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依据不同构造岩浆区单元 ,江西中南部中新元古代 -晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。其中武夷山构造岩浆区共划分了 43个单元 ,归并为 11个超单元 ;赣西南构造岩浆区共划分为 34个单元 ,归并为10个超单元。这样较系统地建立了江西省中南部中新元古代 -晚三叠世岩石谱系单位和等级体制 ,为今后开展全省侵入岩谱系单位划分奠定了基础。
According to the different structural magmatic units, the Meso-Neoproterozoic-Late Triassic intrusions in central-southern Jiangxi can be divided into Wuyishan tectonic magma area and southwest Jiangxi tectonic magma area. Thereinto, there are 43 units in the Wuyishan tectono-magmatic area, which are combined into 11 super-units. The southwest Jiangxi structural magma area is divided into 34 units, which are combined into 10 super-units. This systematically established the Meso-Neoproterozoic-Late Triassic rock pedigree units and grading system in central-southern Jiangxi Province, which laid a foundation for the future division of the intrusive rock pedigree units in the province.