Geochemical constraints on provenance of the mid-Pleistocene red earth sediments in subtropical China
The source of mid-Pleistocene red earth sediments in the middle to lower reaches of the Yangtze (Changjiang) River was investigated based on their geochemical characteristics. The Xuancheng and Jiujiang red earth sediments have similar major and trace element distribution patterns. Compared to the l...
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Published in | Sedimentary geology Vol. 290; pp. 97 - 108 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
15.05.2013
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Subjects | |
Online Access | Get full text |
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