1) Jiaochangba rock body
教场坝岩体
1.
Composed of three units,the Jiaochangba rock body is a compound rock body forming with pulsant magma activity and formed by process of magma mixing.
教场坝岩体是一岩浆多次脉动形成的复式深成岩体,由3个单元组成,它是岩浆混合作用形成的混合花岗岩,在混染较强的花岗闪长岩中分布有大量的镁铁质包体。
2) abutment rock
坝肩岩体
1.
An analysis of high arch dam abutment rock stability based on nonlinear FEM;
基于非线性有限元法的高拱坝坝肩岩体抗滑稳定分析
2.
The safety of arch dam depends on the stability of dam abutment rock in a large degree.
高拱坝的安全性在很大程度上依赖于坝肩岩体的稳定性,目前在设计中,高拱坝坝肩岩体稳定性分析方法主要是刚体极限平衡法,但该法不能考虑岩体的应力-应变关系,不能很好地反映坝肩岩体的破坏机理以及拱坝与坝肩岩体的相互作用效应。
3) rock mass of dam foundation
坝基岩体
1.
The rock mass of dam foundation of Zaoshi Hydroproject is mainly fine silicarenite with soft layers.
皂市水利枢纽坝基岩体主要为石英细砂岩夹软弱夹层。
4) rock mass of dam abutment
坝肩岩体
1.
When the rock mass of dam abutment is enclosed by faults, joint fissures and bedding planes,it is necessary to carry out holistic anti-slide stability analysis in order to make the abutment withstand potential slide.
当拱坝坝肩岩体为断层、节理裂隙、层面等结构面所围成,有可能产生滑移时,就应进行整体抗滑稳定分析。
6) Yangba Pluton
阳坝岩体
1.
Petrogenesis and Crust-Mantle Interaction of Mid-Triassic Yangba Pluton from Kangxian in Gansu Province;
甘肃康县阳坝岩体岩石成因及壳-幔相互作用
2.
The Yangba pluton, located in Bikou area, southern margin of Mianlue Suture, central China, were formed during middle Indosinian.
本文对出露于勉略缝合带南侧碧口地区的阳坝岩体进行了系统的岩石学、锆石U-Pb年代学和地球化学研究研究,重点讨论了阳坝岩体的岩石成因、成岩物质来源及其地质意义。
补充资料：教场
1.亦作"教场"。 2.旧时操练和检阅军队的场地。
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