Polyphase deformation of mylonites from the Renco gold mine (Zimbabwe): identified by crystallographic preferred orientation of quartz.<I> Journal of Structural Geology</I>, 25, 253-262.

Simple item page
dc.contributor.authorKolb J
dc.contributor.authorKisters AFM
dc.contributor.authorMeyer FM
dc.contributor.authorSiemes H
dc.date.accessioned2013-01-23T13:46:54Z
dc.date.available2013-01-23T13:46:54Z
dc.date.issued2003
dc.descriptionNatuurwetenskappe
dc.descriptionAardwetenskappe
dc.descriptionPlease help us populate SUNScholar with the post print version of this article. It can be e-mailed to: scholar@sun.ac.za
dc.identifier.citationJournal of Structural Geology
dc.identifier.urihttp://hdl.handle.net/10019.1/77143
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD, THE BOULEVARD, LANGFORD LANE, KIDLINGTON,OXFORD, ENGLAND, OX5 1GB
dc.titlePolyphase deformation of mylonites from the Renco gold mine (Zimbabwe): identified by crystallographic preferred orientation of quartz.<I> Journal of Structural Geology</I>, 25, 253-262.
dc.typeJournal Articles (subsidised)
Files
Collections
2003 - Research Outputs