1. Evidence for silicate dissolution on Mars from the Nakhla meteorite. (28th January 2013) Authors: Lee, M. R.; Tomkinson, T.; Mark, D. F.; Stuart, F. M.; Smith, C. L. Journal: Meteoritics & planetary science Issue: Volume 48:Number 2(2013:Feb.) Page Start: 224 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. Formation of iddingsite veins in the martian crust by centripetal replacement of olivine: Evidence from the nakhlite meteorite Lafayette. (1st April 2015) Authors: Lee, M.R.; Tomkinson, T.; Hallis, L.J.; Mark, D.F. Journal: Geochimica et cosmochimica acta Issue: Volume 154(2015:Apr. 01) Page Start: 49 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
3. Opal‐A in the Nakhla meteorite: A tracer of ephemeral liquid water in the Amazonian crust of Mars. (30th June 2015) Authors: Lee, M. R.; MacLaren, I.; Andersson, S. M. L.; Kovács, A.; Tomkinson, T.; Mark, D. F.; Smith, C. L. Journal: Meteoritics & planetary science Issue: Volume 50:Number 8(2015:Aug.) Page Start: 1362 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗