TIMES AND CAUSE OF FORMATION OF SAND-DUNE IN MIDDLE REACHES OF THE YANGTZE RIVER

YANG Chao; HUANG Chang-sheng; LI Chang-an; ZHAO Xin

Volume 9 Issue 2

Jun. 2003

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YANG Chao, HUANG Chang-sheng, LI Chang-an, et al., 2003. TIMES AND CAUSE OF FORMATION OF SAND-DUNE IN MIDDLE REACHES OF THE YANGTZE RIVER. Journal of Geomechanics, 9 (2): 176-182.

Citation:

YANG Chao, HUANG Chang-sheng, LI Chang-an, et al., 2003. TIMES AND CAUSE OF FORMATION OF SAND-DUNE IN MIDDLE REACHES OF THE YANGTZE RIVER. Journal of Geomechanics, 9 (2): 176-182.

Citation:

YANG Chao, HUANG Chang-sheng, LI Chang-an, et al., 2003. TIMES AND CAUSE OF FORMATION OF SAND-DUNE IN MIDDLE REACHES OF THE YANGTZE RIVER. Journal of Geomechanics, 9 (2): 176-182.

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TIMES AND CAUSE OF FORMATION OF SAND-DUNE IN MIDDLE REACHES OF THE YANGTZE RIVER

1. Faculty of Earth Science, China University of Geosciences, Wuhan 430074;
2. The main monitoring office of environmental geology in Jiangxi province, Nanchang 330000, China

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Received: 2003-03-27
Published:

Abstract

Abstract

By field research,data analysis and experiment data test as wall as comparing with other studys,we determined the aeolic feature of the sand-dune in the middle reaches of the Yangtze River. It is the first time in discovering the profile of Paleoburial sand-dune in Liangjiadu near Wuchang and corroborating sedimentary of sand-layer in Qingshan of Wuchang and in Yueyang of Hunan province.The time and aeolic micro-feature of sand-dune are also proofed by chronometry and scanning electron microscope.
- sand-dune,
- the middle reaches of Yangtze river,
- scanning electron microscope,
- late Pleistocene