1) fault zone interior structure
断裂带内部结构
2) texture of fracture belt
断裂带结构
3) internal rupture
内部断裂
4) fault structure
断裂结构
1.
According to the geometry and kinematic differences of the boundary faults, the fault structures of the steep slope belts of Chezhen Sag may be classified into two types, simple and composite types, and four kinds of styles, board -like, shovel-style, ladder style, and slope-flat style.
根据边界断层几何学和运动学的差异,将车镇凹陷北部陡坡带的断裂结构分为简单和复式2类及板式、铲式、阶梯式和坡坪式4种。
2.
In this paper,we use the Liuxi structural belt of Raoyang sag as the research object,through making the 3D seismic data interpretation to the datum horizon of Liuxi,analysis the fault structure,developmental stages of fault,structure style of step-fault zone,development history,confirm the beneficial zone,and make a description of beneficial traps.
本文以饶阳凹陷留西构造带为研究对象,通过对留西地区各标志层进行精细的三维地震资料解释,系统分析留西构造带的断裂结构、断裂发育期次、断阶带构造样式、构造发育史,落实有利区带,并对有利圈闭进行综合评价描述。
6) structural fracture belt
构造断裂带
补充资料：间接带隙(见半导体的能带结构)
间接带隙(见半导体的能带结构)
indirect band gap
I’ed接带隙indireet band gap见半导体的能带结构。
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