1) negative inversion structure
负反转构造
1.
The strong negative inversion structure in Mesozoic-Cenozoic is a prominent characteristic during the tectonic evolution of Dongying depression.
为了解负反转构造对东营凹陷中、新生代盆地形成过程中的意义,以高分辨率三维地震资料解释为基础,详细刻画了东营凹陷负反转构造几何学样式,并综合运用计算断层活动速率和负反转率以及编制地层位移-距离曲线等方法,对东营凹陷负反转断层运动学特征进行了系统的定量研究。
2) negative tectonic inversion
构造负反转
1.
This tectonic inversion from compressional structures to extensional structures belongs to negative tectonic inversion, characterized by reactivity of pre_existing thrusts, downsliding along the pre_existing faults surfaces and forming listric normal faults.
由于构造负反转作用，造成了前第三系分布和构造格局相对复杂的面貌，负反转构造在现今地震剖面上难以发现。
3) reversal structure
反转构造
1.
It features three structural evolution stages, showing fault depression at early stage, depression at middle stage, reversal structure at late one.
东南隆起区是松辽盆地的一级构造单元,发育了大量的伸展构造、反转构造,它们对油气的聚集、分布具有较强的控制作用。
2.
The basin evolution history is analyzed in the view of structural transition and its stage on the basis of some reversal structures founded in recent years in Jiyang depression.
依据济阳坳陷近几年发现的一些反转构造 ,从构造转型和构造转型期角度对其演化史进行了分析 ,认为济阳坳陷的演化经历过四次大的周期性构造转型 ;指出孔店组沉积时期是济阳坳陷从中、古生界构造体系向第三系构造体系转换的重要转型期。
3.
The structural style of Beier depression is very complex, which not only includes all kinds of extensional faults, extensional faulted-depression and faulted-up lift associations ,but also has transverse and longitudinal transfer zones, and reversal structures formed in later period.
贝尔凹陷的构造样式复杂,既有伸展构造体系成因的多种伸展断层和其控制的伸展断陷、断凸组合,又有横向和纵向分布的传递带以及晚期反转构造。
4) tectonic inversion
构造反转
1.
, tectonic sequence transition phase of Kongdian, developing phase of Shahejie Depression and the latest tectonic inversion phase of Dongying.
以构造层序学、层序地层学理论为指导,建立了济阳坳陷第三系构造层序体系,细致分析了每个构造层序的识别标志、层序地层学特征及构造特征,首次提出济阳坳陷下第三系构造层序经历了孔店构造层序转型期、沙河街断陷发展期、东营末期构造反转期三个演化阶段。
2.
This superimposed fold interface image of discordant axial trace (E-W and NE) developed in the Cretaceous continental basin suggests that the basin could have been the result of tectonic inversion and progressive deformation in Mesozoic under special boundary conditions when the.
这种发育在田坂陆相红盆中的以E—W向和NE向两组不同轴迹方向相复合的褶皱叠加干扰图像的成因可能是在盆地所处的特殊边界条件下,受中国东部大陆边缘活动带的控制,导致田坂盆地在中生代末发生构造反转及递进构造变形作用的结果。
3.
Evolution of sedimentation and correlation of synsedimentary structures during Ziliujing, LongJing and Early Shaximiao ages (in Jurassic) as well as stratigraphic interface features indicate that a tectonic inversion took place in Weiyuan region at the end of the Ziliujing age, forming Weiyuan uplift which represent embryo of Weiyuan anticline.
根据诛罗纪自流井期、龙井期、沙溪庙早期的沉积演化和同沉积构造特征的对比，以及各地层间和界面特征分析，认为该区自流并期末发生了构造反转，形成了威远隆起，该隆起代表了威远背斜雏形，龙井期末的构造运动使隆起进一步加强。
5) inversion structure
反转构造
1.
Summary of inversion structure on petroliferous basin;
含油气盆地反转构造研究综述
2.
HYS inversion structure in Tuha basin and its balance evolution;
吐哈盆地HYS反转构造及其平衡演化
3.
Characteristics of inversion structures in Yitong Basin since Neogene
伊通盆地新近纪以来的反转构造特征
6) inversion structures
反转构造
1.
It is revealed thatinversion structures that developed in the end of Early Cretaceous enriches the extensional structures style and provides structural trapfavorable for oil and gas accumulation.
通过综合应用地震、钻井等资料,对贝尔凹陷的形成演化进行了深入分析,认为贝尔凹陷早白垩世末期发育的反转构造丰富了伸展构造样式,提供了有利于油气聚集的构造圈闭;决定贝尔凹陷反转构造含油性的主要因素是油气生成时间、运移时间与反转时期的配置和反转强度对油气聚集的控制作用。
2.
The late stage strong inversion structures are an important characteristic of Shiwu fault depression during the process of tectonic evolution.
本文以高分辨率三维地震资料为基础,结合相干技术和三维可视化技术等先进地震资料处理和解释技术,对研究区反转构造进行了精细构造解释和研究。
3.
Based on the synthesis of the development about characteristics of geometry, kinematics and formation of inversion structures in Songliao basin, hydrocarbon accumulation and the formation of gas reservoirs with abnormal low pressures are emphasized in this paper.
文章在综述松辽盆地反转构造几何学、运动学特征及其形成机制等方面研究新进展的基础上，重点对反转构造圈闭类型与油气聚集和负压气藏成因进行了论
补充资料：负负
1.犹言惭愧﹑惭愧;对不起﹑对不起。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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