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dc.contributor.authorMohd Nazry, Salleh
dc.contributor.authorKhairul Nizar, Ismail
dc.contributor.authorChe Mohd Ruzaidi, Ghazali
dc.contributor.authorSuhardy, Daud
dc.contributor.authorSaiful Azhar, Saad
dc.contributor.authorFarizul Hafiz, Kasim
dc.date.accessioned2008-08-27T06:47:30Z
dc.date.available2008-08-27T06:47:30Z
dc.date.issued2006-12-04
dc.identifier.urihttp://dspace.unimap.edu.my/123456789/1886
dc.descriptionOrganized by Kolej Universiti Sains dan Teknologi Malaysia (KUSTEM), 4th - 6th December 2006 at Terengganu.en_US
dc.description.abstractPerlis dolomite or locally known as ‘batu reput’ in state of Perlis explored in Koperasi Rimba Mas Padang Besar Quarry while Ipoh dolomite is a dolomitic limestone provided by Ipoh Seramic Sdn. Bhd.. Perlis is one of the major producers of dolomite in Malaysia that content large deposit of high purity dolomite [CaMg(CO3)2]. In this paper, the morphology of both dolomite surface and chemical composition was studied by using Scanning Electron Microscope (SEM) which is equipped with an Energy Dispersive Spectroscopy (EDS) from JEOL model JSM-6460LA. The fracture morphology of both dolomites showed brittle behavior with elongated and irregular grains embedded on the surface. The chemical composition in EDS technique show Perlis dolomite do not decomposed such as Ipoh dolomite after heating stage at 800 °C.en_US
dc.language.isoenen_US
dc.publisherKolej Universiti Sains dan Teknologi Malaysia (KUSTEM)en_US
dc.relation.ispartofseriesThe 15th Scientific Conference of Electron Microscopy Society of Malaysia (EM 2006)en_US
dc.subjectDolomiteen_US
dc.subjectDolomite rock -- Perlisen_US
dc.subjectSEM-EDSen_US
dc.subjectBatu Reputen_US
dc.subjectMines and mineral resources -- Perlisen_US
dc.titleComparison between Perlis and Ipoh dolomite under heating condition by using SEM-EDSen_US
dc.typeWorking Paperen_US


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