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dc.contributor.authorMokhzani Khair, Ishak
dc.contributor.authorKhairul Nizar, Ismail
dc.contributor.authorKamarudin, Hussin
dc.contributor.authorWan Mohd Sabki, Wan Omar
dc.contributor.authorBanjuraizah, Johar
dc.contributor.authorMohd Nazry, Salleh
dc.contributor.authorUmar, Kassim
dc.date.accessioned2011-01-20T02:49:00Z
dc.date.available2011-01-20T02:49:00Z
dc.date.issued2009-11-09
dc.identifier.urihttp://dspace.unimap.edu.my/123456789/10499
dc.descriptionMineral Symposium 2009 (SIMPOMIN 2009) organized by Mineral Research Centre, from 9th - 11th November 2009 at Bukit Merah Laketown Resort, Perak.en_US
dc.description.abstractDolomite and limestone is considered under a sedimentary carbonated rocks. It contains almost same compound but major difference is on the amount of MgO and CaO which prove with XRF testing. MgO for dolomite shows 23% and much more higher than limestone while CaO amount for dolomite is 33.78% and this percentage does not fulfill the requirement in cement processing. Cement processing requires more than 47% amount of CaO and less than 5% MgO. XRF prove only limestone suit this requirement with 54.88% of CaO and 0.53% of MgO respectively.en_US
dc.language.isoenen_US
dc.publisherMineral Research Centreen_US
dc.relation.ispartofseriesProceedings of the Mineral Symposium 2009 (SIMPOMIN 2009)en_US
dc.subjectDolomiteen_US
dc.subjectLimestoneen_US
dc.subjectX-ray fluorescent (XRF)en_US
dc.subjectCement processingen_US
dc.titleCharacterization of limestone and dolomite using x-ray fluorescent (XRF) for cement processingen_US
dc.typeWorking Paperen_US
dc.contributor.urlmokhzani_ki@yahoo.comen_US
dc.contributor.urlnizar@unimap.edu.myen_US


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