dip fault

dip fault的基本解释

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倾向断层

与dip fault相关的网络例句 [注：此内容来源于网络，仅供参考]

The sealing properties of fault are not only related to tectonic stress, but also to strike and dip angle of fault, depth, lithology of each fault wall, and fluid pressure.

断层的开启与封闭，不仅与构造应力直接相关，而且与断层的走向、倾角、深度、两盘岩性及流体压力直接相关。

The development is mainly controlled by main boundary normal fault with steep dip and plane geometry.

同时这类坡折带发育于主边界断层为陡倾平面状正断层控制的断陷盆地内。

According to the theory of coupling of solid and fluid, the influence of fault step and dip angle on the stresses and deformations of coal layer and confining rock along with the pressure of pore water are numerically simulated by finite element method during the process of excavation above a confined aquifer. The mechanism of water inrush and the potential point of water inrush are explored. The distance of coal column for preventing water inrush is also analyzed quantitatively.

根据流固耦合理论，采用有限元数值模拟的方法，针对承压水体上采煤过程中断层参数对煤层、围岩的应力、变形和水压力变化的影响进行了模拟分析，探讨了存在断层时突水的机理和可能的突水点位置，并定量分析了防水煤柱的预留距离。

The research results indicate that (1) fault-failure-type water inrush occurs more often than floor-failure-type water inrush under the existence of normal fault;(2) the influence of fault step and dip angle on the feature and position of water inrush is not evident, and water inrush may occur at both coal layer and the floor near working face;(3) the distance of coal column for preventing water inrush should be increased with the increase of fault step and dip angle.

得出以下结论：(1)当存在正断层时，多发生断层破坏型突水，而底板破坏型突水发生的几率较小；(2)突水性质和突水发生位置受断层断距和倾角的影响不大，煤层和采煤工作面附近的底板围岩都可能成为突水涌出点；(3)随着断层断距和倾角的增加，防水煤柱的合理留设距离应随之增大。

Finite strain measures and kinematic vorticity analysis of deformed granite in mylonitic zone show that ductile shear zone is between plane strain and constraint strain and belongs to lengthening-thinning shear zone. Sub-striking stretch lineation in ductile shear zone and dip strea on brittle fault surface are not result of transferring of lineation but production of different deformations.

糜棱岩带变形花岗岩的有限应变测量和运动学涡度分析显示剪切带总体应变为介于平面应变与拉长应变之间的类型，属一般加长-减薄剪切带；断层系中近走向线理和倾向擦痕不是线理转化的结果，而是不同阶段变形的产物。

与dip fault相关的网络解释 [注：此内容来源于网络，仅供参考]

dip fault：倾向断层

dip entry 倾斜苍坑道 | dip fault 倾向断层 | dip joint 倾向节理

dip fault：倾斜断层

断层 fault | 断层走向 fault strike | 倾斜断层 dip fault

fault dip：断层倾斜

断层绕射 fault diffraction | 断层倾斜 fault dip | 断层移距 fault displacement

fault dip：断层倾角,断层倾斜

fault diagnosis ==> 事故分析,故障诊断=>故障診断 | fault dip ==> 断层倾角,断层倾斜 | fault display ==> 故障显示

fault dip：傾斜斷層

"复杂断层","Fault,compound" | "倾斜断层","Fault,dip" | "常态断层","Fault,normal"