1. Highly siderophile element (HSE) abundances in the mantle of Mars are due to core formation at high pressure and temperature. (6th January 2015) Authors: Righter, K.; Danielson, L. R.; Pando, K. M.; Williams, J.; Humayun, M.; Hervig, R. L.; Sharp, T. G. Journal: Meteoritics & planetary science Issue: Volume 50:Number 4(2015:Apr.) Page Start: 604 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. Investigating the response of biotite to impact metamorphism: Examples from the Steen River impact structure, Canada. (27th November 2017) Authors: Walton, E. L.; Sharp, T. G.; Hu, J.; Tschauner, O. Journal: Meteoritics & planetary science Issue: Volume 53:Number 1(2018) Page Start: 75 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗