叠加褶皱
- 网络superimposed fold
-
贵州境内扬子准地台燕山期叠加褶皱特征
The Superimposed Fold Features of Yangtze Paraplatform of Yanshan Period in Guizhou
-
遵化期第二幕表现为舒缓的东西向叠加褶皱。
The second episode of Zunhua age was EW stretched superimposed fold .
-
纵弯叠加褶皱的模拟实验研究
A study on model experiment of the superposed folds of flexural folding
-
论中国煤矿中的叠加褶皱
Discussion on superposed folds in coal mines of China
-
大巴山侏罗纪叠加褶皱与侏罗纪前陆
Jurassic Superposed Folding and Jurassic Foreland in the Daba Mountain , Central China
-
纵弯叠加褶皱地区应力场研究-以川东北地区为例
Research on the stress fields in superposed fold Area-An example from northeastern Sichuan
-
东昆仑造山带前陆盆地的叠加褶皱及其变形机制
Superimposed folds and corresponding deformation mechanism in foreland basins in Eastern Kunlun orogenic zone
-
叠加褶皱的类型及变形图像
Types and deformation patterns of superimposed folds
-
叠加褶皱的数学分析
The Mathematical Analysis of the Superimposed Folds
-
赣东北前震旦纪陆内叠加褶皱
Pre-Sinian Superimposed Intracontinental Fold in Northeastern Jiangxi
-
除具陆相盆地的一般特征外,还具有十分突出的叠加褶皱变形特征,因而极为少见。
It has not only common characters of continental basins , but also remarkable superimposed fold deformation .
-
武当山推覆体中段的叠加褶皱及构造序列的初步划分
Primary division of the superimposed fold and tectonic sequence in the middle section of Wudang Mountain nappes
-
纵弯叠加褶皱地区岩石有限应变特征&以川东北地区典型叠加褶皱为例
The Features of Finite Strain of Rocks in the Superimposition Fold Area Under Buckling in Northeast Sichuan Province
-
叠加褶皱的研究是以叠加机制和叠加类型为基础的。
The research on superposed folds is based on the understanding of the mechanism and the types of superposed buckling .
-
晚期褶皱表现为不同时代、不同方向、不同类型的叠加褶皱,轴面近直立,有时伴有轴面劈理。
The later folding is characterized by the superposition of folds of different ages and orientations , nearly-vertical axial-plane and rare cleavages .
-
此外还将讨论叠加褶皱层应变和小构造的多成因和应用问题,其中包括斜纵弯应变和褶皱变缓展平引起的应变和小构造。
The strain and small scale structures in fold layer specially caused by the oblique buckling , opening and unfolding are discussed .
-
因此,正确地识别叠加褶皱,就成为查明变质岩区构造及变形历史的关键之一,也是建立变质岩层层序最需重视的问题。
So to recognize superposed folds correctly is one of the keys to identify the structures and deformation history in metamorphic terrains .
-
中元古代末的神功运动表现强烈,青白口纪末的晋宁运动叠加褶皱明显。
The Shengong Movement in late Middle Proterozoic Era was strong and the superimposed fold of Junning Movement in late Qingbaikou Period was clear .
-
叠加褶皱与拼接带具有成生联系,且各自代表了不同构造部位的变形特点。
Therefore , the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in different structural positions .
-
新疆北山西段中坡山地区褶皱基底中元古界白湖群中普遍存在新月形、蘑菇形及线形紧闭褶皱,构造解析表明它们是由叠加褶皱形成的复杂露头干涉形式。
There are folds formed by superposition of two period folds , in the folded basement of the Zhongposhan area , the western segment of the Beishan tectonic belt .
-
我国有人论述了早期褶皱的枢纽、拐线的迁移是正纵弯再褶皱的一种机制,依此提出了正纵弯叠加褶皱的三种基本类型。
Some domestic workers expound that the hinge and inflexions shifting of early fold as a mechanism of superposed normal buckle fold and three basic types of superposed normal buckle fold .
-
胶南造山带西段显示了以韧性剪切带为主,穹隆构造、弧形构造及复杂的叠加褶皱共存的构造格局。
A paragenetic tectonic framework is reflected in the west part of the Jiaonan orogenic belt , by the coexistence of mainly ductile shear zones and dome structure , arc structures as well as complicated superimposed folds .
-
在地质演化过程中,渣尔泰山群主要经历了3期褶皱变形,即早期的层内褶皱,主期同斜倒转褶皱与晚期叠加褶皱。
In the geological evolution of the fold structure , this suite of strata experienced three stages of fold deformation : the intraformational fold in the early stage , the homoclinal reverse fold in the major stage , and the superimposed fold in the late stage .
-
西部变形弱、以近EW向宽缓褶皱变形为主,东部变形强、并叠加了NE向褶皱和逆冲断层变形。
In the Western part the deformation was weak only EW-trending open folds occurred while in the Eastern part deformation was stronger but some NE folds and thrusts superposed on the EW folds .