WEATHERING CRUST OF CARBONATE ROCKS AND ITS PROCESS OF RESIDUAL SOIL FORMATION

Li JingyangGuizhou Institute of TechnologyPRC. WEATHERING CRUST OF CARBONATE ROCKS AND ITS PROCESS OF RESIDUAL SOIL FORMATION[J]. 中国岩溶, 1992, (S1): 0-0.
引用本文: Li JingyangGuizhou Institute of TechnologyPRC. WEATHERING CRUST OF CARBONATE ROCKS AND ITS PROCESS OF RESIDUAL SOIL FORMATION[J]. 中国岩溶, 1992, (S1): 0-0.

WEATHERING CRUST OF CARBONATE ROCKS AND ITS PROCESS OF RESIDUAL SOIL FORMATION

  • Weathering crust of carbonate rocks refers to the terra rossa formation, which is derived from limestone, dolomite and transitional rocks between the two. Terra rossa is widespread in the tropical and subtropical areas over the world. It is also well distributed in southern China, such as Yunnan. Guizhou Sichuan, Hunan, Guangxi and other provinces. Its thickness is generally 7-8 m
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刊出日期:  1992-12-01

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