断裂破碎带形成的构造空间，对湖北内生金矿具有重要控制作用。
The structural Spaces resulting from the faulted fracture zones significantly control the endogenetic gold deposits in Hubei province.
柿树底金矿床赋存于中元古界熊耳群安山岩中，矿体受断裂破碎带控制。
The Shishudi gold deposits is located in Mesoproterozoic Xiong 'er Group Anshan Ore.
矿床受近南北向断裂构造控制，矿体以脉状、透镜状、豆芽状赋存于这些断裂破碎带中。
Mineral deposit controlled by north and south faulted structure, mineral body exist in faulted structure with lenticular style, vein style and sprouted style.
冷水北沟铅锌矿赋存于元古界栾川群和管道口群地层中，矿体受断裂破碎带及矽卡岩带控制。
The Lenshuibeigou lead-zinc deposit occurs in Proterozoic Luanchuan group and Guandaokou group formation and is controlled by faulted and fractured zone and skarn zone.
不论岩浆成因还是构造成因，金矿体均受断裂破碎带、断层带或片理化带等构造带控制，产于大断裂带旁侧。
Whether magma reason or structure reason, the gold mine is all controlled by fracture zone beside large fracture.
矿体受地层和构造联合控制，一般产在褶皱的层间剥离裂隙、构造裂隙及节理中，或产于褶皱翼部的断裂破碎带内。
Ore bodies are jointly controlled by both strata and structures, and usually they are distributed in folded layers' fissures, structural fissures and joints or in the broken belts of fold flanks.
层间滑动破碎带、岩体接触面和断裂构造是主要的含矿构造，它控制了矿体的形态和产状。
The main ore-bearing structure are the interlayer-gliding fracture zone, contact area of rock mass and fracture structure, which controlled the shape and the occurrence of orebody.
采用HDS-1型快速数字闪烁测氡仪，对温泉水库坝址区活动断裂（带）或破碎带以及地震鼓包等进行了氡气测试。
Using HDS-1 fast data flashing Rn measure instrument, the gas radon was measured in the active fault(zone)or broken zone and earthquake swell of the Wequan reservoir dam location.
潦河附近的F（14）断裂带是一条规模较大的含金破碎带。
Fault zone F(14) near the Liaohe River would be a significant target for gold dePOSits.
断裂构造破碎带是该地区主要控矿、容矿构造。
The fault structural fracture zone is the main ore-control, ore-bearing structure.
断裂带产生于大理岩之中，地下水沿断层破碎带运移，并对岩石进行浸蚀与溶蚀进而发育地下暗河，冲蚀加剧，最终形成今日看到的溶洞。
Flowing of underground water along faulted zones in marble eroded and corroded wall rocks and formed underground rivers, which finally created karst caves.
断裂带产生于大理岩之中，地下水沿断层破碎带运移，并对岩石进行浸蚀与溶蚀进而发育地下暗河，冲蚀加剧，最终形成今日看到的溶洞。
Flowing of underground water along faulted zones in marble eroded and corroded wall rocks and formed underground rivers, which finally created karst caves.
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