


Extreme 18O-enrichment in majorite constrains a crustal origin of transition zone diamonds
R.B. Ickert, T. Stachel, R.A. Stern, J.W. Harris 1 1507 13 May 2015 18 May 2015 9 June 2015 65 74 0 Next article >> 7 ‰) sufficiently strong to cause the observed 13C depleted signature. Similarly, evidence based on the rare earth element signatures (observation of...
Magnesium isotopic systematics of metapelite in the deep crust and implications for granite petrogenesis
S.-J. Wang, F.-Z. Teng, F. Bea 1 1508 17 April 2015 05 June 2015 22 June 2015 75 83 0 Next article >> 830 ºC; Whalen et al., 1987 Whalen, J.B., Currie, K.L., Chappell, B.W. (1987) A-type granites: geochemical characteristics, discrimination and petrogenesis....
The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet
J.R. Hawkings, J.L. Wadham, M. Tranter, E. Lawson, A. Sole, T. Cowton, A.J. Tedstone, I. Bartholomew, P. Nienow, D. Chandler, J. Telling 1 1510 10 March 2015 19 June 2015 23 June 2015 94 104 0 Next article...