1) structural belt
构造带
1.
Oil and gas migrate laterally to the side slope of the subsag with radiation distribution; the strike of structural belts (including fault around subsidence center, lithologic pinchout, formation antidip .
油气向洼陷边坡侧向运移 ,呈放射状分布 ;环绕沉降中心分布的断层、岩性尖灭、地层反倾等构造带与鼻状构造带走向垂直 (或斜交 ) ,油气呈环带状分布 ;其放射状及环带状复合 ,形成了现今点、线、面多种油气分布格局 ;沉降中心及沉积中心不一致 ,位于沉积中心附近的构造带油气最富集。
2.
The Chong an-Shicheng structural belt is one of the important mineralization belts in northwestern Fujian Province.
在简述福建省崇安—石城构造带地质特征的基础上 ,对比了不同性质的构造岩的地球化学特征 ,并对其与金、银等多金属成矿的关系进行了初步的探讨。
2) Structural zone
构造带
1.
Hydrocarbon distribution and accumulation laws of Aershan structural zone in Erlian Basin;
二连盆地阿尔善构造带油气分布与聚集规律
2.
Structure study shows that faults were very developed in this area with a variety of configurations in both areal and vertical directions thus formed different structural zones.
构造研究发现,唐庄地区断层极为发育,平面和剖面组合形态多样,组成不同类型构造带。
3) tectonic belt
构造带
1.
Tangzang-Huangbaiyuan tectonic belt, is the extension part toward west of Shangdanjunction belt, has two sites of different periods volcanic rocks, in which volcanic rock seriesof neo-Proterozoic Danfeng group were basalt-andesite-rhyolite, that of early PaleozoicLuohansi group were picrite-andesite basalt-andesite-rhyolite.
唐藏一黄柏塬构造带是商丹结合带的向西延伸，有两套不同时代火山岩系相依分布，其中新元古代丹凤岩群火山岩系主要为玄武岩—安山岩—流纹岩，早古生代罗汉寺岩群火山岩系为苦橄岩—安山玄武岩—安山岩—流效岩，通过岩石常量元素和稀土、微量元素地球化学特征研究，证明丹凤岩群火山岩系形成千岛弧构造环境，罗汉寺岩群火山岩系形成于陆壳增厚的活动陆线构造环境。
2.
The northern margin of the Alxa block is the junction of the North China platform, Tarim platform and Siberian plateform and the foldbelts on their margins, There are four tectonic units with different sedimentary assemblage and magmatic rocks in the region, The Yagan tectonic belt is located to the north of the Yagan fault.
阿拉善地块北缘是一个多构造单元的结合部,可以划分出以下4个一级构造单元:①不成熟岛弧性质的雅干构造带;②早古生代被动大陆边缘,到晚古生代转化为活动大陆边缘的珠斯楞-杭乌拉构造带;③成熟岛弧性质的沙拉扎构造带;④元古代造山带,在古生代演化成拉张型过渡壳的诺尔公-狼山构造带。
3.
According to the plastid distribution of the tectonic belt and the shear deformation, this tectonic magma belt can be divided as follows: the north zone, the middle zone and the south zone, each of which is charac.
通过野外地质研究,大滩-四子王旗-召河庙近东西向构造岩浆岩带由色尔腾山岩群和太古代变形变质的花岗质岩侵入体组成,构造带的总体几何学特征是片理走向近东西。
4) Tectonic Zone
构造带
1.
Characteristics experimental of surrounding rock mass in tectonic zone and its rheological law analysis
构造带围岩特性实验及流变规律分析
2.
On the basis of long-range seismic profiles data obtained by peaceful nuclear explosions(PNEs) and chemical explosions,this paper introduces the research on origin and evolution of the earth,the crustal and upper mantle structure and geodynamic process of various tectonic zones in Russia,such as Uralian Orogen,Siberia Basin,Kola Peninsula,Turanian Platform and Barents Sea.
介绍了俄罗斯利用原子弹爆炸获得的长地震剖面资料和利用这些资料对地球的起源和演化的研究成果 ,以及对不同构造带 ,如乌拉尔造山带、西伯利亚盆地、科拉半岛、图拉地台和巴仑支海等地区的地壳和上地幔结构及地球动力学过程等方面的研究成果。
5) structure belt
构造带
1.
Fracture,magma activity and volcanism in Daiyun mountains structure belt are very intensive.
戴云山构造带的断裂活动、岩浆活动及火山作用强烈,不同期次的岩浆侵入和火山活动对Au、Ag、Cu、Pb、Zn矿床的形成起着一定的控制作用。
6) tectono-orogen
构造造山带
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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