Anticline and monocline are major trap types.
圈闭类型主要为背斜圈闭及单斜圈闭。
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。
The mining area is situated at the northeast wing of Xian'ebaodan Anticline.
矿区位于仙鹅抱蛋背斜的东北翼。
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。
Tangxinzhai gold deposit is located in the northwest part of Laizishan anticline.
塘新寨金矿位于赖子山背斜北西端。
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。
There are a lot of traps with the main styles of draping anticline, fault trap and deepwater fan.
圈闭数量较多，其类型主要有披覆背斜、断层圈闭和深水扇体等。
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。
Among them, rollover anticline, compression anticline and horst are the main area of hydrocarbon enrichment.
滚动背斜、挤压背斜、地垒等构造是油气富集的主要场所。
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、向斜常呈相间排列。
Distortion phenomenon for deviated seismic height in high dipping anticline widely existed in seismic section.
高陡背斜的地震高点在地震剖面上普遍存在着偏离畸变现象。
Geological condition and TEM geophysical anomaly is suitable for mineralization in south flank of the anticline.
在主背斜南侧存在着有利的成矿地质条件及矿致TEM物探异常。
Sazhi oil sand mine is located at Sazhi anticline of the western margin of Yuanmou uplift belt in Chuxiong Basin.
楚雄盆地洒芷油砂矿位于元谋隆起西部边缘洒芷背斜上。
It has been proved that the indication of the upheaval at the lower part of the section is the reflection of trapped anticline.
正演结果表明，时间剖面上的深层隆起显示是圈闭的背斜构造的反映。
Huoyanshan structure belts are controlled by the basement thrusts. The formation of anticline traps is controlled by the faults.
火焰山构造带受基底逆冲断裂控制，断裂控制背斜圈闭形成。
The salt flow resulted in several kinds of structural traps mainly including salt ridge anticline, salt dome and salt edge syncline.
因盐体塑性流动形成的构造圈闭类型主要有盐脊背斜、盐丘背斜、盐边向斜等。
Synsedimentary anticline traps mainly distribute in Mangya depression, and mainly develop in the middle-shallow layers (N23-Q1 + 2).
同沉积背斜圈闭主要分布在茫崖坳陷，层位上主要发育在中浅层(N23 - Q 1 + 2)。
The tunnel goes through complex geological conditions in Maoba syncline, Tongmaling anticline and Lengshuihe shallow-buried section.
该隧道穿越地质复杂的毛坝向斜、桐麻岭背斜和冷水河浅埋段。
The ore-hosted strata of Xitieshan lead-zinc ore deposit is located in a limb of a anticline and suffered from deformation partition.
锡铁山大型铅锌矿床含矿岩系的构造格架位于背斜的一翼，普遍遭受变形分解作用。
The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.
盐上构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造和盐推覆构造等；
Because of special characteristics of petroleum geology in Liyuan anticline, hydrocarbon shows interpretation and evaluation becomes very difficult.
栗园背斜特殊的石油地质特点，给油气显示层解释评价带来一定困难。
The Kelasu triangle zone occurs under the Paleogene evaporites in Kelasu anticline zone of Kuqa thrust-and-fold belts, Tarim basin (Northwest China).
塔里木盆地库车褶皱冲断带克拉苏构造带在古近系膏盐岩之下发育克拉苏三角带。
This paper studied the formation of the Yulong porphyry copper deposit controlled by the anticline trap structure and the distribution of the ore bodies.
文章研究了背斜圈闭构造控制玉龙斑岩-矽卡岩型铜(钼)矿的形成和矿体的分布。
Under the effect of regional tectonics there develop many raws drape anticline and active fault in the front of mountain and they have especial motion fashion.
由于受区域构造长期作用的影响，在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂，且运动方式具有独特性。
The Central Anticline Zone composed of fault-band folds and a few fault-propagation folds, which started to form during Miocene to the middle stage of Pliocene.
中部背斜带中发育的构造主要为断层转折褶皱和少量断层传播褶皱，开始形成于中新世上新世中期；
The attitude of gold ore bodies are strictly controlled by that of the strata in different parts of the Tongguanshan overturned anticline and interlayer faults.
金矿体的产状严格受铜官山倒转背斜不同部位地层岩石的产状及其层间断裂的控制。
Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion.
由于受区域构造长期作用的影响，在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂，且运动方式具有独特性。
The Dongxin oilfield is a part of the oil and gas accumulating zone in the central anticline of the Dongying depression and has very complex oil source relations.
东辛油田是东营凹陷中央背斜带复式含油气聚集带的一部分，是一个多油源汇集的地区，油源关系复杂。
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。
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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