摘要
本文对江西省的地壳演化问题有了新的认识。提出前加里东期扬子板块与华南板块地壳演化的不均一性;加里东期—印支期扬子板块与华南板块接合和加里东褶皱带,以及燕山期江西地壳演化发展新阶段等看法。
This paper deals with the basic features of the pre-Caledonian, CaledonianIndosinian and Yanshanian crusal tectonic evolution of Jiangxi Province. The author considers that in the pre-Caledonian the crustal tectonic evolutions were different in the yangtze region, the Cathaysian region and the Hunan-Jiangxi-Guangdong region. The author discusses in detail the convergence between the yangtze plate and the South China plate the formation of the Caledonian fold belt. It is believed that the convergence between the two plates was completee in the Indosinian.
出处
《中国区域地质》
CSCD
1991年第3期229-233,共5页
Regional Geology of China
