Tectonic fluid inclusion is the fluid representative of thermal events in structure and is preserved in a great quantity within faulting tectonic rocks.
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。
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This paper makes a study on the tectonic stress field by insitu stress measurements using hollow inclusion technique in overcoring in Xishimon iron mine.