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![The xenon isotopic signature of the mantle beneath Massif Central](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/04/GPL1805_abstract-1.jpg)
![Oxygen minimum zones in the early Cambrian ocean](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/05/GPL1806_abstract.jpg)
Oxygen minimum zones in the early Cambrian ocean
R. Guilbaud, B.J. Slater, S.W. Poulton, T.H.P. Harvey, J.J. Brocks, B.J. Nettersheim, N.J. Butterfield 6 1806 18 September 2017 07 February 2018 1 March 2018 33 38 5734 Next article...![Diffusive fractionation of Li isotopes in wet, highly silicic melts](https://www.geochemicalperspectivesletters.org/wp-content/uploads/2020/04/GPL1807_abstract.jpg)
Diffusive fractionation of Li isotopes in wet, highly silicic melts
M.E. Holycross, E.B. Watson, F.M. Richter, J. Villeneuve 06 1807 16 November 2017 9 February 2018 5 March 2018 39 42 4260 Next article >> 0) faster than 7Li, fractionating the isotopes in the melt. If the Li isotopes were diffusing at the same speed in rhyolitic...Reply to Comment on “Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes” by Griffin et al., 2018: No evidence for transition zone metamorphism in the Luobusa ophiolite
C. Ballhaus, R.O.C. Fonseca, A. Bragagni 7 1810 06 January 2018 29 January 2018 9 March 2018 3 4 3815 Next article >> 12 GPa because it carries clinopyroxene exsolutions. In the Griffin et al. (2016a) Griffin, W.L., Afonso, J.C., Belousova, E.A., Gain, S.E., Gong,...![Comment on “Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes”](https://www.geochemicalperspectivesletters.org/wp-content/uploads/images/comment_and_reply-1.jpg)