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1)  reversal anticline
反转背斜
1.
Forming pattern of self-generating and self-preserving reservoirs in reversal anticline structure;
反转背斜构造自生自储油藏成藏模式
2)  faulted slope overfold
反转断坡背斜
1.
Tongue-like structures develop in the middle part of the fracture zone,and faulted slope overfolds develop in the west and east part, and faulted nose-like structures develop in the north slope.
构造带中段主要发育"舌状断鼻",东西两段发育反转断坡背斜,北坡发育断鼻。
3)  Inversion anticline
倒转背斜
4)  back-switching
背向反转
1.
Based on back-switching reaction,domain-inverted velocity can be accurately controled by multi-impulse electric field,which can be used to fabricate MgO:LiNbO_3 with submicron uniform periodical structure.
研究了掺镁铌酸锂(MgO:LiNbO3)的极化特性及其畴壁运动的性质,通过调节多个脉冲外加电场来控制畴壁的运动,在背向反转效应作用下,反转畴发生劈裂,制备出均匀的掺镁铌酸锂亚微米周期畴结构,并分析探讨了掺镁铌酸锂亚微米结构的成因及其反转机理。
5)  anticline [英]['æntiklain]  [美]['æntɪ,klaɪn]
背斜
1.
Tectonic evolution and oil and gas accumulation analysis of Dongwan anticline in west of south margin of Junggar Basin, China;
准噶尔盆地南缘西部东湾背斜带构造演化及含油气性分析
2.
The drain character and hydraulic linking are studied by analyzing the property of water-bearing and water-resisting,groundwater flowing and hydrochemistry character in Libi Gorge anticline.
通过对沥鼻峡背斜地层含水性、隔水性、地下水流向及其水化学特征的研究,得出了该区地下水的径流特征及其水力联系,并据此研究了该区水文地质对煤层气富集的控制规律。
3.
Dongwan anticline is located in the southern margin of Junggar basin with better source, reservoir and cap rocks.
东湾背斜位于准噶尔盆地南缘,其烃源岩、储集层以及盖层等条件都较好,且采用多种地球物理及地质方法,通过多次论证,证明构造是落实的,但2003年完钻的东湾1井钻探结果却无任何油气显示。
6)  backswitching
背向反转效应
1.
Using the spontaneous domains backswitching and domain side-grown effects,we can explain the mechanism of the submicron domains evolution.
基于畴背向反转效应 ,利用外加短脉冲极化电场 ,通过对脉冲宽度、脉冲间隔以及脉冲个数的有效控制 ,在掺5mol%镁的铌酸锂晶体上得到周期为 1 7μm的均匀亚微米畴结构 ,其纵向深度为 30— 5 0 μm 。
补充资料:反转

反转——
       股价朝原来趋势的相反方向移动分为向上反转和向下反转。


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