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dc.contributor.authorPatel, J.P
dc.contributor.authorPalmer, H.C
dc.date.accessioned2013-07-04T13:49:21Z
dc.date.available2013-07-04T13:49:21Z
dc.date.issued1982
dc.identifier.citationJ.P. Patel and H.C. Palmer (1982). Results of optical, thermomagnetic and electron microprobe analyses of titanomagnetite grains. Physics of the Earth and Planetary Interiors Volume 30, Issue 4, December, Pages 373en
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/0031920182900462
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/45380
dc.description.abstractThis paper presents results of a study of titanomagnetite from specimens of ten different rock units. The rock units comprise trachytes, basalts, ignimbrites, nephelinites, olivine melanephelinites and welded tuffs from Kenya, with ages ranging from recent to Precambrian. The correlations of the stability index with opaque petrology and with thermomagnetic analyses of the titanomagnetite and titanomaghemite bearing specimens appear to be significant. Electron microprobe analyses of the titanomagnetite grains indicate a high percentage of “impurities” in the low stability index specimens and elevation of the Curie point in the high stability index specimens.en
dc.language.isoenen
dc.titleResults of optical, thermomagnetic and electron microprobe analyses of titanomagnetite grainsen
dc.typeArticleen
local.publisherDepartment of Physics, University of Nairobi, Kenyaen
local.publisherDepartment of Geophysics, University of Western Ontario, London, Canadaen


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