查询词典 nappes

The identification of RaoNan stripping and gliding nappes has an important role on the research of regional structure and oil and gas exploration.

饶南拆离滑覆体的确定，对该区地质构造研究和油气勘探有重要的意义，依据拆离滑脱构造特征，可识别滑脱型断裂、韧性挤压揉皱构造、滑覆体前缘构造、后缘构造以及滑脱面掩盖构造，这些构造与成藏条件相配伍，形成不同类型油气藏，为油气的勘探开发奠定了坚实的理论基础。

The RaoYang stripping and gliding nappes can be divided into different belts in north-south direction and different zones in east-west direction.

饶阳拆离滑覆体具有南北分带、东西分区的基本特征，其发生时间在早第三纪末和晚第三纪沉积之前，滑移方向主体为北西西向，滑移距离在6KM左右，地温场反映拆离滑覆构造发育区地温剃度低而稳定。

The evolution of the stripping and gliding nappes can be divided into the following stages: regional differential elevation and subsidence, unstable gravity and gravitational sliding, the frist wholly stripping faults and sliding stage, and the following second and third stripping faults and sliding stages.

其演化过程概括为区域差异隆升、重力不稳定、重力滑覆、大规模第一序次的拆离断层和滑覆体、依次形成第二、第三序次拆离断层和滑覆体。

In author's opinion, it had taken place back-arc foreland thrust belt during Triassic abased on the S-D peripheral foreland basin thrust nappe in South-eastern Tarim depression and Southern Tarim uplift, which made of a series of nappes and fault-related folds from south to north.

初步提出盆地南缘在志留—泥盆纪周缘前陆冲断系的基础上发育三叠纪古弧后前陆冲断带。它位于现今塔里木盆地的东南坳陷和塔南隆起地区，由一系列自盆地南部边缘向盆地内部叠瓦冲断的逆断层及相关褶皱组成的复杂冲断构造。

Applied the balanced cross-section technique to explain the characteristics of Kuqa rejuvenated foreland basin nappes and its structural shorten distance, and applied the structural triangle deposition bed discussed the time of structural deformation, that is structural deformation time in north older than in south area in Kuqa depression.

建立了库车再生前陆盆地6种局部构造变形的地质模型；利用平衡剖面技术解释了库车再生前陆冲断带，查明了构造变形特征和地层缩短量；研究了库车再生前陆盆地构造变形时间，探讨了前陆冲断带造山运动的特征和规律，指出库车前陆冲断带构造变形自北(25Ma)向南(2.5Ma)依次变新。

During early and middle Jurassic period, as a northern boundary, the fault zone controlled a seires of sedimentation of coal basins and magma activity. A lot of nappes developed during Ⅰ,Ⅱ and Ⅲ phase of the Yanshan movement. The strongest structural activity during the Yanshan movement is the Ⅱ phase, It had three pulsation and formed large-scale tectonic system with dextral strike slip.

早、中侏罗世，断裂带作为北界，控制了由西向东一系列煤系盆地的沉积作用和岩浆活动；在燕山运动的Ⅰ、Ⅱ、Ⅲ幕中分别形成了一系列逆冲构造；其中，以燕山Ⅱ幕构造活动最强，并至少经历了三次脉动作用，形成的逆冲构造不是由盆缘到盆内的&对冲&，而是受本断裂带限制，并以之为主滑面构成了区域上的大型右行走滑斜压式构造系统。

In the Paleozoic era,the northern border area of North China Craton belonged to the tectonic domain of south peri-Paleozoic ocean and is characterized by subduction-collision orogenesis,leading to the formation of EW- to ENE-trending folds,thrust faults,nappes and ductile shear zones etc.

古生代，华北地块北缘处于古亚洲洋构造域，造山作用属陆缘俯冲-碰撞型，形成以EW向至NEE向为主的褶皱、逆冲推覆构造及韧性剪切带等构造类型。

The Quele, Dabei-Tubei, Kelasu, Yiqikelike and Tugerming paleo-uplifts are located in the Kelasu-Yiqikelike and Qiulitage structural belt, as well as salt pillows, salt nappes and salt walls.

依据钻井和地震资料，在库车坳陷识别出却勒、大北-吐北、克拉苏、依奇克里克和吐格尔明等古隆起以及盐枕、盐推覆、盐墙等盐构造。

Do you know, i need you to come back

你知道吗，我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书，王祥生，李德昌。安徽省首次发现嗜群血蜱。