主控矿构造为寨子湾韧- 脆性剪切构造带。
The main ore-controlling structure is Zaiziwan brittle-ductile shear zone.
郯庐韧—脆性剪切带是主要的导矿构造，其次级断裂是主要容矿场所。
The Tanlu ductile brittle shear zone is the major structure as passageway for ore fluid and its secondary faults are the main host.
进一步找矿方向应为深大断裂两侧及韧(脆)性剪切带。
The further prospecting directions should be in two sides of deep fracture and ductile (brittle) shear zones.
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