重力滑动构造在我国煤田中广泛分布。
The gravity gliding structures are widely spreaded in the coal fields in China.
说明：一款很漂亮的圆盘形的菜单，实现重力滑动，点击等。
A very nice disc-shaped menu, realize the gravity slide, click, etc.
三个带呈东拉西压模式，它是盖层沿基底发生重力滑动的产物。
The three zones display a model of extension in the east and compression in the west. This belt is the product of gravitational gliding of the covers along the basement.
凹陷北部斜坡带的变形机制主要是山前重力滑动和山麓逆冲作用。
So in the northern slope of the depression developed gravitation gliding tectonics and fold and thrust structures.
煤系向斜两翼产生的重力滑动构造，可导致向斜轴部出现复杂的构造图象。
The gravity slide structures occurred in both limbs of coal measure synclines will give rise to complicated structural image in the axial part of the syncline.
早期重力滑动与晚期断裂深部挤压复合型；5。深断裂挤压与重力扩张复合型。
The early gravity sliding with the late fault compression 5. The deep fault compression with the gravity spreading.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Thrust and gravity gliding structures are both developed in the west of Lianyuan depression.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Because of the magmatite intrusion in Late Yanshan period and the formation of Xikuangshan anticline, gravitation gliding structures are developed at the both wings of the anticline.
库车前陆褶皱带盐构造的形成可能受挤压作用、重力滑动和重力扩展作用多重控制。
The Formation of the salt tectonics in the Kuqa foreland fold belt may be controlled by compression, gravitational gliding and gravitational spreading.
该带在形成过程中经历了块断抬斜、重力滑动、反拖牵引、盐岩拱升等多种形式的构造变动。
The central uplift belt underwent a series of structural evolution:fault block tilting, gravity slumping, inverse drag, rock salt uplifting and so on.
盖层内抗变形能力不同的海相地层在构造推挤和重力滑动中形成了多期次、多方向的滑脱构造。
The Marine strata with different anti-deformability in the cover formed polydirectional and polyphase decollements under the tectonic compression and gravitational sliding.
滑坡形成与长江下切产生临空面、重力滑动密切相关。 测定滑坡区结构面（带）形成或滑动年龄是区分断层、滑动面以及研究滑坡形成历史的有效手段之一。
Therefore dating the formation of structural faces (zones) or slide time is an effective means for distinguishing faults and landslides and for studying the history of formation of landslides.
本文讨论利用重力资料反演莫霍面时，地壳横向不均一性，密度随深度变化以及异常数据滑动平均处理对解释结果的影响程度。
The lateral inhomogeneity and the variation of density contrast with depth in the crust and their effects on the inversion of gravity field are discussed.
但是在钢轨的内侧面，由于车轮经常滑动和重力延缓了保护层的生成。
But at the gauge face of the rail, high levels of slip and gravity inhibit the formation of protective layers.
在同一凹陷中，断层的旋转、滑移运动，生、储、盖层的沉积作用和重力侧向滑动作用同步发生。
In the same depression, the rotation and slide of the fault, the sedimentation of source-reservoir-cap rock and gravity caused lateral sliding take place synchronously.
利用岩石破坏过程分析软件——RFPA2D对该模型进行数值模拟，模拟结果显示了重力坝破坏的三种模式：表层滑动、深层滑动及混合滑动。
The failure process of the model was simulated by RFPA2D software. Simulation results show three failure modes of gravity dam, such as surficial slide, deep slide and mixed slide.
结果表明斜坡为多级阶地特征，在没有外界动力的作用下，斜坡坡体重力作用不足以使斜坡产生滑动。
The result demonstrated that the slope is a multistage terrace, if there is no exokinetic force existed, the gravity action of the slope body is insufficient to make the slope sliding.
结果表明斜坡为多级阶地特征，在没有外界动力的作用下，斜坡坡体重力作用不足以使斜坡产生滑动。
The result demonstrated that the slope is a multistage terrace, if there is no exokinetic force existed, the gravity action of the slope body is insufficient to make the slope sliding.
应用推荐