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Geology of China : ウィキペディア英語版
Geology of China
:''For other uses, see Chinese rock (disambiguation).''
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. South of the Yangzi river, most of the landscape is mountainous, dominated by sedimentary deposits and by the Yangzi craton. The most famous scenery in China is found in the karst landscapes of Guangxi and Yunnan provinces. The alluvial Sichuan basin is surrounded by mountains, the Qinling mountains to the north and the Himalaya to the west and southwest. Much of Northeast China, or Manchuria, is dominated by alluvial plains, but the border regions with Korea are also highly mountainous. In the west, most of the Tibetan plateau is in China, and averages over 4000 metres in elevation. The Yunnan-Guizhou plateau is also an extension of the Tibetan plateau.〔() Outline of Chinese Geology J. Marvin Weller (2) AAPG Bulletin Volume 28 (1944)〕
==Geoscience==
It was not until late in the Qing Dynasty (1644–1911) that the government formulated a policy to introduce foreign science and technology into China. Modern geologic ideas were introduced with the establishment of technical schools and the translation into Chinese of works by James D. Dana and Charles Lyell during the 1870s. Early in the twentieth century, foreign geology teachers were brought to China and Chinese students were sent to foreign countries to study geology. This infusion successfully developed the modern teaching and practice of geology in China.〔( A History of Geology and Geological Education in China (to 1949) )〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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