normal fault的意思
normal fault中文翻譯:
[地質]正斷層;[地質]正常斷層
fault fault───斷層斷層
fault───vi.弄錯;產生斷層;vt.(通常用于疑問句或否定句)挑剔;n.故障;[地質]斷層;錯誤;缺點;毛病;(網球等)發球失誤
normal───n.(Normal)人名;(德)諾馬爾;adj.正常的;正規的;標準的;n.正常;標準;常態;法線(數學)
fault fault pack───故障故障包
double fault───兩次發球失誤,雙誤;發球雙誤
normal time───[管理]正常時間;[計量]標準時間;純勞動時間;純勞動時間,正常時間
squite normal───斜視正常
black normal───黑色正常
normal balance───[經] 正常余額
On type, the fractures appear normal fault, strike-slip fault and so on.───類型上,斷裂主要有正斷層、逆斷層和雁行斷層等形式。
I said:" this is a normal fault occurred in television, quality again good and well.───我說:“電視機發生故障這是正常的事,質量再好還有個萬分之一嘛。”
fault, reverse fault and strike-slip fault.───斷層、逆斷層和走滑斷層。
The vertical surficial strain during the great earthquake is produced by the displacement of this normal fault.───唐山地震時的垂直地形變主要是由陡河正斷層的滑動引起的。
the focal mechanism is mainly left - lateral strike - slip , with a very small normal fault slip component.───這次地震的震源機制基本上是左旋走滑,帶有微小的正斷層滑動分量。
The paper focus on the horizontal and vertical characters of tensional normal fault formed in the early Caledonian.───著重分析了加里東早期張性正斷裂的平面和剖面特征。
normal fault - a dip-slip fault in which the block above the fault has moved downward relative to the block below.───正斷層-斷層上面的巖體相對于下面的巖體作向下運動的一種傾滑斷層。
The profile morphology of normal fault includes non-rotation plane type, rotation plane type and shovel-like type.───正斷層的剖面形態以非旋轉平面式和旋轉平面式居多,可見鏟式正斷層;
the fault faults from basement to quaternary system , and has the feature of contemporaneous and normal fault.───該斷裂自基底一直斷到第四系,具同生正斷特征。
On type, the fractures appear normal fault, strike-slip fault and so on.
The structural pattern of the normal fault assemblage that occurred in the Early and Middle Jurassic may have initiated some small-scale petroleum and gas pools.
The normal fault type earthquake faults mostly strike N-S and the horizontal component of the displacement vectors of the faults is largely oriented in a nearly E-W direction.
Extensional basins are dominated by normal fault half-graben system, and there is an asymmetry in specific sense on any section across the basin.
The district normal fault is the most universal and typical structure in the extension area.
Its common structural forms are the shovel-like normal fault and spoon-like normal fault.
The normal fault zone with NEE trending are cut by some NNW faults with left-lateral dislocation in the north of the basin.
Normal fault, reverse fault and strike - slip fault.
This study shows that the formation of antithetic normal fault is controlled by NE WS strike tensile stress and dextral shear stress and the strike is nearly vertical to the tensile stress.
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