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Discover how limestone, a biochemical sedimentary rock mainly of calcium carbonate, forms from marine shells. Explore the anatomy of limestone, including grains, lime mud, and cement, and learn about the factors influencing its precipitation. Find out where limestone forms and its various products and uses in construction, steel production, water treatment, and more.
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What is limestone? • Limestone = a biochemical sedimentary rock made up mostly of calcium carbonate
How do limestones form? • Most limestones are simply the cemented remains of marine shells • Limestone “anatomy” • Grains • Skeletal particles, ooids, peloids • Lime mud • Microscopic crystals produced by calcareous algae and through abrasion of larger particles • Cement • Inorganically precipitated CaCO3 crystals
Where do limestones form? • Because CaCO3 precipitates most readily in warm, well lit, agitated water of normal marine salinity…..most limestones form in shallow, tropical depositional environments • e.g., Bahamas, central America, Persian Gulf, NW shelf of Australia, Great Barrier Reef, Malaysia, Indonesia, etc.
Modern CaCO3 depositional environments *Note: Although cool water carbonates Are forming in many places, they are highly prone to dissolution and therefore do not become major limestone accumulations
Caicos Platform Reef tract Quiet water high-energy sand shoals Prevailing winds
What are limestone products? • Whole rock • Crushed limestone • Dolomitic limestone • Burned lime (calcium oxide) • High calcium lime • Dolomitic lime • Hydrated lime (calcium hydroxide)
How is limestone used? • Construction • Soil stabilization • Flue Gas Desulfurization • Steel Production (flux for blast furnaces) • Glass Production • Water Treatment • Waste Treatment • Paper Production (filler) • Chemical Production • Masonry, Mortars and Other Building Materials