矿区位于仙鹅抱蛋背斜的东北翼。
The mining area is situated at the northeast wing of Xian'ebaodan Anticline.
背斜的岩石皱褶，核心部有柱状盐填充。
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。
Distortion phenomenon for deviated seismic height in high dipping anticline widely existed in seismic section.
霍10井是新疆油田公司准噶尔盆地南缘霍尔果斯背斜的一口重点探井。
Well Huo 10 is an important exploration well in south edge area of Zhungeer basin.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Because of the magmatite intrusion in Late Yanshan period and the formation of Xikuangshan anticline, gravitation gliding structures are developed at the both wings of the anticline.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成，在背斜两翼产生重力滑动构造。
Thrust and gravity gliding structures are both developed in the west of Lianyuan depression.
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 ore-hosted strata of Xitieshan lead-zinc ore deposit is located in a limb of a anticline and suffered from deformation partition.
戒台寺滑坡位于北京市门头沟区马鞍山的北麓，马鞍山背斜的北翼，组成边坡的岩性较为软弱。
Jietai temple landslide is located in the north wing slope of Ma anshan mountain, Mentougou district of Beijing.
背斜形态多为复式箱状背斜和不对称的斜歪背斜，分别与断层弯曲背斜和断层扩展背斜的几何形态一致。
The major morphology of the anticline is multiple box-shaped or asymmetry inclined, mostly, and it is similar to that of fault-bend fold and fault-propagation fold.
山东省莱西县南墅石墨矿位于胶东隆起栖霞复背斜的南翼，石墨赋存于太古界胶东群旌旗山组刘家庄大理岩段。
Nanshu graphite deposits, located at the south side of Qixia synclinorium in Jiaodong uplift, exist in Liujiazhuang marble member of Jingqishan formation, Jiaodong group of Archaeozic Erathern.
洪日豪(1994)台湾西部三义逆冲断块及出磺坑背斜的变形组构分析。台湾石油地质，第29号，第105 - 126页。
Hong, R. H. (1994) Analysis of deformation fabrics in the Sani thrust sheet and the Chuhuangkeng anticline of western Taiwan. Petroleum Geology of Taiwan, 29, 105-126.
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。
Controlled by structure trap, ore body located in the core of the brachyanticline or pitch part of plunging anticline which was intersected by high angle longitudinal fault.
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。
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.
鲕状灰岩可形成背斜油藏、断块油藏、地层油藏，是值得重视的油气勘探后备资源潜力。
Oolitic limestone can form anticlinal reservoirs, fault block reservoirs and stratigraphic reservoirs, and is the important reserve resource potential of the oil and gas exploration.
以往所用的取值方法是沿用背斜圈闭的要素统计方法，不能适用于复杂的断块构造圈闭。
Common trap factor calculation methods are suitable for anticlinal trap, but they are not applicable to complicated fault block traps.
有许多术语用来描述圈闭的各种参数，下面罗列了这些术语的定义，并以最简单的圈闭类型—背斜圈闭为例解释了这些术语。
Many terms are used to describe the various parameters of a trap. these terms are defined as follows and illustrated with reference to an anticlinal traps the simplest type.
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。
The salt flow resulted in several kinds of structural traps mainly including salt ridge anticline, salt dome and salt edge syncline.
综述了许多学者对逆牵引背斜构造特征和形成机理的讨论。
The structural characteristics and origin of reverse drag anticlines discussed by many authors are reviewed in this paper.
岩石磁组构反映的应力状态总体为以NE向挤压为主，与轴向NW的背斜构造发育相一致。
The stress state reflected by the rock magnetic fabric is mainly manifested by NE compression, which is consistent with the arrangement of the anticlines with axes running NW.
长坡倒转背斜控制长坡-钢坑矿床的产出，层间剪切破碎带和逆掩断层控制着矿体的空闻位置。
The Changpo reverse anticline controls the location of Changpo-Tongkeng deposit, while the bed-parallel shear fracture zone and thrust fault control the ore bodies.
转换斜坡连接一条断层的上盘和另一断层的下盘，具有特殊的变形特征，在转换斜坡近旁的断层系上盘伴生横向背斜。
They connect the hanging wall of one fault to the footwall of another fault, and have special deforming feature, beside them on the hanging wall there are transverse anticlines.
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。
Geological condition and TEM geophysical anomaly is suitable for mineralization in south flank of the anticline.
明化镇组晚期反转构造形成了众多的小背斜。
Thirdly, the reverse tectonic activities produced numerous small anticlines during the late period of the Minghuazhen Formation developing.
同时，该应力场所控制的层间破碎带和背斜，大大影响了地下空洞的成生和分布。
The research shows that the latter tectonic stress field controlled the origin and distribution of interlayer fracture zones, transverse interlayer anticlines and underground openings.
鼓山背斜是峰峰矿区的主控构造。
Gushan anticline is the main controlling structure in Fengfeng mine district.
鉴于倾斜方向的变化，此地可能存在一个局部的背斜褶皱。
In view of the variation in the dip, here could be a local anticlinal fold.
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 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.
背斜褶皱的核部在断层间受到挤压，遭受到很强的破坏。
The core of the anticlinal fold, which is squeezed between faults, underwent intense crushing.
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。
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。
Anticline and syncline, geometrical elements of fold, description and recognition of fold in the field.
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