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- W2371271724 abstract "Shanxi bauxite, a paleresiduum or paleresiduum R E bauxite, is aggraded-sedimentated on the carbonate tableland of North China which is weathered over a long period. The mantle of original rock is the base carbonate rock and transition rock. The formation of residuum is a floating process from south to north latitude through the equator after bulge of the tableland, but the original formation of gibbstite may be nearby 10°N, which is the paleolatitude that the carboniferous period land block of Shanxi is relatively detained. The annual average temperature is 32.4～33.1℃ in the process of the formation of the suberustal, which is counted by oxyhydrogen isotope. It belongs among tropical-subtropical climate." @default.
- W2371271724 created "2016-06-24" @default.
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- W2371271724 date "2002-01-01" @default.
- W2371271724 modified "2023-09-25" @default.
- W2371271724 title "Discussion on ore-forming factors of Shanxi bauxite" @default.
- W2371271724 hasPublicationYear "2002" @default.
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