Mantle deformation during rifting: Constraints from quantitative microstructural analysis of olivine from the East African Rift (Marsabit, Kenya)
Lherzolitic and harzburgitic peridotite xenoliths from the Marsabit volcanic field of the East-African Rift,Kenya, display a range of porphyroclastic to ultramylonitic textures that record intense deformation andstrain localisation during decompression, cooling and exhumation of subcontinental mantl...
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| Format: | Journal Article |
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Elsevier Science BV
2013
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| Online Access: | http://hdl.handle.net/20.500.11937/49050 |