Summary if silica sand deposits in Sarawak Azemi Eki, George Peter Meran.
Material type:
TextPublisher: 1992Description: viii, 71 p. ill., maps 30 cmSubject(s): Hydrology -- Sarawak | Geology -- Sarawak | Topography -- Sarawak | Sand -- Sarawak | Sediments (Geology) -- Sarawak | Bintulu (Sarawak)Summary: Silica (Si 02) is one of the commorest material in the earth's crust. Mineralogically it occurs maily as quartz, which in its promary form is found as diseeminted grains in both igneous and metamorphic rocks such as granite or quartzite, and in sedimentary rocks such as sendtone.
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Silica (Si 02) is one of the commorest material in the earth's crust. Mineralogically it occurs maily as quartz, which in its promary form is found as diseeminted grains in both igneous and metamorphic rocks such as granite or quartzite, and in sedimentary rocks such as sendtone.
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