东华理工大学地球科学学院
Published:2015
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[1]钟志菲.华南地区燕山晚期岩浆活动与成矿作用研究进展[J].能源研究与管理,2015(01):15-18.
钟志菲. Magmatic Process and Metallization of Yanshanian in South China[J]. 2015, (1): 15-18.
[1]钟志菲.华南地区燕山晚期岩浆活动与成矿作用研究进展[J].能源研究与管理,2015(01):15-18. DOI: 10.16056/j.1005-7676.2015.01.005.
钟志菲. Magmatic Process and Metallization of Yanshanian in South China[J]. 2015, (1): 15-18. DOI: 10.16056/j.1005-7676.2015.01.005.
燕山期是中国最重要最为强烈的岩浆活动期
通过总结前人对华南地区燕山晚期的研究
发现其岩浆活动可分为2个时间段
晚燕山早期的岩浆活动主要集中分布在长江中下游地区与东南沿海地区
晚燕山晚期岩浆活动主要集中在武夷山以西地区。通过SiO2-Alk图解与AFM图解以及Sr、Nd、Pb同位素对岩石类型与来源进行划分
并根据燕山晚期岩浆活动的规律与燕山晚期成矿建立关系。
Yanshanian is the most important and intense magmatic activities in China. In this paper
through summarizing predecessors’ research on southern China in the late yanshan
found that the magmatic activity can be divided into two periods
the early late yanshan magma activity mainly distributed in the middle and lower reaches of the Yangtze river region and the southeast coastal area
late late yanshanian magmatic activity mainly concentrated in the west of wuyi mountain area.Through the SiO 2-Alk graphic and AFM diagrams and Sr
Nd
Pb isotopes of source rock type and classification
and according to the law of the late yanshanian magmatic activity and the late yanshan metallogenic relationship building.
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