main orebody 中文意思是什麼
main orebody
解釋
主礦體-
Lode country assume silllike - similar silllike, and the next big anastigmatic, ground and west branch river set strench are consistent. it suffer the gravel silica rock, arena silica control. a handful of lode country or main lode country byway little orebody assume vein, or have the characteristic of balk reappear, compound of branch. these manifest the obvious characteristic of ore construct control
礦體以層?似層狀產出為主，其次為大的透鏡狀，地表延伸與西岔河組地層一致。受礫屑硅質巖、含礫砂屑硅質巖控制。少數礦體或主礦體旁側小礦體呈脈狀、或具尖滅再現、分支復合特徵。 -
In the main ( no. ) orebody, it is characterized by high as content but low sb, in no. orebody, it is characterized by high sb content but low as ; in both orebodies, it is characterized by high zn content and insignificant temporal and spatial variations of chemical compositions
在以銅為主的主礦體（號礦體）中，黝銅礦幾乎均屬鋅砷黝銅礦，含銀甚低，其化學成分在時空分佈上變化不大且無顯著的變化規律，不同類型礦石之間黝銅礦的成分變化也不大；但在以鉛鋅為主的次要的號礦體中黝銅礦含一定量的銀。 -
There are five main gold - containing ruptures, which are in the approximate sn - orientation, the strike is nne, the dip is about 80 ; the gold mine beds exist in above ruptures and accessorial ruptures, rupture ' s breadth is about 10 meters, and their shapes is f lexuosity in the strike and dip, and orebody pinches, then appears or pinches then appears in both sides of rupture in strike and dip
牟乳礦帶內主要有5條近南北向的主幹容礦斷裂，走向約nne10 ，傾角80左右，區內金礦床主要賦存於上述斷裂和次級斷裂之中。斷裂帶一般寬10m左右，斷裂在走向與傾向上多呈舒緩波狀，礦體沿走向與傾向呈尖滅再現或尖滅側現。
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