 January 2020 26 February 2020 7 12 1965 Next article >> 15), with moderate negative Eu anomalies (Eu/Eu* ≈ 0.5). Similarly, sanukitoids and high Ba-Sr...![Unravelling lunar mantle source processes via the Ti isotope composition of lunar basalts](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/04/GPL2007_abstract.jpg)
Unravelling lunar mantle source processes via the Ti isotope composition of lunar basalts
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Massive sulfide Zn deposits in the Proterozoic did not require euxinia
J.M. Magnall, S.A. Gleeson, N. Hayward, A. Rocholl 13 2008 31 July 2019 27 January 2020 6 March 2020 19 24 7 Next article >> 25 ‰) correspond with euxinic conditions that developed due to high organic loading (i.e. productivity) and not basin restriction. This basin...![Mantle cooling causes more reducing volcanic gases and gradual reduction of the atmosphere](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/04/GPL2009_abstract.jpg)
Mantle cooling causes more reducing volcanic gases and gradual reduction of the atmosphere
S. Kadoya, D.C. Catling, R.W. Nicklas, I.S. Puchtel, A.D. Anbar 13 2009 11 October 2019 12 February 2020 16 March 2020 25 29 1392 Next article >> 1 with cooling, and an initial Koxy that is less than unity...![Concentration of meteoritic free organic matter by fluid transport and adsorption](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/04/GPL2010_abstract.jpg)