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泥屑灰岩

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泥屑灰岩(英語:calcilutite[1]是一種石灰岩,主要由超過50%的粉砂黏土顆粒的碎屑碳酸鹽顆粒組成。這些顆粒由沙粒大小的珊瑚、貝殼、鮞粒、石灰岩白雲石的碎片組合組成。此一詞最初由Grabau[2][3]於1903年提出,作為碎屑石碳酸鹽分類系統的一部分[4][5]。泥屑灰岩可以在各種海洋和非海洋環境中堆積, 包括、海灘、近海沙壩淺灘濁積岩[6]

參考文獻

  1. ^ Belt, Edward (November 1967). "Sedimentology of Carboniferous Cementstone Facies, British Isles and Eastern Canada". The Journal of Geology. 75 (6): 711–721. doi:10.1086/627295. JSTOR 30061239.
  2. ^ Grabau, A.W. (1903) Paleozoic coral reefs. Geological Society of America Bulletin. vol. 14, pp. 337-352.
  3. ^ Grabau, A.W. (1904) On the classification of sedimentary rocks. American Geologist. vol. 33, pp. 228-247.
  4. ^ Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, J.A., eds. (2005) Glossary of Geology (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. ISBN 0-922152-76-4
  5. ^ Scholle, P.A., D.G. Bebout, and C.H. Moore (1983) Carbonate Depositional Environments. Memoir no. 33. Tulsa, Oklahoma, American Association of Petroleum Geologists. 708 pp. ISBN 978-0-89181-310-1
  6. ^ Flügel, E. (2010) Microfacies of Carbonate Rocks, 2nd ed. Springer-Verlag Berlin, Germany. 976 pp. ISBN 978-3-540-22016-9