Research on Superimposed Metallogenic System
摘要
As located in the junction of three tectonic plates (the Eurasian plate, the Indian plate and the west Pacific plate), the China continent shows complex regional metallogenic features due to tectonic evolution of micro-plates, polycycle tectonic movements. Well developed superimposed metallogenic systems have constituted one of the regional metallogenic features in China. Through the study on superimposed metallogenic system of the middle and lower reaches of the Yangtze River and of the Yuebei basin (northern Guangdong Province), the authors put forward some basic combination pattern of sedimentary-magmatic superimposed metallogenic system and summarize its forming conditions (controlling factors).
引用本文（GB/T 7714）
ZHAIYusheng, WANGJianping, DENGJun, 等. Research on Superimposed Metallogenic System[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2004.
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