Trace Element Stratigraphy of the Bellevue Core, Northern Bushveld: Multiple Magma Injections Obscured by Diffusive Processes
The 3 km long Bellevue Core was recovered from the Upper Zone (UZ) and Main Zone (MZ) of the Northern Limb of the Bushveld Complexçthe largest known layered mafic intrusion. We present abundance data for 57 trace elements hosted in plagioclase, clinopyro
|Collections||ANU Research Publications|
|Source:||Journal of Petrology|
|01_Tanner_Trace_Element_Stratigraphy_of_2014.pdf||2.62 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.