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褶皱

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In addition to these two types of folds, however, we must mention another one, which is not easily classifiable as either anticline or syncline and is referred to as a monocline .

然而,除了上述两种褶皱外,我们还必须提到另外一种,这种褶皱不易归类为背斜或向斜,而被称为单斜褶皱

Is the fold structure can control large-scale the medium landform growth in the fold change aspect's significance; The fold structure often can control the minerals the formation and the tax saves the situation; The large-scale fold structure to studies the whole world diastrophism the way the direction and the nature significance significant and so on four aspects.

褶皱变动方面的意义是褶皱构造能控制大、中型地貌的发育;褶皱构造往往能够控制矿产的形成和赋存情况;大规模的褶皱构造对研究全球地壳运动的方式、方向及其性质意义重大等四个方面。

There are some small scale folds in the foliated rock. Their fold axial planes are parallel to the foliation and on the surface of folded foliation, the stretching lineation is parallel to the fold hinges.

在这些片理化岩石中有一些小型褶皱,这些小型褶皱的轴面平行片理面,在被褶皱了的片理面上有着平行褶皱枢纽分布的拉伸线理。

Type IB: Isocline is convergent towards inner arc at a right angle to the fold.

根据等斜线的收敛层度,再细分为三个亚型:IA型:等弧线向内弧强烈收敛,各线长短判别极大,内弧曲率远大于外弧曲率,为典型的顶薄褶皱;IB型:等倾斜线向内弧收敛,并与褶皱面垂直,各线长短大致相等,褶皱层真厚度不变,内弧曲率仍大于外弧曲率,为典型的平行褶皱;IC型:等斜线相内弧轻微收敛,转折端等倾斜线比两翼附近的要略长一些,反应两翼厚度有变薄的趋势,内弧曲率略大于外弧曲率。

A-type folds and sheath folds: a-type folds are those whose axis is parallel to the elongation lineation.

a型褶皱和鞘褶皱:a型褶皱褶皱轴与拉伸线理平行的褶皱,可以由剪切作用直接形成,或是由b型褶皱随着剪切变形的加剧改造而成,一般发育在剪切带的中心部位。

Based on our own simulation results and results of some numerical simulation of single Fold structure by other investigators in recent years, the factors that affect single fold shapes and the variation of maximum principal stress and horizontal strain during the deformation of single fold are discussed in this paper.

本文结合近年来单层褶皱构造数值模拟研究进展,以及笔者近几年来对单层褶皱所进行的数值模拟实验研究,主要论述了单层褶皱变形的影响因素,单层褶皱变形过程中的最大主应力与水平应变的变化及其影响因素等。

There are some small scale folds in the foliated rock. Their fold axial planes are parallel to the

在这些片理化岩石中有一些小型褶皱,这些小型褶皱的轴面平行片理面,在被褶皱了的片理面上有着平行褶皱枢纽分布的拉伸线理。

According to the classification and stage principles of folds, we divided the folds into three stages. The first periodic folds: the prime folds of the Indosinian orogenic cycle; the second periodic folds: the intrafolial theomorphic folds of Post Indosinian; the third periodic folds: the superposed folds of Himalayan to Yanshanian.

根据褶皱构造的分类、分期原则,首次将雅砻江锦屏水电站地区褶皱划分为3期:第1期为印支造山期主褶皱;第2期为印支期后层内流变褶皱,第3期为燕山期-喜山期叠加褶皱

This paper identified two generations of superimposed folds that widely develop in Indosinian to early Yanshanian tectonic layer (DJ12) in South China, and it is found that the earlier generation of folds is well zonated in WE and the later one is distributed in NNE.

通过分析华南印支-早燕山构造层(D-J12)广泛发育的褶皱构造,识别了早中生代两个世代褶皱构造的横跨叠加型式,发现早期近东西向褶皱构造具有南北成带、晚期NNE向褶皱构造具有东西分区的区域展布特征。

The former fold is also called flow fold, consisting of a series parallel folds characterized by closed but well developed synclines with wide and gentle anticline in between. On thecontrary, the latter fold is characterized by completely developed anticlines with wide and gentle box shaped syncline in between.

隔档式褶皱又称流状褶皱,由一系列平行褶皱组成,其特征是背斜紧闭,发育完整,而两个背斜之间的向斜平缓开阔;隔槽式褶皱与前者相反,特征是向斜紧闭且发育完整,而两个向斜间的背斜平缓开阔,常呈箱状。

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