各构造带发育不同的构造变形样式。
There are different tectonic styles in different structural belt.
赣抗构造带具明显的继承性。
其它构造带的断层形变速率都比较低。
The fault deformation rates of other tectonic zones are relatively low.
最后确定了该构造带各类原油的分布特征。
The distribution characteristics of different kinds of crude oil in this structural belt were determined.
主控矿构造为寨子湾韧- 脆性剪切构造带。
The main ore-controlling structure is Zaiziwan brittle-ductile shear zone.
盆地形成演化受特提斯构造带地球动力学控制。
Its formation and evolution was controlled by the dynamics of the Tethys tectonic belt.
北淮阳盆岭构造带是大别造山带的重要组成部分。
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
依奇克里克原油的煤系成分大于克拉苏构造带原油。
The natural gas in Ke-Yi tectonic belt is from coal measures.
吐哈盆地北部凹陷不存在大型盖层滑脱型推覆构造带。
There are no large slipping nappe structure belts on the north depression in the Turpan Hami basin.
概略陈述了新城金矿床及焦家构造带的基本地质特征。
Basic geological characteristics of Xincheng gold deposit and Jiaojia faults have been briefly stated.
该断裂带由构造混杂带和推覆构造带两个构造单元组成。
The fracture is composed of the tectonic melange zone and the nappe structure zone.
综合研究表明，坡折带是斜坡构造带油气勘探的重要方向。
Comprehensive research presents that slope break belt is the important exploration orientation in slope structural zone.
全球褶皱构造带的空间分布规律完全符合这种地球物理机制。
The space distribution regularity of global folded tectogene is well agreed with the geophysical mechanism.
北秦岭为一复杂构造带，形成向北反转的叠瓦状逆冲推覆构造。
The north Qinling is a complicated structural zone, forming an imbricated thrust napped structure overturning northward.
其特有的地质特征使泥底辟构造带广泛形成具有特色的油气藏。
Being its extra geological qualities, special oil gas reservoir come into being extensively over the mud diapiric structure belt.
秦岭纬向构造带不仅在地表发育明显，而且延伸至地幔一定深度。
Qinling latitudinal structural belt is developed very clear on the surface, and extends to a certain depth.
哀牢山构造带是云南重要的地质构造，也是云南宝玉石成矿集中区。
Ailaoshan structural belt is the important geologic structure and is also the gem concentrated mineralization area in Yunnan Province.
贝尔凹陷的北东东向和北北东向构造带是研究区有利的油气聚集带。
The disconformities in this area were important migration pathways and favorable reservoir space.
现在我将说明如何构造带附件的SOAP消息以及如何从SOAP消息引用附件。
I will now explain how a SOAP message can be constructed with attachments and how to reference an attachment from a SOAP message.
板桥断裂构造带位于板桥凹陷的东侧，受板桥凹陷和大张坨断层控制。
Banqiao rupture structural belt is located on the eastside of Banqiao sag, which is controlled by Banqiao and Dazhangtuo faults.
张秋文。张培震。王乘中国大陆若干地震构造带的地震准周期丛复发行为。
Zhang Qiuwen. Zhang Perzhen. Wang Chen Quasi-periodically clustering earthquake recurrence in some seismotectonic belts of China Continent.
新开断裂对新开鼻状断裂构造带的形成及油气的分布起着重要的控制作用。
Xinkai fault plays a important role in controlling the forming of Xinkai nose structure belt and the distribution of oil and gas.
坡洼过渡地区是已往勘探常被忽略的构造带，但却是岩性油藏形成的有利场所。
Slope-bottom land transition zone was usually neglected in previous exploration but was favorite site of forming lithologic reservoir.
研究成果很好地解释了东辛油田隆起带断裂分布与该构造带油气聚集分配的规律。
The study results correctly explained faults distribution and oil and gas accumulating in structural belt of Dongxin uplift.
自来屯油田位于黄骅坳陷南部，处于孔店潜山构造带西翼北端，孔西断层西侧北段。
Zilaitun oil field lies in the south of Huanghua depression, locating to the north part of the west limb of Kongdian submoutain and north to west of Kongxi Fault.
北部“明龙山—上窑构造带” ，是位于淮南煤田北缘由北向南逆冲的推覆构造带；
Minglongshan-Shangyao structural belt in north is other over-thrust belt with N-S direction.
不同构造带存在不同的油气成藏期次，因而油气分布在平面上及垂向上存在不均一性。
There are different pool-forming stages for different structural zones, resulting in the heterogeneity of oil-and-gas distribution both laterally and vertically.
构造带的推覆构造特征很可能控制了地震震源深度、震中区与烈度区的不同位等特征。
The characters of the nappe structure may control the locations of the focus and epicenter as well as the other features.
新的野外调查研究结果表明，六盘山东麓断裂是一条第四纪以来的活动逆断裂构造带。
New results of field investigations show that the eastern Liupanshan piedmond fault is an active reverse fault zone since late Quaternary.
该构造带的发现支持了古亚洲构造域对东北微陆块区的影响一直延续到中侏罗世的观点。
The discovery of this tectonic zone supports the view that the influence of the Paleo-Asiatic tectonic domain on the Northeast China microblock persisted till the Middle Jurassic.
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