该区的地震资料证实有正反转构造存在。
The existence of inverted structures can be proved by seismic data in this area.
正反转构造可分为单一型和复合型2大类。
The structures can be divided into 2 kinds: single type and composite type.
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.
负反转构造对潜山油气藏的形成具有重要意义。
The negative inversion structure is of importance for the formation of buried hill reservoirs.
提出了反转构造的定义，分类及反转构造与油气藏的关系。
This paper presents the definition, classification of tec-tonic inversion and its relationship with forming hydrocarbon reservoirs.
负反转构造中可常见风化壳储层，为油气储集创造有利条件。
Weathering crust reservoirs are common in negative reversal structures, which are also favorable to hydrocarbon accumulation.
负反转构造中可常见风化壳储层，为油气储集创造有利条件。
In positive reversal structures, the moderate extent of ones are most favorable to hydrocarbon accumulation but texture o...
之后在左旋压扭应力场作用下，形成了盆地西北部的反转构造；
After 24Ma B. P. , with the stress field of the sinistral rotation and compressive shearing, formed the reverse structure in the northwestern basin.
区域上组成二个东西向反转构造带：北带为商丘-新郑反转构造带；
Its consist of two structural inversion zones in west-eastern direction:the northern zone is ShangQiu-XinZhen and the southern is LuYi-PingDinShan.
负反转构造和断块型古潜山普遍存在于东营凹陷通王地区古生界之中。
Negative reversal structure and the fault - block type buried hills are very common in Palaeozoic group in Tongwang area of Dongying Sag.
以地表地质和勘探地震资料为基础，对洛阳盆地的负反转构造进行了研究。
The negative inverted structure in Luoyang basin is studied on the basis of geological data and prospecting seismic data.
每种反转构造在演化过程中均形成与潜山油气藏有关的、特定的成藏条件。
Each reverse structure has formed distinctive reservoir condition related with buried hill type...
松辽盆地的反转构造以宽缓的褶曲和长垣背斜为主，属小变形量的反转构造。
Reverse structures in Songliao basin are mainly wide and gentle folds and placanticline with small deformation.
此外，新方法技术的综合运用是盆山一体化反转构造研究的重要支撑和必然趋势。
Moreover, the comprehensive application of new methods and technology is an inevitable trend in the research of basin-orogen integration for inversion tectonics.
多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构。
Complicated tectonic styles and geological structures were generated by multi-episodic rifting and inversion.
负反转构造是断块型古潜山形成的主要因素，其构造演化决定了断块型古潜山的形成。
Negative reversal structures are the main factors of forming fault - block type buried hills and their structural evolution determined forming the fault - block type buried hills.
重点论述中国近海盆地的正反转构造，并探讨正反转构造的形成机制及石油地质意义。
The paper focuses on the positive inversion structures in China offshore basins, and discusses their mechanism of formation and significance to petroleum geology.
该周期控制了盆地内的沉积与剥蚀的过程及成藏旋回，并至少控制了古生代的反转构造。
All of the processes no matter what of deposition, erosion or entrapment cycles and, at least the inversion tectonics of Paleozoic, are all controlled b.
松辽盆地主要经历了伸展构造期和反转构造期两个构造时期，形成了复杂的构造裂缝组系。
The Songliao Basin experienced the extensional and reversal tectonic stages, which resulted in a complex structural fracture system.
反转构造与油气成藏密切相关，目前西湖凹陷已发现油气储量的90 %与反转构造有关。
The inversion structures are closely related to hydrocarbon accumulation, and about 90% of the reserves discovered are associated with these structures in the sag.
大庆长垣位于松辽盆地中部坳陷区，其内部的反转构造主要分为断层控制型和非断层控制型。
Daqing Changyuan lays on middle sag region of Songliao basin. The reversal construct in its interior mostly divided into dislocation-controled type and not dislocation-controled type.
大杨树盆地经历了多期变形作用，具有以伸展构造为主、并被挤压构造和反转构造叠加的构造特征。
Dayangshu Basin experienced multistage deformations, which is characterized mainly by extensional structures, and was superimposed by compressional structures and positive inversion structures.
盆地早期的构造样式均为半地堑式箕状凹陷，晚期均发生方式不同的的构造反转，形成全反转的逆冲推覆和半反转的正或逆反转构造。
The structural styles of the basins in early stage are all half-graben depression and in late stage are total-reverse thrust nappe and semi-reverse normal- or abnormal-reverse structures.
在系统分析北部湾盆地涠西勘查区地震剖面的基础上，认为北部湾盆地涠西勘查区发育两期反转构造即渐新世末期及中新世末期反转构造。
It was indicated that there were two different inversion structures formed in two period based on analysis of seismic profiles in Weixi exploration region of the Beibuwan Basin.
采用零点、距离位移曲线和生长指数等定量分析方法，讨论了断裂的构造负反转过程。
By means of the null point, growth index analysis and displacement distance plot, the authors discussed the process of negative structure inversion.
对剖面中反映的构造反转、褶皱组合样式、逆冲断裂带、直立地层发育带的构造特征进行了探讨。
Structural characteristics of inversion structure, fold association style, thrust fault zone upright strata developed belt shown in great profiles were also discussed.
经晚白垩世和新近纪的构造反转改造后，呈改造残留型含油气、含煤盆地。
After reverse tectonic period in Late Cretaceous and Neogene, it became a relict basin with oil-gas and coal.
早—中侏罗世研究区处于一种张扭构造环境之中，晚侏罗世盆地发生明显抬升和反转。
The study area was in a tectonic setting of transtension during Early and Middle Jurassic, and the basins were reversed and uplifted in Late Jurassic.
早—中侏罗世研究区处于一种张扭构造环境之中，晚侏罗世盆地发生明显抬升和反转。
The study area was in a tectonic setting of transtension during Early and Middle Jurassic, and the basins were reversed and uplifted in Late Jurassic.
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