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south-central jiangxi
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  赣中南地区
     Qingbaikouan strata are well developed and widespread in south-central Jiangxi. They belong to the Guangxi-Hunan-Jiangxi stratigraphic subregion of the Southeast stratigraphic region.
     赣中南地区青白口纪地层发育,出露面积广泛,属东南地层区桂湘赣地层分区。
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     Stratigraphic division and correlation of Qingbaikouan strata in south-central Jiangxi
     赣中南青白口纪地层划分与对比
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     Memories of the South
     忆江南
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     North and south
     专业面粉市场:南强北弱 “金像杯”面包烘焙大赛侧记
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     The Precious Pearl-South Pearl
     珠中极品——南洋珠
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The Lower Carboniferous is one of the main coal--bearing strata in southernChina, widely exposed in Hunan, Guangxi, Guangdong, Guizhou, Yunnan, Xizang(Tibet), Jiangxi, Zhejiang, Fujian, Jiangsu, Anhui and Hubei. On the basis of thehorizon of the coal--bearing strata, coal formation involves four coal--forming peri-ods (see Table 1). According to different coal-forming periods, coal--bearing natu-res, coal beds of commercial value and the number of coal layers, southern Chinamay be divided into eight coal--accumulating...

The Lower Carboniferous is one of the main coal--bearing strata in southernChina, widely exposed in Hunan, Guangxi, Guangdong, Guizhou, Yunnan, Xizang(Tibet), Jiangxi, Zhejiang, Fujian, Jiangsu, Anhui and Hubei. On the basis of thehorizon of the coal--bearing strata, coal formation involves four coal--forming peri-ods (see Table 1). According to different coal-forming periods, coal--bearing natu-res, coal beds of commercial value and the number of coal layers, southern Chinamay be divided into eight coal--accumulating regions: the south--central Hunancoal--forming region, the northern Guangdong coal--forming region, the northernGuangxi coal-forming region,the southern Guizhou coal-forming region,the easternYunnan coal--forming region, the eastern Xizang coal-forming region, the easternGuangdong coal-forming region, and the south-central Jiangxi coal--forming region(see Table 1 and Fig.1).

华南下石炭统为中国南部地区的主要含煤地层之一。据其聚煤期的先后、含煤性及其工业可采煤层等不同因素,划分为Ⅰ、Ⅱ、Ⅲ、Ⅳ和Ⅴ聚煤期及8个聚煤区,并对有关存在争议地层的时空关系和化石带作了阐明。

The Yihuang area lies in the contact zone between the low grade metamorphic series of south central Jiangxi and the medium and high grade metamorphic series of Wuyi. 1∶50 000 regional survey has confirmed that the two metamorphic series have the same protolith formation and deformational history. Their metamorphism is characterized by “gradational transition in space and progressive evolution in time”, implying the entire process of the Caledonian orogeny from generation→development→elimination.

宜黄地区是赣中南浅变质岩系与武夷中深变质岩系的接触地带,1∶5万区调证实,两套变质岩系具有相同的原岩建造和变形历史,其变质作用具“空间上渐变过渡,时间上渐进演化”之特点,反映了加里东期造山作用的发生→发展→消亡的全过程。

Based on new data from regional survey and scientific research in the recent time, the metamorphic basement of Jiangxi is divisible into the Jiangnan type (North Jiangxi), the mixed type (Central Jiangxi) and the South China type (South-Central Jiangxi); while the sequences and ages of the metamorphosed strata are divided and correlated in this paper.

根据近期区调、科研的新资料,将江西省北、中、中南部的变质基底划分为江南型、混杂型和华南型三类,并对变质地层层序与时代进行了划分对比。

 
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