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陕西八卦庙金矿床深部矿体形态变化分析
引用本文:何秋生,侯满堂.陕西八卦庙金矿床深部矿体形态变化分析[J].陕西地质,2009,27(1):19-26.
作者姓名:何秋生  侯满堂
作者单位:1. 陕西凤县四方金矿有限责任公司,凤县,720012
2. 陕西省地质调查院,西安,710054
摘    要:陕西八卦庙金矿床1290m标高以上矿体为层状、似层状、透境状,单矿体最大厚度70.3m,金品位≥3×10^-6。62-72线长200m,宽200m范围内金品位≥2×10^-6,形状完整。从1290m标高以下矿体均分支为单脉体,厚度2~10m,地质品位≥3×10^-6,矿体形态上,下部与深部变化较大。

关 键 词:八卦庙  金矿床  深部矿体  形态变化  地质特征

CONFORMATIONAL CHANGES OF OREBODIES AT THE DEPTH OF THE BAGUAMIAO GOLD DEPOSIT IN SHAANXI PROVINCE
He Qiu-shen,Hou Man-tang.CONFORMATIONAL CHANGES OF OREBODIES AT THE DEPTH OF THE BAGUAMIAO GOLD DEPOSIT IN SHAANXI PROVINCE[J].Geology of Shaanxi,2009,27(1):19-26.
Authors:He Qiu-shen  Hou Man-tang
Institution:He Qiu-shen, Hou Man-tang ( 1. Shaanxi Fengxian Sifang Gold Mining Ltd, Fengxian 720012; 2. Shaanxi Geological Survery, Xi' an 710054 )
Abstract:Mineralized ores above the elevation of 1, 290m in the Baguamiao gold deposit are present in stratiform, stratoid and phacoidal shapes, in which the maximum thickness of in- dividual orebodies is 70.3m with gold grade ≥3 × 10^-6. Gold grade is ≥2 × 10^-6 within an area of 200 m long and 200 m wide bounded in between exploration lines No. 62 and No. 72. Orebodies under the elevation of 1, 290m are present in individual mineralized veins. They have a thickness ranging between 2-10 m and gold grade ≥3 × 10^-6 , which is different from the orebodies above the elevation that the gold grade is higher at line 62, middle at line 72 and poor at line 67. Some suggestions and recommendations have been made for next production through analysis of lithology, structures, alteration and macro-variation of minerals that are obtained from underground exploration and drilling.
Keywords:Baguamiao gold deposit  orebodies at the depth  conformational changes  geological features
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