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Clay deposit of Muaraenim Formation in Ogan Komering Ulu Selatan Regency is found as overburden on top of coal seam, and as interburden among two coal seams. Ranau Formation consists of rhyolitic tuff, pumice tuff, and tuff intercalation with carbonize claystone. Early result through high temperature combustion at 1,400°C shows that clay from Muaraenim Formation in study area can be utilized as stoneware ceramic body, while diagenetic feldspar (feldsphatic tuff) can be utilized as fusion material (flux) for ceramic body in the combustion process. Tile prototype analysis with composition ratio of clay and diagenetic feldspar (feldsphatic tuff) 1 : 1 shows that within combustion temperature 1,150°C, it can produce grade II of glazing ceramic tile based on stoneware body. This abundant clay and felsdpar resources can be utilized and developed for ready-made alternative raw material in ceramic industry.

buletin sumber daya geologi/buletin sumber daya geologi

PROSPEK PEMANFAATAN LEMPUNG FORMASI MUARAENIM DAN TUF FORMASI RANAU SEBAGAI BAHAN BAKU KERAMIK DI KABUPATEN OGAN KOMERING ULU SELATAN, PROVINSI SUMATERA SELATAN