特别是构造砾岩与韧性剪切带中糜棱岩相伴生，在区域上研究划分剪切带具有一定的意义。
Especially, tectonic breccia associated with mylonitic lithofacies in tenacity shear zone, it has significance in dividing different shear zones on regional scale.
火山周边断裂规模相对较大，其内多形成构造角砾岩带，是成矿物质沉淀、富集的理想场所和最有利的容矿构造。
The fractures around the volcanic dome are rich in structural breccia belt, which is good place for the ore depositing, and became the host structure.
本文根据现代构造理论，认为修水组底部砾岩属于挤压造山作用中晚期的沉积产物。
Based on modern tectonic theory, the authors believe that this conglomerate is a product of middle-late stage sedimentation during a compressional orogeny.
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