复理岩

复理岩（英语：Flysch）是指一系列沉积岩层，从深水和浊积流沉积物演变到浅水页岩和砂岩^[1]。复理岩由重复的沉积循环组成。每一循环有向上颗粒变细的特征。通常循环底部是砾岩或角砾岩，逐渐向上演变为砂岩和页岩/泥岩^[2]。复理岩一般形成在前陆盆地磨拉岩下部。代表盆地从深水盆地缓慢地被填满后变成陆相山麓盆地的过程^[3]

参考文献

^ Moores, Eldridge M.; Twiss, Robert J. (2000). Tectonics (3rd print ed.). New York: Freeman. pp. 265–266. ISBN 0716724375
^ Labhart, Toni P. (2005). Geologie der Schweiz [Geology of Switzerland] (in German) (7th ed.). Bern: Ott Verlag. p. 64. ISBN 3-7225-0007-9
^ Einsele, Gerhard (2000). Sedimentary Basins : Evolution, Facies, and Sediment Budget (2nd ed.). Berlin: Springer. pp. 210–211. ISBN 9783540661931

[”Moores”-1] Moores, Eldridge M.; Twiss, Robert J. (2000). Tectonics (3rd print ed.). New York: Freeman. pp. 265–266. ISBN 0716724375

[”Labhart”-2] Labhart, Toni P. (2005). Geologie der Schweiz [Geology of Switzerland] (in German) (7th ed.). Bern: Ott Verlag. p. 64. ISBN 3-7225-0007-9

[”Einsele”-3] Einsele, Gerhard (2000). Sedimentary Basins : Evolution, Facies, and Sediment Budget (2nd ed.). Berlin: Springer. pp. 210–211. ISBN 9783540661931

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