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(Article of periodic en Anglais - 2000)

Document title

Channel characteristics and formation mechanism of Ganjiang River

Authors(s) and Affiliation(s)

CHEN ZHI-QING ;

Abstract

Relative straight channel of the middle and upper reaches of Ganjiang has been formed due to the contraction of mountains and hills being composed of bedrocks on both banks of the river. But however, at the lower reaches, branching channel predominates due to limited contracting force of the river banks as the evolution and development of branching channels are closely related with locations and controle effect of nodal points. There are sufficient water containing less sediments in particles rather coars

Source

Article of periodic

published at : The Journal of Chinese geography / ISSN 0218-1444

Editor : Guoji Translation and Publishing, Singapore - SINGAPOUR (1990- 2000)

Millesime : 2000, vol. 10, no4 [pp. 422-427]

Bibliographic references : 6 ref.

Collation : Illustration ;

Language

Anglais

Localisation

Laboratoire INTERGEO - Paris

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2001.
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