构造流体包裹体是构造热事件的流体代表,在断裂构造岩中大量保存。
Tectonic fluid inclusion is the fluid representative of thermal events in structure and is preserved in a great quantity within faulting tectonic rocks.
绍兴-江山深大断裂控制了矿田和岩株的构造。
Structures ofthe ore-field and the stock are controlled by the Shaoxing-Jiangshan deep fault.
地层、侵入岩、断裂构造是工作区内钨矿的三个基本的成矿地质条件。
The stratum, intrusive rock, and faulted structure are three basic ore-forming geology factors of tungsten ore in the work area.
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