矿体的分布受侵位后的脆性剪切带控制。
六批叶矿区大架金矿床与韧-脆性剪切带密切相关。
The Dajia gold deposit of Liupiye ore district is closely related to the ductile-brittle shear belt.
湘西沃溪断裂为一具走向剪切滑移性质的脆性剪切带。
The Woxl-fault in western Hunan is a brittle shear zone characterized by shearing—sliding along its strike.
矿床受控于由阿尔金大断裂派生的北西向韧脆性剪切带中。
The deposit is controlled in NW-trending shear zone derived by Altyn fault.
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.
中酸性火山岩是本区主要成矿母岩，韧-脆性剪切带是金矿形成的重要导矿构造。
There is a closely retationship between the formation of gold deposit and the tectonics, stratigraphy, petrological character, intrusive rocks, Uolcanic rocks and ductile shear zone.
东准噶尔双泉一带的韧-脆性剪切带是在板块结合带基础上，形成于陆-陆碰撞体制。
Basing on the combination of plates, ductile-brittle shear zone in the ShuangQuan area, Eastern JungGar forms in the system of continental - continental collision.
北部控矿韧脆性剪切带是区域韧性剪切带演化的产物，以左行剪切为主，位于铁夹树—庙湾北部厚层灰岩的下部。
The North ore-controlling ductile-brittle shear zone, which is the production of the evolution of the regional ductile zone, is located at the bottom of Tiejiashu-Miaowan thick-bedded limestone.
文章从成矿地质条件、矿床地质特征等入手，分析了矿床的控矿因素，认为该矿床受含矿地层、韧脆性剪切带构造、岩浆岩等因素的制约。
Based on ore-forming condition and ore geology, ore-controlling factors are analyzed. It is suggested that the deposit is controlled by ore-hosting strata, ductile-brittle shear zone and magmatism.
韧性剪切带型金矿床中金主要富集在应变最强部位和韧性向脆性转换的部位。关键词：沂沭断裂带；龙泉站金矿；
The places of gold ore are mainly in the powerfulness place and in the place which is from toughness to brittleness conversion.
金矿床严格受剪切构造带的控制，金矿体一般赋存于韧—脆性构造和构造扩容带中。
The gold deposit is totally controlled by shear structures and is formed in the ductile brittle structures and structural extension zone.
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.
样品变形处于半脆性域，以出现非破裂的准韧性剪切带为特征。
Optical micrographs of deformed samples show that different scales of semi brittle ductile shear zones (SBDSZ) occur with different strains.
燕山期，该构造带以韧脆性-脆性断裂变形为主，在早期韧性剪切变形的基础上叠加一系列同方向的高角度压性-压扭性逆冲断裂。
In Ysashanian stage, it was characterized by ductile brittle and brittle faulting and formed a series of east west trending high Angle thrust faults superposed on the early mylonite zones.
韧性剪切带形成以后，区内主要经历了热蚀变和脆性变形，韧性变形很弱。
After the formation of ductile shear zones, there is no strong ductile shear deformation in the region, except some thermal alterations and brittle deformation.
金矿化的构造控制作用主要体现为剪切带的动力作用和脆性断裂作用两方面。
The structural controlling in mineralization mainly results from driving force in shear zone and fracturing.
两组断裂均为长期多次活动断裂，早期活动具强烈韧性变形特征，晚期在韧性剪切带基础上再叠加脆性断裂。
Two sets of fault are all long-lived faults. They exhibited sharply ductile deformation in early activities and superimposed brittle deformation in later activities.
两组断裂均为长期多次活动断裂，早期活动具强烈韧性变形特征，晚期在韧性剪切带基础上再叠加脆性断裂。
Two sets of fault are all long-lived faults. They exhibited sharply ductile deformation in early activities and superimposed brittle deformation in later activities.
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