地质异常是在结构、构造或成因序次上与周围环境有着明显差异的地质体或地质体组合。
A geological anomaly is a geological body or complex of bodies with obvious different compositions, structures or orders of genesis as compared with the surrounding circumstances.
低序次断裂是地壳变形的直接产物，具有丰富的构造变形信息。
Subordinate fault is the direct production of crust deformation, It has rich information of structure deformation.
赣湘地区的变质核杂岩和变质穹窿构造中，晚期脆性断裂与早期低序次韧性构造间存在着明显的相关联系。
In the metamorphic core complex (MCC) and the metamorphic arch, Jiangxi and Hunan area, there is an obvious correlation between the late brittle fault and the early subordinate ductile structure.
低序次断裂是地壳变形的直接产物，具有丰富的构造变形信息，经过转换的低序次构造。
Subordinate fault is the direct production of crust deformation, It has rich information of structure deformation.
黄-破断裂是其主要的导矿构造，其次级低序次NNE向断裂带是主要的容矿构造。
The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host.
黄-破断裂是其主要的导矿构造，其次级低序次NNE向断裂带是主要的容矿构造。
The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host.
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