1) east-west structural zone
东西构造带
2) EW structure belt
东西向构造带
1.
EW structure belt and function of controlling diagenesis and mineralization in Danghe'nanshan district;
党河南山地区东西向构造带及其控岩控矿作用
3) E-W-trending structure
东西向构造
1.
The E-W-trending structures formed earlier and t.
在收集整理大量资料的基础上,总结出赤水地区二叠系、三叠系储层构造是在四川盆地形成的大环境下形成的,其东西向构造形成时间早于南北向构造,早期的东西向构造是由于黔中古隆起向北的构造挤压力作用形成的;晚期的近南北向构造则是受四川盆地东部边缘北西向构造作用力在南端的派生应力作用形成的。
2.
It was generally considered that the Xuzhou arc probally terminated on the southern side of the original Feng-Pei fault and that north of it may be an E-W-trending structure.
传统认为徐州弧止于原丰沛断层南,其北则为东西向构造。
4) eastern and western Himalayan syntaxis
东、西构造结
5) Kuidong structural belt
葵东构造带
1.
Oil and gas accumulation conditions and exploration potential in Kuidong structural belt of Liaohe tidal zone;
葵东构造带油气成藏条件及勘探潜力研究
6) the Baidong structural belt
白东构造带
1.
Based on structural stress analysis and graben structural assemblage, we consider that the Baidong structural belt was formed in an extension-slipping setting rel.
位于渤海湾盆地黄骅坳陷北部的白东构造带,受新构造运动影响形成了整体东西向"S"型展布,堑心组合内断层成弧形交错、南北对掉的"包心菜"状构造。
补充资料：东西
①东边和西边。②从东到西（距离）：这座城～三里，南北五里。
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