平流岩

平流岩（英語：），又称等深岩，是由平流沉积物或经平流改造的原有沉积物所形成的沉积岩，常产于复理石等深水相层系中，这一地質名詞最先由Hollister和Heezen於1972年提出。[1][2]

參考文獻
  1. Hollister, C.D.; Heezen, B.C. (1972). "Geologic effects of ocean bottom-currents: western north Atlantic". In: Studies in Physical Oceanography. 2: 37–66
  2. Rebesco, M. & Camerlenghi, A. 2008. Contourites, Elsevier Science, 688pp. ISBN 978-0-444-52998-5
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