背斜

A series of NW-SE-trending faults and reverse"S"anticlinal bulge in central depression zone between north center fault and south center fault, which are main position of celestite deposits, come into being storage ground of celestite deposits.

中央断块内一系列北西向张性断裂和大量的反"S"型背斜构造带是锶矿的主要定位场所，形成了成矿系统的储矿场。

The other is concave upward with younger rocks of Silurian shale and siltstone toward the center of curvature. The former is called anticline and the latter syncline. The sides of the folds are known as limbs

而另一个褶曲向上凹，较新的志留系页岩和砂岩位于弯曲的中心部位，前者被称为背斜，后者则称之为向斜，褶皱核部两侧叫做褶皱的翼部。

The other is concave upward with younger rocks of Silurian shale and siltstone toward the center of curvature. The former is called anticline and the latter syncline. The sides of the folds are known as limb s

而另一个褶曲向上凹，较新的志留系页岩和砂岩位于弯曲的中心部位，前者被称为背斜，后者则称之为向斜，褶皱核部两侧叫做褶皱的翼部。

DF1—1 gas field is located in the north of the mud diapir structure belt in Yinggehai Basin,being a successive anticlinal structure formed by mud diapiric activity,i.e.an integral shallow giant gas field.

DF1—1气田位于莺歌海盆地泥底辟构造带北部，是一个由泥底辟而形成的继承性背斜构造，即整装的浅层大气田。

A syncline is the opposite type of fold, having downwardly convex layers with young rocks in the core.

向斜是背斜褶曲的相反形式。岩层向下凹，核心为年青的岩层。

Hongqiling Cu, Ni sulphide deposit is located in ca. 45km south of Panshi city, Jilin province. It is also situated tectonically in the Tieling contact zone between Jihei geosyncline and Liaodong syncline in North China plate, which is divided by Huifahe fault.

红旗岭铜镍硫化物矿区位于吉林省磐石市南约45Km，地处吉黑地槽与华北台块辽东台背斜铁岭台凸接触地带，辉发河断裂是其分界线，特殊的构造位置决定了本区的构造活动强烈，岩浆活动发育，具备良好的成矿环境和条件。

6In reservoir aspect, the oil source is sufficient in the study region, which betweeneastern side of main hydrocarbon hollow trough in the northwest of Beier and deep big faultcrossing segment;the reservoir mainly develops sandstone and the gritstone sub-faciesdeposition of the front fan delta. Petrophisical is bad, the reservoir bearing oil type mainly isfault anticline oil pool and the lithological character-structural oil pool.

6研究区位于贝西北主生烃洼槽的东侧和深大断层的交汇处，油源充足；储集体主要为扇三角洲前缘亚相砂砾岩体，物性较差；油藏类型主要为断背斜油藏和岩性—构造油藏。

In it, there may exist many incompletely reversed normal faults and the corresponding rolling anticlines.

在这一层可能还存在很多没有完全反转的正断层及其相应的滚动背斜。

It is known from the active tectonic research results that the northern margin of Tianshan mountains is characterized with typical intracontinental active tectonics,which has thrust faults and anticlines with multiple parallel mountains.

已有活动构造研究结果表明，天山北缘具有典型的大陆内部活动构造特征，表现为多排平行山体的背斜和逆断裂。

In later Guantao Formation, compression is primary, the maximal principle stresses no more than 0.1 MPa, and in central of Jiyang Depression horizontal shear stresses are dextral displacement, but sinistral displacement showed in west and east.

馆陶组油气藏都是它源性油气藏，断层是油气垂向运移的主要通道，盆地主要断裂系统控制油气垂向和平面上的分布，断层活动形成的披覆背斜，断鼻、断块构造，岩性尖灭是馆陶组主要的油气圈闭类型。

But we don't care about Battlegrounds.

但我们并不在乎沙场中的显露。

Ah! don't mention it, the butcher's shop is a horror.

啊！不用提了。提到肉，真是糟透了。