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泥屑灰岩

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泥屑灰岩(英语:calcilutite[1]是一种石灰岩,主要由超过50%的粉砂黏土颗粒的碎屑碳酸盐颗粒组成。这些颗粒由沙粒大小的珊瑚、贝壳、鲕粒、石灰岩白云石的碎片组合组成。此一词最初由Grabau[2][3]于1903年提出,作为碎屑石碳酸盐分类系统的一部分[4][5]。泥屑灰岩可以在各种海洋和非海洋环境中堆积, 包括、海滩、近海沙坝浅滩浊积岩[6]

参考文献

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  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