| 黑龙江省嘉荫县平顶山金矿控矿构造及找矿方向 |
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| 引用本文： | 徐国彬.黑龙江省嘉荫县平顶山金矿控矿构造及找矿方向[J].黄金地质,1995,1(2):26-29. |
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| 作者姓名： | 徐国彬 |
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| 作者单位： | 黄金第五支队!黑龙江林口，157600 |
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| 摘 要： | 平顶山金矿属中低温热液蚀变岩－石英脉型金矿，在空间上与元古宙变质岩基底，花岗闪长岩及闪长玢岩，细晶闪长岩紧密伴生，矿体严格受ＮＮＥ向断裂构造控制，控矿断裂构造在成矿阶段的应力处于张扭状态，有利于矿液的充填，沉淀，并指出该区ＮＮＥ向断裂，特别是Ｆ０断裂的下盘应为进一步工作动向。
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| 关 键 词： | 金矿床 控矿构造 断裂构造 热液成矿 找矿方向 |
ORE-CONTROLLING STRUCTURES AND PROSPECTING GUIDES IN PINGDINGSHAN GOLD DEPOSIT, JIAYIN, HEILONGJIANG |
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| Xu Guobin.ORE-CONTROLLING STRUCTURES AND PROSPECTING GUIDES IN PINGDINGSHAN GOLD DEPOSIT, JIAYIN, HEILONGJIANG[J].Gold Geology,1995,1(2):26-29. |
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| Authors: | Xu Guobin |
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| Abstract: | Pingdingshan gold deposit is a low-middle temperature hydrothermal altered rock-quartzvein type one, is spatially closely associated with the basement of Proterozoic metamorphics,granodiorite, diorite-porphyrlte and luciite. The. orebody is strictly controlled by NNEfaulted structures. The stress of ore-controlling faulted structure is in a tenso-shhear stateduring the metallogenic stage, which is favorable for the infilling and precipitation of oresolution- NNE faults, especially the lower wall of F0 fault, are pointed out to be targets forfurther prospecting in this district. |
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| Keywords: | Heilongjiang gold deposit ore-controlling structure faulted structure hydrothermal deposit prospecting guide |
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