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논문 기본 정보

자료유형
학술저널
저자정보
(Chungnam National University) (Hanil Cement) (Korea Institute of Geosciences and Mineral Resources)
저널정보
한국에너지학회 에너지공학 에너지 공학 제27권 제3호 (통권 제95호)
발행연도
수록면
48 - 56 (9page)

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초록· 키워드

The shell waste biomineralization process has known a tremendous metamorphosis and also the nanostructure with the identification of matrix proteins in oyster shells. However, proteins are represented in minor shell components and they are the major macromolecules that control biocrystal synthesis. Aragonite and calcite were derived from molluscan shells and evaluated the source of carbonate minerals and it helps for the formation of limestone. The oyster shell wastes are large and massive. The paleoecological study of oyster beds has discovered a near-shore and thin Upper Rudeis formation with storm influence during the accumulation of oysters with highly altered by disarticulation, bioerosion, and encrustation. It is possible even in the Paleozoic mollusks provided sufficient carbonate entirely to the source of microcrystalline of limestone. The present review is to discuss paleoecologically a number of oyster shell beds accumulated and sediment to form the different types of limestone during the Middle Miocene time.
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목차

  1. Abstract
  2. 1. Introduction
  3. 2. Origin of Oyster shells
  4. 3. Limestone origin
  5. 4. Conclusions
  6. References

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UCI(KEPA) : I410-ECN-0101-2019-572-000038346