摘要
远在十九世纪晚年和二十世纪初叶,以德国学者李希霍芬和美国学者维理士为首的外国地质工作者,即曾对中国的地质构造进行初步分析和研究,发表了在当时被认为水平很高的总结性论文。由于所掌握的资料极度贫乏,他们的结论和推论,纵然对后来的工作有一定的参考价值,但是今天看来许多结论是笼统的,片面的,甚至错误的。
Ⅰ.Geotectonic Subdivisions of China and their Main Characteristics China is subdivided into:The Chinese Platform Northeastern Paraplatform Sino-Korean Paraplatform Yangtze Paraplatform South China Paraplatform Western folded regions Tienshan-Mongolian Fold-System Altai Fold-System Tienshan Fold-System Inner-Mongolian-Great Khingan Fold-System Tarim Massif Kunluen-Tsinling Fold-System Kunluen Fold-System Nanshan Fold-System Tsinling Fold-System Sungpan-Kantze Fold-System Tibet-W.Yunnan Paraplatform Tibetan Paraplatform W.Yunnan Fold-Fracture System Himalayan Fold-System Taiwan Fold-System 1.The Sino-Korean Paraplatform Consists of a more or less well-consolidated Pre-Sinian crystalline foundation and amoderately disturbed blanket partly of marine Paleozoic and partly of continental Mesozoic sediments.
作者
黄汲清
T.K.HUANG(Geological Institute,Ministry of Geology)
出处
《地质学报》
1960年第1期1-37,135,共38页
Acta Geologica Sinica
