1. In situ oxygen-isotope, major-, and trace-element constraints on the metasomatic modification and crustal origin of a diamondiferous eclogite from Roberts Victor, Kaapvaal Craton. (1st February 2016) Authors: Riches, A.J.V.; Ickert, R.B.; Pearson, D.G.; Stern, R.A.; Jackson, S.E.; Ishikawa, A.; Kjarsgaard, B.A.; Gurney, J.J. Journal: Geochimica et cosmochimica acta Issue: Volume 174(2016:Feb. 01) Page Start: 345 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. In situ oxygen-isotope, major-, and trace-element constraints on the metasomatic modification and crustal origin of a diamondiferous eclogite from Roberts Victor, Kaapvaal Craton. (1st February 2016) Authors: Riches, A.J.V.; Ickert, R.B.; Pearson, D.G.; Stern, R.A.; Jackson, S.E.; Ishikawa, A.; Kjarsgaard, B.A.; Gurney, J.J. Journal: Geochimica et cosmochimica acta Issue: Volume 174(2016:Feb. 01) Page Start: 345 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
3. Open system sulphate reduction in a diagenetic environment – Isotopic analysis of barite (δ34S and δ18O) and pyrite (δ34S) from the Tom and Jason Late Devonian Zn–Pb–Ba deposits, Selwyn Basin, Canada. (1st May 2016) Authors: Magnall, J.M.; Gleeson, S.A.; Stern, R.A.; Newton, R.J.; Poulton, S.W.; Paradis, S. Journal: Geochimica et cosmochimica acta Issue: Volume 180(2016:May 01) Page Start: 146 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
4. Open system sulphate reduction in a diagenetic environment – Isotopic analysis of barite (δ34S and δ18O) and pyrite (δ34S) from the Tom and Jason Late Devonian Zn–Pb–Ba deposits, Selwyn Basin, Canada. (1st May 2016) Authors: Magnall, J.M.; Gleeson, S.A.; Stern, R.A.; Newton, R.J.; Poulton, S.W.; Paradis, S. Journal: Geochimica et cosmochimica acta Issue: Volume 180(2016:May 01) Page Start: 146 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗