2) gentle slope
缓坡
1.
Numerical analysis of regular wave deformation and breaking on gentle slope;
规则波在缓坡上变形与破碎数值分析
2.
This new sequence stratigraphic style is called fault controlled type 1 gentle slope sequence.
对于这种新的层序地层样式 ,可称之为受断裂控制的Ⅰ型缓坡层序地层样
3.
The numerical simulation is applied to the solitary wave running and breaking on beach of gentle slope.
对孤立波在缓坡海滩上的运动进行了数值模拟 ,当孤立波接近海岸时 ,波高随水深减小迅速增大 ,以至波浪破碎 ;揭示了孤立波在不同底坡下破碎时的相对波高极值 (H/h) b,以及 (H/h) b 随坡度的变化情况 ,与合田的相对波高极值的表达式及 (H/h) b 随hb/L0 的变化曲线比较 ,吻合良
3) mild-slope
缓坡
1.
After calculating the angle between the direction of wave and current by use of the dispersion relation, a finite element model for solving the mild-slope equation with the effect of current is established in this paper.
本文利用波浪弥散关系的迭代计算求得波向与流向的夹角,并用有限元法求解含流的缓坡方程,得到在缓变地形和定常流场共同影响下的大尺度圆柱周围的波流场的耦合解。
4) ramp
[英][ræmp] [美][ræmp]
缓坡
1.
Diagenesis within the sequence stratigraphic framework in the ramp zone of the half-graben fault lake basin:An example from the Shahejie Formation in the southern ramp zone of the Dongying depression,Shandong;
箕状断陷湖盆缓坡带层序地层格架内成岩特征研究——以东营凹陷南部缓坡带沙河街组为例
2.
Its petroliferous strata around the ramp margins of depression-lacustrine basin belong to the K1q11 sand layer of Qingshuihe formation of Cretaceous.
石南31油田是准噶尔盆地腹部石南地区近年来发现的一个大型岩性油气藏,其地层属于白垩系清水河组一段的K1q11砂层组,发育于坳陷湖盆缓坡构造背景下,储集层沉积类型认识存在争议。
3.
The wide distribution and differences in regional distribution of tempestites indicate that the sedimentary environment of the western margin of Yangtze Block during Ladinian stage might be a ramp oflowlatitudes where the stormactivities were frequent.
风暴岩的区域展布差异和广泛分布表明,拉丁期上扬子西缘处于风暴活动频繁的低纬度陆棚缓坡沉积环境。
5) ramp
[英][ræmp] [美][ræmp]
缓坡带
1.
In consideration of special sedimentary and structural characteristics in northern ramp of Chenjiazhuang uplift, sequence boundary is identified by using logging curves.
针对陈家庄凸起北部缓坡带特殊的沉积、构造特征,应用测井曲线来识别层序边界。
6) gentle slope
缓坡带
1.
Study on sedimentary pattern and favorable reservoir distribution at the gentle slope of Jiyang depression.;
济阳坳陷缓坡带沉积模式及有利储集体分布研究
2.
The sags in Erlian Basin can be divided into three kinds of typical structural zones: steep slope,gentle slope and depression zone.
二连盆地各凹陷内部划分出3种典型构造带:陡坡带、缓坡带和洼槽带;不同的构造带岩性油藏成藏条件组合特征不同。
3.
Talaha region in Songliao Basin is the gentle slope which was covered with water in long term during the depositional periods of the Fourth Member of Quantou Formation to Third Member of Nenjinag Formation.
松辽盆地他拉哈地区在泉头组四段—嫩江组三段沉积时期为长期被湖水覆盖的缓坡带,层序地层学研究结果表明,层序界面在岩性—测井曲线特征上,有7种表现形式:(1)砂岩发育段内正反旋回的分界面;(2)砂岩发育段与含砂泥岩层(组)之间的正反旋回的分界面;(3)含砂泥岩层(组)与砂岩发育段之间的正反旋回的分界面;(4)钙质含量较高层段内正反旋回的分界面;(5)钙质含量较高的层(组)与含砂泥岩层(组)之间的正反旋回的分界面;(6)含砂泥岩层(组)与钙质含量较高的层(组)之间的正反旋回的分界面;(7)含砂泥岩层(组)内部的正反旋回的分界面。
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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