混杂沉积物
外观
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混杂沉积物(英语:Diamicton)是一种由未淘选或低淘选度的陆源沉积物组成,其颗粒大小差距很大,从粘土到巨砾,基质为泥岩或砂岩[1][2][3] 该地质名词由 Richard Foster Flint 和其他人创造的,作为一个纯粹的描述性名词,并没有提及任何该名词的起源或沉积环境[4]。地质学家通用这名词于未分选的冰碛石,但其他地质作用亦能造成,例如泥流,山体滑坡,浊积流等. [2][3]。
参考文献
[编辑]- ^ 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.