磨拉岩

磨拉岩（英語：）是指在上升山脈前形成陸相碎屑沉積物。磨拉岩和造山運動有關，通常聚集在前陸盆地，碎屑物顆粒的變化，一般反應造山運動的强烈[1][2]。

參考文獻
  1. Stanley, Steven M., Earth System History, New York: W.H. Freeman and Company, 1999, p.243 ISBN 0-7167-2882-6
  2. Tenchov, Yanaki G. (1989) "Demarcation of Molasse from Non-molasse sediments" Zeitschrift für geologische Wissenschaften 17(8): pp. 791–796
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