铜录山古铜矿开采遗址存在于大理岩与花岗岩接触带中的风化土中。
Ancient exploited traces of Tonglushan ancient copper mine occur in weathered soil of contact metamorphic zones between granite and marble.
下岩带和过渡带的古铜辉岩可与斯蒂尔·沃特杂岩的基底岩带相比。
The lower zone and the bronzite of the transition zone may be compared with the basal zone of the still-water complex.
下岩带和过渡带的古铜辉岩可与斯蒂尔·沃特杂岩的基底岩带相比。
The lower zone and the bronzite of the transition zone may be compared with the basal zone of the still-water complex.
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