泥屑灰岩
泥屑灰岩（英語：calcilutite）[1]是一種石灰岩，主要由超過50%的粉砂和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、石灰岩和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、近海沙壩和淺灘、濁積岩等[6]。
參考文獻
- ^ 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.
- ^ Grabau, A.W. (1903) Paleozoic coral reefs. Geological Society of America Bulletin. vol. 14, pp. 337-352.
- ^ Grabau, A.W. (1904) On the classification of sedimentary rocks. American Geologist. vol. 33, pp. 228-247.
- ^ 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
- ^ 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
- ^ Flügel, E. (2010) Microfacies of Carbonate Rocks, 2nd ed. Springer-Verlag Berlin, Germany. 976 pp. ISBN 978-3-540-22016-9