1) rock salt mass
盐岩体
1.
According to the reality of bedded rock salt and clay interlayer in China,the constitutive model of seepage in rock salt mass is constituted and some numerical simulations are carried out in this paper.
结合中国地下油气储库建造过程中所出现层状盐岩体问题,建立盐岩体裂缝流体渗流数学模型,并进行了相应的数值模拟。
2) laminated salt rock
层状盐岩体
1.
Program implementation of 3-D expanded constitutive model of Cosserat medium for laminated salt rock;
层状盐岩体三维Cosserat介质扩展本构模型的程序实现
2.
Three-dimensional expanded Cosserat medium constitutive model for laminated salt rock;
层状盐岩体的三维Cosserat介质扩展本构模型
3.
It was validated primarily by an experiment on laminated salt rock samples under uniaxial compression.
该模型为分析层状盐岩体提供了一条新思路:首先利用该模型求得平均意义下的Cosserat应力,然后再回到某材料点,得到传统意义上的各层岩体的不等梯度的甚至非连续的各层介质的应力应变;结合传统的材料强度理论,可以判断某层盐岩体介质是否开始破坏。
3) carbonate mass
碳酸盐岩体
4) Weixi rock salt
威西岩盐体
5) carbonate reservoir
碳酸盐岩储集体
1.
It is difficult to be explored because of the high heterogeneity of carbonate reservoirs and the complexity of fluid in the weathering crust.
轮南奥陶系大型古潜山具有整体含油、局部富集的特点,但由于风化壳碳酸盐岩储集体非均质性极强,流体十分复杂,油气藏类型特殊,勘探难度很大。
2.
Based on the geological and geophysical study result, Cambrian-Ordovician carbonate reservoir char.
本文主要通过较系统地论述区内寒武—奥陶系碳酸盐岩储集体特征和展布规律,指出了研究区寒武—奥陶系碳酸盐岩勘探应以内幕型非浅滩储层和古风化壳再造型储层为主,今后的勘探目标应是上寒武统和盐下白云岩大中型深层内幕圈闭和中—上奥陶统缺失区潜山型和改造型潜山圈闭。
6) diagenetic fluid salinity
成岩流体盐度
1.
Discussion of diagenetic fluid salinity, carbon source and formation cause suggest that, diagenetic fluid salinity of calcite cement in this area is high, a.
探讨了碳酸 盐岩的成岩流体盐度及碳的来源和成因等问题,认为本区的方解石胶结物成岩流体为高盐度流体,方解石胶结物主要来自层内碎屑 碳酸盐颗粒或者邻近碳酸盐岩层的溶解,其碳来源主要为还原有机碳。
补充资料：高温岩体发电
利用地表深层高温干岩体所含的热量发电（见高温岩体电站）。
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