| 论华南红色风化壳 |
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| 引用本文： | 席承藩.论华南红色风化壳[J].第四纪研究,1991,11(1):1-8. |
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| 作者姓名： | 席承藩 |
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| 作者单位： | 中国科学院南京土壤研究所 |
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| 摘 要： | 本文论述了我国南方广泛分布的富含铁铝氧化物的红色粘土的成因、分布及其所形成的土壤,并论述了第四纪红色风化壳的时代划分问题。
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| 关 键 词： | 红色风化壳 脱硅富铁铝风化 红色风化壳的时代划分 网纹红土 |
ON THE RED WEATHERING CRUSTS OF SOUTHERN CHINA |
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| Institution: | Nanjing Institute of Soil Science, Chinese Academy of Sciences |
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| Abstract: | Red clay materials formed by chemical weathering under wet tropical and subtropicalconditiins are widely distributed in Southern China,south of Yangtze River.They are formedby leaching away of alkaline and alkaline earth ions accompanied with moving out of silicaions from the bed rocks and weathering crust.Under the rainforests,seasonal rainforests and broadleaf forests,various ferrallitic soilssuch as latosols,latosolic red earths,red earths and yellow earths are formed.The present paper discusses the stratification of Quaternary.It is considered that thematerials of red clay mixed with round gravels and pebbles are the lower Pleistocene （Q1）.While the thick plinthic red clay beds are the middle Pleistocene （Q2） and the homogeneousred clay with four layers are upper Pleistocene （Q3）.The red coloured weathering surfaceon the thick gray sands are the result of the early Holocene.Station observation shows thatthe desilicification and ferrallitic weathering are still going on. |
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