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.
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