復理岩

復理岩（英語：Flysch）是指一系列沉積岩層，從深水和濁積流沉積物演變到淺水頁岩和砂岩^[1]。復理岩由重複的沉積循環組成。每一循環有向上顆粒變細的特徵。通常循環底部是礫岩或角礫岩，逐漸向上演變為砂岩和頁岩/泥岩^[2]。復理岩一般形成在前陸盆地磨拉岩下部。代表盆地從深水盆地緩慢地被填滿後變成陸相山麓盆地的過程^[3]

參考文獻

^ 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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