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hydrothermal altered rock
相关语句
  热液蚀变岩
     On Superhigh ̄18O Hydrothermal Altered Rock and Mineral Deposti
     论特高~(18)O热液蚀变岩石与矿床
短句来源
     Original Co-deposits of Pule and Hengdong in northeast Hunan occurred in tectonic, hydrothermal, altered rock zone of the lower plate of main fracture belt F2, Changping fracture zone.
     湘东北普乐及横洞原生钴矿床均赋存于长平断裂带F2主干断裂下盘构造热液蚀变岩带中。
短句来源
  相似匹配句对
     THE KAOLIN DEPOSITS OF TYPE OF HYDROTHERMAL ALTERED TUFFS IN CHINA
     我国凝灰岩蚀变型高岭土矿床
短句来源
     Hydrothermal Eruption
     水热爆炸
短句来源
     ON HYDROTHERMAL ROCK
     关于热液岩
短句来源
     the hydrothermal alteration includs three altered stagespyritesericitization,silicification and carbonation.
     热液蚀变包括黄铁绢云岩化、硅化、碳酸盐化三个蚀变阶段。
短句来源
     On Superhigh ̄18O Hydrothermal Altered Rock and Mineral Deposti
     论特高~(18)O热液蚀变岩石与矿床
短句来源
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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...

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.

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方向。

Kangguer gold polymetallic deposit with associated copper,lead,zinc and silver,lying south of the Tu Ha basin in the eastern Tianshan Mountains,occur in the gigantic Qiugemintashi Huangshan ductile compressional belt.The formation of the deposit is closely related to the evolution of this ductile compression belt and the deposit is considered as a hydrothermal altered rock type gold deposit under the control of the ductile deformation belt. The gold deposit occurs in the intermediate acid rift volcanic...

Kangguer gold polymetallic deposit with associated copper,lead,zinc and silver,lying south of the Tu Ha basin in the eastern Tianshan Mountains,occur in the gigantic Qiugemintashi Huangshan ductile compressional belt.The formation of the deposit is closely related to the evolution of this ductile compression belt and the deposit is considered as a hydrothermal altered rock type gold deposit under the control of the ductile deformation belt. The gold deposit occurs in the intermediate acid rift volcanic rocks,was confined to the ductile compressional belt and the syntectonic pluton which formed during the orogeny as a result of the closing of the rift.The metallogenesis was synchronous with the tectono magmatic activity. A trio model comprising volcanic rocks,syntectonic pluton and normal brittle ductile shear zone in one area is proposed for the ore deposit.Volcanic rock series provided most of metallogenic material,and syntectonic pluton supplied hydrothermal fluid,thermal energy and also part of metallogenic material while the normal brittle ductile shear zone formed the ore trapping structures.“Three in one” is the necessary condition for the formation of ore deposit. The normal brittle ductile shear zone,as a late product of ductile deformation is the main target for the prospecting of ore deposits.

作者通过构造控矿分析发现,康古尔金矿是受一韧性挤压带控制的中低温岩浆-变质热液型金矿床。成矿作用与控矿韧性挤压带从韧性向脆、韧性变形演化密切相关。本文具体分析了控矿构造类型和构造演化对矿化的控制程序以及矿体定位机制,建立了构造成矿模式指出了找矿方向。

The Shanhou gold deposit is located in the middle-south of the Zhaoping fault zone. It is a clastic zone mid-low temperature hydrothermal altered rock type deposit. The mineralization is featured by multistage and multiphase superimposing. According to the theory of structural superimposed halo, the model of structural superimposed halo of the Shanhou gold deposit has been made, and deep prospecting prediction has been done for No.1-1 and No.1-2 ore body. It is regarded that the former has...

The Shanhou gold deposit is located in the middle-south of the Zhaoping fault zone. It is a clastic zone mid-low temperature hydrothermal altered rock type deposit. The mineralization is featured by multistage and multiphase superimposing. According to the theory of structural superimposed halo, the model of structural superimposed halo of the Shanhou gold deposit has been made, and deep prospecting prediction has been done for No.1-1 and No.1-2 ore body. It is regarded that the former has weak mineralization in the deep, and the latter has strong mineralization and extended widely. Proven by the engineering, the prediction result fit the boring information.

胶东山后金矿位于招平断裂中南段,是一破碎带中低温热液蚀变岩型金矿床,其成矿作用具有多期、多阶段叠加的特点。根据构造叠加晕理论,建立了山后金矿床的构造叠加晕模型,对1 1、1 2号矿体深部进行了找矿预测,认为前者深部矿化较弱,后者矿化较强,并且矿体有较大延深。经工程验证预测结果与钻孔见矿情况基本吻合。

 
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