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1)  extensional fault system
伸展断裂系统
1.
Based on detailed interpretation of over 3 000 km of seismic profiles,the fault systems in the Eastern Tarim basin have been established and three systems,the Kongquehe fault system,the Southeast fault system,and the extensional fault system,have been identified.
通过逾3 000 km地震剖面的精细解释,构建了塔里木盆地东部的断裂系统,它们分别是孔雀河断裂系统、东南断裂系统和伸展断裂系统
2)  outstretching rift system
伸展断裂系
3)  extensional fault
伸展断裂
1.
Characteristics and mechanism of Late Mesozoic extensional faults in West Shandong Uplift
鲁西隆起晚中生代以来伸展断裂特征及形成机制
2.
According to the two schemetic maps of the faults from 3D seismic data, the extensional faults in this area trend mainly NE, NEE, EW, and minor other secondary direction.
在不同地段,伸展断裂具有不同的优势方向。
4)  extensional fault systems
伸展断层系统
1.
Sand box analog models have been proved to be powerful tools for demonstrating the structural styles of extensional fault systems.
砂箱模拟实验已被证明是研究盆地内部伸展断层系统的有效工具。
5)  fault system
断裂系统
1.
Genetic mechanism of the fault system in the Yinggehai basin;
琼西莺歌海盆地断裂系统的成因机制
2.
Application of ant colony algorithm in fault system interpretation
蚂蚁算法在断裂系统解释中的应用
3.
Formation mechanism of Cenozoic fault system of Nanpu sag in Bohai Bay Basin
渤海湾盆地南堡凹陷新生代断裂系统形成机制
6)  Fault systems
断裂系统
1.
Fault systems in central area of the Tarim Basin:geometry,kinematics and dynamic settings;
塔里木盆地中央地区的断裂系统:几何学、运动学和动力学背景
2.
As a result,the authors find that these fault systems are statistically self similar within the scale range studied (r=0.
本文运用分形理论对张强凹陷科尔康油田沙海组下段顶(T1)、九佛堂组顶(T2)和义县组顶(T3)3个反射层断裂系统的分布特征进行了研究,发现在标尺范围(8—0。
3.
Combined with research of fault systems in structural subarea,the writers divided the southern NCC in Meso—Cenozoic into western Henan basin—ridge area,eastern Henan basin area and Xuzhou—Huainan basin area.
结合分区断裂系统研究,指出华北克拉通南部中新生代构造分区包括豫西盆岭区、豫东盆地区和徐州—淮南盆地区。
补充资料:伸展链长
分子式:
CAS号:

性质:在充分伸展状态下的高分子链的长度。常用R2表示。R2为高分子链的均方末端距,是表征高分子尺寸的一个重要物理量。伸展链主要有锯齿型结构和螺旋型结构两种。对应的伸展链长分别为R2链齿=[Nb·sin(a/2)]2(式中b为键长,a为相邻两键夹角,N为键数)和R2螺旋=K2N2b2(式中K为取向参数的平均值)。

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