淯

花园冲铜铅锌矿床受北北西向淯溪断裂带F5断层控制，含矿岩性为白垩系上统跑马岗组褪色白云质含砾次长石砂岩；

Huayuanchong copper-lead-zinc deposit is controlled by NNW F5 trending fault , while the ore-bearing lithology being Paomagang Fm fade dolomitic gravel subarkose .

随即，长宁开始了淯江河沿岸的治理工程。

Immediately , the construction project on the banks of Yujiang River began .