赣东北万年地区万年群的建立及其意义

吴新华,楼法生,刘春根,赵炼忠. 赣东北万年地区万年群的建立及其意义[J]. 地质通报, 2005, 24(9): 819-825.
引用本文: 吴新华,楼法生,刘春根,赵炼忠. 赣东北万年地区万年群的建立及其意义[J]. 地质通报, 2005, 24(9): 819-825.
WU Xinhua1,LOU Fasheng1,LIU Chungen1,ZHAO Lianzhong2 1. Jiangxi Institute of Geological Survey,Xiangtang 330201,Nanchang,Jiangxi,China, 2. Western Jiangxi Geological Survey Party,Jiangxi Bureau of Geology and Mineral Exploration and Development,Xiangtang,330201,Nanchang,Jiangxi,China. Establishment of the Wannian Group in the Wannian area,northeastern Jiangxi, China and its significance.[J]. Geological Bulletin of China, 2005, 24(9): 819-825.
Citation: WU Xinhua1,LOU Fasheng1,LIU Chungen1,ZHAO Lianzhong2 1. Jiangxi Institute of Geological Survey,Xiangtang 330201,Nanchang,Jiangxi,China, 2. Western Jiangxi Geological Survey Party,Jiangxi Bureau of Geology and Mineral Exploration and Development,Xiangtang,330201,Nanchang,Jiangxi,China. Establishment of the Wannian Group in the Wannian area,northeastern Jiangxi, China and its significance.[J]. Geological Bulletin of China, 2005, 24(9): 819-825.

赣东北万年地区万年群的建立及其意义

  • 万年群是发育在江南复合混杂岩带中之赣东北进贤—万年地区的一套中元古代蓟县纪浅变质岩系。据其岩性组合、沉积环境等特征自下而上进一步划分为枫树岭组、牛头岭组、皮库组和程源组,岩石地球化学特征反映其大地构造环境为大陆岛弧—弧后盆地,其层位与弧后盆地之双桥山群安乐林组、修水组,溪口岩群,火山岛弧的双溪坞群和弧间盆地的张村群相当,但岩性组合差异甚大,属同时异相的产物。万年群的建立为华南中元古代地层的划分对比提供了新的思路。
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出版历程
修回日期:  2004-10-27
刊出日期:  2005-09-15

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