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(Article of periodic en Chinois - 1984)

Document title


Features and geneses of the diamicton in the Lushan Region. (Inconnue)

Authors(s) and Affiliation(s)

ZHANG Lin-yuan ; MU Yun-zhi ;

Abstract

Based on an examination of the characteristics of the diamictons of this low latitude mountain region it is suggested that they are not of glacial origin although they cannot be explained by any single non-glacial process. The Dagu diamicton (corresponding to Mindel glaciation) which was said to be typical morain debris is really a sediment of piedmont fan. Its main features can be explained by the mechanism of debris-mud flow accumulation. (TNC).

Source

Article of periodic

published at : Scienta geographica sinica Changchun, Jilin

Editor :

Millesime : 1984, vol. 4, no2 [pp. 167-176]

Language

Chinois

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