Material Analysis Supporting Cement Industry Muara Dua Area South Oku Regency South Sumatera
DOI:
https://doi.org/10.33536/jg.v8i01.1386Keywords:
Carbonate, XRF, Trass, Packstone, WackstoneAbstract
Material cement industry are mostly formed by carbonate and silica. Mineralogy of carbonate mostly formed by Calcium (Ca) contained on Calcite (CaCO3), Dolomite (CaMg(CO3)2) while Silica, Alumina, Iron Oxide element found as SiO2, Al2O3, Fe2O3, MgO on rock. Identification of the spread of this material on the surface is expected to provide accurate information for the implementation of further exploration activities. Three analysis method were conducted which are Surface Geological Mapping to describe macro petrology, Petrography analysis to determine mineralogy microscopic and Geochemical method using XRF to identified chemical mineralogy of rock. Research area mostly generated by tectonically complex where the sedimentation mostly controlled the existence of material using in cement industry Limestone is carbonate lithology unit that develop on research area where known as Packstone to Wackestone (Petrography) while "Calcitic Limestone” to “Marly Limestone” classification from Geochemical analysis (XRF). Another material such as Silica and trass material are also found on this research area to support cement industry.
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References
Agnello, VN. 2005. Dolomite and Limestone in South Africa. Supply and Demand. Directorate Mineral Economics. Pretoria. Africa.
Budding, Antonius J. and F, Rolland. 1977. Petrographic Description of This Sections of Drill Cuttings from KCM No.1 Forrest Federal Well. Soccorro, New Mexico.
Dietrih, V. and Schwandner, F. 2000. Preparation of glass beads and powder pills for XRF Analysis of silicic and calcareous rocks. Institute of Mineralogy and Petrography. Swiss.
Darman, H. and Sidi, F.H. (2000) an Outline of the Geology of Indonesia. Indonesian Association of Geologists (IAGI). Jakarta, 192 p.
Goldsmith J. R. and Heard H. C. (1961). Subsolidus phase relations in the system CaCO3-MgCO3. J. Geol., 69:45–74.
Goldsmith J. R. and Newton R. C. (1969). P-T-X relations in the system CaCO3-MgCO3 at high temperatures and pressures. Amer. Jour. Sci., 267A:160–190.
Hill, Carrol A and Schluter, Cristian M. June 1993. Petrographic Description of Calcite/Opal Samples Collection on Field Trip of December 5-9 1992. Special Report submitted to the Nuclear Waste Project Office. State of Nevada.
Hinrichsen T, and Schurmann K. (1971). Synthese und stabilita¨t von glimmern im System CaONa2O-Al2O3-SiO2-H2O. Forschr. Mineral.
Japanese Industrial Standard Committee. 1992. Japanese Industrial Standard JIS. Particulate Materials – General Rules for Methods of Sampling JIS M 8100. Japanese Standard Association, 1-24. Akasaka 4. Minatoku. Tokyo 107. Japan.
Katz A. and Matthews A. (1977). The dolomitization of CaCO3: An experimental study at 252–295°C. Geochim. Cosmochim. Acta.
Ottonello Giulio.1997. Principles of Geochemistry. Columbia University Press. New York Chichester, West Sussex.
Ozkan, A. Mudjat and Dinc, Salih. 2011. Petrographic Characteristics of the Hacialabaz Formation Dolomites (Upper Jurassic) In The Bagbasi Area, Turkey.
Pan African Capital PLC-Industry Report. April 2011. Nigerian Cement Industry a Review of Opportunities and Recurrent Price Hike, Adeola Odeku, Victoria Island, Lagos.
Van Kranak P. 1974. Petrography and Geochemistry of Butterly Dolomite and Associated Sphalerite Mineralization Turner Prospect. Arbuckle Mountain Ocklahoma. University of Washington. Washington.
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