麻山群和黑龙江群是佳木斯地块前寒武纪基底的重要组成。
The Mashan group and Heilongjiang group are major components of the base of Precambrian Jiamusi block.
利用MT资料研究位于佳木斯地块和兴凯地块之间过渡地带的岩石圈结构特征。
The characters of the lithosphere structure is studied by using the data of the MT in the transition zone between Jiamusi massif and Xingkai massif.
运用超低密度地球化学调查方法，对佳木斯地块北缘乌拉嘎金地球化学块体的金矿资源潜力进行了预测。
We forecasted potential of gold mine resource in Wulaga Au geochemical block in the north of Jiamusi block by using the method of ultra-low density geochemical survey.
佳木斯地块西缘金矿带是受深断裂控制的，矿床之间是相互联系的，是在一个构造应力体制下完成它们的成矿作用的。
Auriferous belt at western margin of Kiamusze massif is controlled by deep rupture, depositions are correlative. The auriferous belt 's mineralization is finished under same tectonic stress system.
佳木斯地块西缘金矿带是受深断裂控制的，矿床之间是相互联系的，是在一个构造应力体制下完成它们的成矿作用的。
Auriferous belt at western margin of Kiamusze massif is controlled by deep rupture, depositions are correlative. The auriferous belt 's mineralization is finished under same tectonic stress system.
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