Matches in DBpedia 2016-04 for { ?s ?p "The Geology of China (中国地质, Zhōngguó dì zhì) (or the geological structure of the People's Republic of China) can be divided into several parts. The historical centre of Chinese culture is on the loess plateau, the world's largest Quaternary loess deposit, and on the alluvial lands at the east of it. The alluvial East China plain extends from just south of Beijing in the north, to the Yangzi river delta in the south, punctuated only by the igneous Shandong highlands and peninsula."@en }
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- Geology_of_China comment "The Geology of China (中国地质, Zhōngguó dì zhì) (or the geological structure of the People's Republic of China) can be divided into several parts. The historical centre of Chinese culture is on the loess plateau, the world's largest Quaternary loess deposit, and on the alluvial lands at the east of it. The alluvial East China plain extends from just south of Beijing in the north, to the Yangzi river delta in the south, punctuated only by the igneous Shandong highlands and peninsula.".
- Q5535349 comment "The Geology of China (中国地质, Zhōngguó dì zhì) (or the geological structure of the People's Republic of China) can be divided into several parts. The historical centre of Chinese culture is on the loess plateau, the world's largest Quaternary loess deposit, and on the alluvial lands at the east of it. The alluvial East China plain extends from just south of Beijing in the north, to the Yangzi river delta in the south, punctuated only by the igneous Shandong highlands and peninsula.".