这种应力场特征与上述阶段形成的盆地原型、盆地反转、构造变形相匹配。
This tectonic stress field feature is consistent with the basin prototype, basin reversal and tectonization forming in the relevant period.
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.
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.
盆地形成机制研究在深部过程控制、多重机制联合作用、幕式裂陷和反转过程等方面取得显著进展。
Recent studies have further improved our understanding of basin forming mechanism in deep processes, combined mechanism and multiple rifting and inversion.
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.
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.
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.
前述各种特征则可能是此类构造反转盆地所具有的特殊的地质构造现象。
The above mentioned characteristics may be the special geotectonic phenomena which only this kind of inversion basin has.
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.
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.
在晚侏罗世，该地区的拉分盆地由于受到阿拉善地块的东向挤压而反转。
During the Late Jurassic, this pull-apart basin reversed resulting from the eastward compression of the Alxa Block.
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.
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.
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.
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.
由此也进一步证明，吐哈原型盆地属伸展性盆地，后期则因挤压改造而发生了构造反转。
This further improves that the original Turpan-Hami basin is extensional. The basin inversion occurred caused by the compression in the later stage.
重点研究了吐哈盆地构造单元的类型、构造属性及其与构造反转之间的关系等相关问题。
This paper focuses on such related aspects as the types and attributes of tectonic units, and the relation between the tectonic units and basin inversion of Turpan-Hami Basin.
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.
对塔里木盆地北部隆起轮台断裂带进行的实例分析表明，轮台负反转断裂主反转期为中新世苏维依期一吉迪克期，反转率为0．85～0．98。
Taking Luntai fault belt of northern Tarim uplift as an example, the main negative inversion phase of the fault may be Suwiyi-Jidike epoch of Miocene, and the inversion ratio is 0.85~0.98.
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.
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.
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