1) Gao-liu fault
高柳断层
1.
Sedimentation process was entirely controlled by boundary fault in the first and second period,sedimentary and subsidence were controlled by stepped-shaped slope belt in steep slope of the eastern Nanpu Sag in the third period,while Gao-liu fault became marginal fault and controlled sedimentary filling in its downing wall in the fourth period.
南堡凹陷的幕式构造活动可以分为三个阶段:在第一个阶段(即裂陷Ⅰ幕、裂陷Ⅱ幕),完全受到边界断裂活动的控制;在第二阶段(即裂陷Ⅲ幕),高柳断层开始活动,在南堡凹陷东部地区形成了陡坡断阶坡折带控制着沉积发育;而在第三阶段(即裂陷Ⅳ幕),高柳断层发育为控边断裂并控制着其下降盘的沉积充填。
2) high-obliquity fault
高角度断层
1.
Geomechanical analysis demonstrates that high-obliquity faults are produced by the compression-torsion stress field existing in Chinese western basins, and they may also be related to the stratum's brittle deformation.
给出了中国西部盆地台盆区普遍发育高角度(倾角>45°)断层的证据,从断裂形成的力学机制上分析了高角度断层的成因,认为中国西部盆地台盆区高角度断层的形成主要受压扭性应力场控制,同时与脆性地层的变形特点有关。
3) high-angle reverse fault
高角逆断层
4) Liukuang red beds
柳夼红层
1.
According to the principle of regional climatic stratigraphy, the author of this paper considers that Liukuang red beds characterized by the paleoclimatic marks of red colour and remaining paleosol horizons are obviously different from Malan loess and Xia shu loess formed in late pleistocene.
“柳夼红层”是分布于山东荣成市成山头半岛北岸海拔５０ｍ以下坡麓地带的一套棕红色砂层。
5) Gaoliu area
高柳地区
1.
Effect of formation pressure and temperature on rock physical properties of Neogene in Gaoliu area;
高柳地区新近系地层压力和温度对岩石物性的影响
6) Takayanagi Giichi
高柳底下
补充资料：Anglelapping角度研磨
angle lapping 的目的是为了测量junction的深度，所作的芯片前处理，这种采用光线干涉测量的方法就称之angle lapping。公式为xj=λ/2 nf即junction深度等于入射光波长的一半与干涉条纹数之乘积。但渐渐的随着vlsi组件的缩小，准确度及精密度都无法因应。如srp(spreading resistance prqbing)也是应用angle lapping的方法作前处理，采用的方法是以表面植入浓度与阻值的对应关系求出junction的深度，精确度远超过入射光干涉法。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条