anticline

Tectonic type is anticline.

构造类型为背斜。

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Aran anticline northwest dumping fractured reservoir development is the most favorable position. 6.

Aran背斜的西北倾伏端是裂缝性储层发育最有利的部位。

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Anticline and syncline, geometrical elements of fold, description and recognition of fold in the field.

背斜和向斜 、 褶皱的几何要素、褶皱的描述和褶皱的野外描述.

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The structure is a compressive long-axis anticline with low relief and extends NE-SW. There are three local structural highs which formed three traps in the area.

通过构造分析得出本区的构造类型为NE-SW向展布的、挤压应力形成的长轴低幅度背斜构造，长轴背斜上发育三个局部高点，形成了三个局部的背斜圈闭。

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It appears to be a sharp anticline with a strong suggestion of faulting on one side.

它看来象是在一边有着明显的断层迹象的陡峭的背斜.

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Stretching structural pattern principally consists of listric normal fault and tilt block, antithetic fault and rollover anticline, and "horst-graben" structure;

伸展构造样式主要有铲形正断层与掀斜断块、反向断层与滚动背斜、垒－堑构造等；

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The structure of basement is composed of one group of East-west trending or similarly East-west trending anticline, syncline and fracture zones, and the mine is controlled by tectogenesis and distributed as East-West belt-shaped.

基底构造由一组东西向或近东西向的背斜、向斜和断裂带构成，矿床受构造控制，呈东西带状分布。

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The rolling anticline associated with declining plate of growth fault a main and gas accumulating position.

经研究可知,陆上及滨岸带与生长断层下降盘伴生的滚动背斜是主要油气聚集部位.

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Yaken anticline zone controlled by deformation mechanism of foreland basin is characterized by subtle detachment along the formation surface and shows gentle fold.

亚肯背斜带在前陆盆地变形机制控制下，以隐伏的顺层滑脱&推覆为特点，褶皱平缓。

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Controlled by structure trap, ore body located in the core of the brachy anticline or pitch part of plunging anticline which was intersected by high angle longitudinal fault.

矿体具体受断裂交汇部位附近的次级短轴背斜轴部、倾伏背斜的倾伏端及其翼部被纵向陡倾角断裂构造所切穿的部位控制，是断裂导矿与背斜构造圈闭的体现。

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The major structure in the region is a brachy anticline, in which the circular bedding slip faults strictly controlled the localization of the orebodies.

区内主体构造为一短轴背科，产于背斜中的环状层滑断层严格控制了矿体的展布。

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The low angle thrust fault at section bottom branched forward in piggy-back thrusting style, in the west of anticline they become imbricated thrust structure; in the east of anticline they become antiformal duplex structure. The south of Junggar basin;

背斜深部的低角度逆冲断层以‘前展式’向前分支，在背斜西段形成叠瓦状推覆构造，在背斜东段形成堆垛式双重构造。

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The anticline consists mainly of an overthrust nappe and two partial anticlines, and includes a blind thrust and two surface active faults.

它主要由一个逆掩推覆构造体和两个局部背斜组成，存在一条盲断层和两条地表出露断层。

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Anticline and monocline are major trap types.

圈闭类型主要为背斜圈闭及单斜圈闭.

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In Bohai Bay basin, there are some oil bearing structures, such as buried hill drape anticline structure, drag structure, gravity slumping structure, thrust structure and complex subtle fault structure combined by inhomogeneous and asynchronous structure.

在盆地内，常出现含油的潜山披覆背斜构造、拖曳构造、重力滑动构造、冲断构造和不同时期不同类型构造复合叠加而成的复杂隐蔽断裂构造。

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Trap door structure, pop up structure, and assemblage of listric thrust, dragged anticline and dragged syncline are most favorable to the accumulation of oil and gas.

滚板构造、冲起构造和铲形逆断层与牵引背斜、牵引向斜组合对油气的聚集最为有利。

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The transition zone between Structure 4 and Structure 5 occur as faulted and oblique anticline.

4号、5号构造过渡区为断裂斜歪背斜。

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Gushan anticline is the main controlling structure in Fengfeng mine district.

鼓山背斜是峰峰矿区的主控构造.

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This fold is an anticline and that one is a syncline. a fold has two limbs.

这一个褶曲是背斜而那一个则是向斜, 一个褶曲具有两个翼.

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Three anticline zones developed on the south margins of Junggar Basin.

准噶尔盆地南缘发育三排背斜带.

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This zone has little folds includes huangshan anticline, laiwu syncline and fangzhen syncline.

褶曲构造不甚发育,主要有矿山背料及其两翼的莱芜向斜和方下镇向斜.

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At present, it includes sand/ gravel body, vulcanite body, deep buried-hill, anticline with low amplitude and fractured reservoir etc.

目前，它主要包括砂砾岩体、火山岩体、深部潜山、低幅度背斜和裂缝型油气藏。

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Thermal history of TWT-2 well in the central anticline belt in Xihu Depression is reconstructed using the methods of combination and fluid inclusion microthermometry.

利用结合法与流体包裹体测温法能有效地恢复含油气盆地的热演化历史。

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Zoumaling tunnel passes through the Fangdoushan anticline where the karst development is strong.

走马岭隧道通过方斗山背斜可溶岩地区,岩溶发育强烈.

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For the rational utilization of karstic water, preliminarily studied the Shushan anticline karstic hydrogeological characteristics based on geophysical prospecting and water source well data.

为了岩溶水的合理利用，根据物探及水源井资料，对蜀山背斜岩溶水水文地质特征进行了研究。

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The compact fold structure area , anticline and. syncline in North Guizhou are often in opposite arrangement.

贵州北部紧密褶皱构造区,背斜、斜常呈相间排列.

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Now, use your compasses to measure the attitude of the two limbs of the anticline.

现在用你们的罗盘去测量一下那个背斜两翼的产状.

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Sloping downward in opposite directions, as in an anticline.

'背斜'.''的沿不同方向向下倾斜的, 如在''.'背斜'. ''地势中.

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TuoSitai anticline may be a profitable structure trap.

托斯台背斜可能是有利的构造圈闭.

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It is concluded that the seismic-tectonic activity of the Huangling anticline area behave as whole and the tectonic process is under way in the depth of 15 ￣ 20 km as well as direction distribution of tensile stress axes appears radioactive from the centre of the anticline.

结果表明，黄陵背斜的地震构造活动具有整体性，构造过程发生在15～20km的深度，张应力轴的方向分布显示以背斜为中心的幅射状态。

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