混杂沉积物
混杂沉积物(英語:Diamicton)是一種由未淘選或低淘選度的陸源沉積物組成,其顆粒大小差距很大,從粘土到巨礫,基質為泥岩或砂岩[1][2][3] 該地質名詞由 Richard Foster Flint 和其他人創造的,作為一個純粹的描述性名詞,並沒有提及任何該名詞的起源或沉積環境[4]。地質學家通用這名詞于未分選的冰碛石,但其他地質作用亦能造成,例如泥流,山体滑坡,浊积流等. [2][3]。
參考文獻
- ^ Jackson, J.A., J. Mehl, and K. Neuendorf (2005) Glossary of Geology American Geological Institute, Alexandria, Virginia. 800 pp. ISBN 0-922152-76-4
- ^ 2.0 2.1 Bennett, M.R., and N.F. Glasser (2009) Glacial Geology: Ice Sheets and Landforms, 2nd Ed. John Wiley & Sons, Ltd., New York, New York. 400 pp. ISBN 978-0470516911
- ^ 3.0 3.1 [[Tucker, M. E.]] (2003) Sedimentary Rocks in the Field John Wiley & Sons, Ltd., New York, New York. 244 pp. ISBN 978-0470851234
- ^ Flint, R.F., J.E. Sanders, and J. Rodgers (1960) Diamictite, a substitute term for symmictite Geological Society of America Bulletin. 71(12):1809–1810.