CAJ | 학술논문

赣北大湖塘钨矿田大地构造位置位于扬子陆块区‐下扬子陆块‐江南古岛弧的中北部，其北临幕阜山（鄂东）被动边缘盆地，南接宣春断陷盆地。区域出露有中元古代、新元古代、古生代和中生代地层，其中以中元古代地层最发育，新元古代、古生代、中生代地层零星出露。区内经历了多次构造活动，其中晋宁运动、印支运动和燕山运动最为醒目，表现为强烈的褶皱和断裂广泛发育。
공북대호당오광전대지구조위치위우양자륙괴구‐하양자륙괴‐강남고도호적중북부，기북림막부산（악동）피동변연분지，남접선춘단함분지。구역출로유중원고대、신원고대、고생대화중생대지층，기중이중원고대지층최발육，신원고대、고생대、중생대지층령성출로。구내경력료다차구조활동，기중진저운동、인지운동화연산운동최위성목，표현위강렬적습추화단렬엄범발육。
Dahutang tungsten ore field in north of Jiangxi province is located in the Yangtze continental block‐of‐lower Yangtze Jiangnan Proterozoic in the Northern ,mufu mountain in the North (Hubei Province) ,passive margin basins ,Xuan Chun rift basin in the South .Regional outcropping Proterozoic , neoproterozoic and Paleozoic and Mesozoic strata ,with middle Proterozoic strata are most developed , neoproterozoic ,Paleozoic ,Mesozoic strata scattered outcrops .Has experienced a number of tectonic activity in the district ,jinning movement ,Indo‐China yanshanian movement in sport and the most eye‐catching , characterized by widely developed strong folds and faults .