背斜的

Results Gas accumulation dynamics researches focus on anticlinal trap （including updip structure and stratigraphic trap）, synclinal trap and coalbed gas trap.

结果对天然气成藏动力学机制的研究主要围绕背斜圈闭气藏（含上倾型构造及地层圈闭）、向斜圈闭气藏及煤层气藏3类气藏进行，但是，研究的侧重点差别很大。

Jilegeyoute synclinorium belt, lies in front of Pamirs-Kunlun, being a counterpart of Kangsu-Wulukeqiati synclinorium belt, Coupling Pamirs-Kunlun.

其总体呈向斜型，地层外老内新，发育复杂多样的次级构造，如多种形式的背斜与冲断构造为特征。

Raplee Ridge, part of the Monument Upwarp in southeastern Utah, is a long, narrow, folded anticline that formed about 70 million to 50 million years ago.

Raplee岭，纪念碑的一部分向上翘起在犹他的东南部，是一个狭长，折叠背斜，形成约7000万至5000万多年前。

Based on studying of these special structure bodies and fluid movement s for gas hydrate formation,six types of tectonic-controlled gas hydrate reservoirs including accretionary prism,buried anticline,basin-edge slope,fault-folded,slide and dirpir are summarized.

通过对这些特殊构造体与天然气水合物成藏关系的研究，结合流体活动对水合物形成的影响，总结出陆缘地区有增生楔型、盆缘斜坡型、埋藏背斜型、断褶型、滑塌型及底辟型等六类构造控制型水合物矿藏。

Based on studying of these special structure bodies and fluid movements for gas hydrate formation, six types of tectonic-controlled gas hydrate reservoirs including accretionary prism, buried anticline, basin-edge slope, fault-folded, slide and dirpir are summarized.

通过对这些特殊构造体与天然气水合物成藏关系的研究，结合流体活动对水合物形成的影响，总结出陆缘地区有增生楔型、盆缘斜坡型、埋藏背斜型、断褶型、滑塌型及底辟型等六类构造控制型水合物矿藏。

Structural wedges are very typical in the southern margin of Junggar Basin and exhibit a variety of shapes and styles imbricated each other out of sequence.

准噶尔盆地南缘3排背斜内带的构造楔形体模式非常典型，并表现为&混序&的特征。

By comprehensive analysis of the characteristics of formation and reconstruction, six tectonic belts in the northeast part of Junggar basin were divided: marginal obduction zone in Early Paleozoic(O1-2)?melange mag-ma collision zone of late Paleozoic (D1), volcanic arc-compression zone of Late Paleozoic (D1), back-arc folded belt of Late Paleozoic (D2_3), marginal depression folded belt of Late Paleozoic (C1-P2) and foreland basin gentle anticline belt of Mesozioc era, etc.

通过&建造&与&改造&特征的综合分析，划分了准噶尔盆地东北缘的构造带：早古生代（1－2）陆缘逆冲带；晚古生代（D1）混杂岩浆碰撞带；晚古生代（D1）火山岩浆岛弧挤带；晚古生代（D2－3）弧后盆地褶皱带；晚古生代（C1－P2）陆缘盆地褶皱带以及中生代前陆盆地平缓背斜带等6个构造带。

This kind of structure develops in the platform cover of slight structure deformation, dominated by olivary dome, stretched short-axis anticline and long wall.

这类构造发育于构造变形十分轻微的地台盖层中以卵圆型穹窿、拉长的短轴背斜和长垣为主。

According to their forms and the stratigraphic facing, folds can be subdivided into anticlines and synclines.

P13 根据褶皱的形态和组成褶皱的地层面向，将褶皱进一步分为两种基本类型：背斜和向斜。

The Baoertu copper deposit is located in the Metamorphic rocks in the anticlines crest of Aimutaiwula, which located in the east part of the contact belt between South Tianshan and Middle Tianshan in the plate of Tarim, and on the south of the great faults of Wu\'wamen-Bao\'ertu. And the Baoertu copper deposit is one of the mainly metallogenetic areas, which are polymetallic metallogenic belts in South Tianshan-Haerke-Kumishenjin, including gold, copper, lead, zincum.

包尔图铜矿位于塔里木板块北缘南天山与中天山接触带的东段，乌瓦门-包尔图大断裂南侧，分布于艾木太乌拉背斜核部的一套变质岩中，是南天山-哈尔克-库米什金、铜、铅、锌多金属成矿带主要成矿区之一。

We have no common name for a mime of Sophron or Xenarchus and a Socratic Conversation; and we should still be without one even if the imitation in the two instances were in trimeters or elegiacs or some other kind of verse--though it is the way with people to tack on 'poet' to the name of a metre, and talk of elegiac-poets and epic-poets, thinking that they call them poets not by reason of the imitative nature of their work, but indiscriminately by reason of the metre they write in.

索夫农 、森那库斯和苏格拉底式的对话采用的模仿没有一个公共的名称；三音步诗、挽歌体或其他类型的诗的模仿也没有——人们把&诗人&这一名词和格律名称结合到一起，称之为挽歌体诗人或者史诗诗人，他们被称为诗人，似乎只是因为遵守格律写作，而非他们作品的模仿本质。

The relationship between communicative competence and grammar teaching should be that of the ends and the means.

交际能力和语法的关系应该是目标与途径的关系。