查询词典 anticlines

Within the zone, all the anticlines and synclines, successively wavy, are distributed with the same development in the entire area.

其基本特点是：一系列线状褶皱成带状展布，所有褶皱的走向基本上与构造带的延伸方向一致；在整个带内的背斜和向斜呈连续波状，基本同等发育，布满全区；不同级别的褶皱往往组合成巨大的复背斜和复向斜。

Based on analysis for paleostructural characteristics of above four areas,the paper proposed that there developed a series of paleostructure belts under the background of regional uplifting in latest Mesozoic at the front of south Qilian Mt,and those paleostructures are characterized by NWNNWstriked anticlines and synclines,whose wavelengths are 15～20 km and middlescaled. At the same time,the paper also points out that most areas in western China are lack of upper Cretaceous,which implies the existence of a broad Late Cretaceous plateau in central Asia.

通过这4个地区古构造特征的研究，提出南祁连山前区中生代晚期在区域性隆升的背景下，形成了一系列古构造带，古构造活动的特点是形成北西-北北西走向的背斜和向斜构造，这些褶皱的波长为15～20 km，为中尺度规模。

These develop from the gentle flexural undulations of earlier stages, which start to be visibly amplified by 3km shortening, and form quite strong peripheral anticlines and synclines by 8km shortening, decaying away from the fault.

这些褶皱是从早期轻微的挠曲起伏演化而来的，到挤压位移3km时，它们开始明显增强，到挤压位移8km时，已经形成非常大的背斜和向斜，其幅度从断层向两侧逐渐减小。

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。

Among such features may be synclines and anticlines, geological faults , salt domes, undulations of the crystalline bedrock under a cover of moraine, ore bodies, clay deposits and so on.

例如向斜、背斜、断层、盐丘，冰碛层之下结晶岩的顶面起伏形态，矿体以及粘土矿床等。

The survey declared that the uncomformity surface between Devonian Tiaomajian Formation and Predevonian basement make up anticlines and synclines, which indicate that the folded basement participated in Indosinian folding.

调查表明，泥盆纪跳马涧组与前泥盆纪褶皱基底间不整合界面在空间上组成背、向斜，表明褶皱基底参与了印支期褶皱作用。

The Zhouzishan part of is charactered by thrust nappe which is composed by faults thrust from west to east, anticlines and synclines, involving much of Proterzoic, Palozoic and very limited Mesozoic in which a suite of conglomerate is found in the front of thrust fractures in Late-Jurassic.

北区以正谊关断层为界，可进一步分为桌子山段和银川地堑及横山堡两大段，其中的横山堡段可根据断层展布方向、构造特征的差异，分为铁克苏庙、陶乐东和色伦卡德庙南三段。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。