转换带

苏丹福拉凹陷转换带特征及其与油气的关系

Transfer zone character and its relationship to hydrocarbon in Fula Sag , Sudan

转换带可以形成有利于油气聚集的构造或圈闭；

The transfer zone may form structures or traps that are prone to hydrocarbon migration and accumulation .

石榴子石的高温塑性：地幔转换带的流变特性

High temperature plasticity of garnets : rheology of the mantle transition zone

龙门山构造转换带对油气成藏的控制作用

Control of transfer zones on hydrocarbon accumulation in Longmen Mountains thrust belt

构造转换带精细研究及非构造油气藏勘探

Detailed Study of Structural Transposition Zone and Exploration of Non - Structural Reservoir

高邮凹陷构造转换带控油机制研究与实践

Research and Implementation of Oil-control Mechanism in the Transition Section of Gaoyou Depression

转换带密集发育的断裂系统为油气的运移和聚集提供通道。

The dense faults in the zone provide channel for hydrocarbon migration and accumulation .

砂岩脆－韧性变形转化的特征东天山脆-韧性变形转换带与金矿带

The brittle - ductile deformation transition zone and gold deposit belt in eastern Tianshan

挤压区局部构造转换带类型及石油地质意义

Types of Structural Transfer Zone in Compressional Area and Its Significance of Petroleum Geology

转换带对油气聚集的影响贯穿油气成藏的整个过程。

The effect of the zone to hydrocarbon accumulation exists in the whole reservoir-forming process .

调节带和转换带及其在伸展区的分段作用

Accomodation Zones and Transfer Zones and Their Roles in the Segmentation of the Extended Terranes

天山陆内俯冲造山转换带的基本特征

The transfer zone within intra continent subduction orogenic belt in the tianshan , Northwest China

在区域上，脆韧性剪切转换带是金矿的有利成矿部位。

The transitional place of the ductile-brittle shear zone is the favorable position for gold mineralization .

该转换带开始形成于早白垩世第一裂谷期，在晚白垩世第二裂谷期，断裂再次活动，转换带基本定型；

During the second rifting phase in Late Cretaceous , faults reactive and the zone is finalized .

其中当伸展量增加时，高凸起转换带可能发展为低凸起转换带。

Convergent and synthetic transfer zones of high relief may develop into low relief ones as stretch gets large .

福拉凹陷转换带位于中部构造带，是重要的含油气构造带。

Fula Transform Zone in the middle structural zone is formed during the first rifting phase in Early Cretaceous .

根据新西兰从消减至走滑的板块边界转换带的地方震来研究地震各向异性

Seismic anisotropy from local earthquakes in the transition region from a subduction to a strike-slip plate boundary , New Zealand

沉积期后构造转换带，使储集层构造特征发生变化，各种非构造油气藏集中分布。

In post-depositional structural transposition zone , central distribution of a variety of non-structural reservoirs takes place due to variation of reservoir characteristics .

据现有大中型金矿研究建立了区域脆-韧性变形转换带结构模式和金矿预测模式，可有效指导找矿勘探。

A model for gold prognosis and regional brittle-ductile shear deformation transition was set up by study of the known large-and middle-scale gold deposits .

川滇应力区东边界（东边的应力转换带）基本上与川滇菱形块体的东边界相吻合；

The eastern boundary of Sichuan-Yunnan stress zone ( the eastern stress transition belt ) is basically consistent with the eastern boundary of Sichuan-Yunnan rhombic block .

铲形正断层围限块体的滑脱深度达到或超过脆韧性转换带深度，为20&30公里。

The detachment depth of the tilted block controlled by listric normal fault is about 20-30km , which reaches and exceeds the depth of brittle-ductile transition zone .

该带不仅是一个地理界线，而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。

It serves not only as a geographic boundary but also as pre-tertiary en-echelon drapes and a Cenozoic tectonic conversion zone controlled by the basement fault zone .

断层转换带多分布在断层的交汇处、拐弯处和末端处，是伸展、走滑构造应力场联合、复合作用的产物。

Fault transfer zones grow on the cross ; round and the end of faults generally , are the effect of extensional , strike slip , and inversion structural stress .

构造转换带内部构造变形复杂，控制了地层分布，其内部密集的断裂体系有利于形成相关构造圈闭，同时也为油气运移提供了有效通道。

The complex structure deformation interior of structural transfer zone can control the distribution of strata , be used as the favorable channel for hydrocarbon , and then form effective hydrocarbon traps .

认为研究区局部物源可以分为三种沉积物源体系，分别为：断槽物源沉积体系、垂向沉积物源体系和转换带沉积物源体系。

It is concluded that the local provenance can be divided into three systems , respectively : fault-trough sedimentary provenance system , the vertical sedimentary provenance system and transfer zone sedimentary provenance system .

转换带可划分为5种类型：离散型转换带，汇聚型高凸起与低凸起转换带，同向型高凸起与低凸起转换带。

Transfer zones are divided into 5 types in this paper : divergent transfer zone , convergent transfer zones of high relief and low relief , synthetic transfer zones of high relief and low relief .

应用断层转换带的理论，识别出东辛油田的11个断层转换带，分为4种类型（平行同向断层型，平行对向断层型，叠覆断层型，趋近断层型）。

Based on the transfer theory of fault , 11 fault transfer zones are identified , which belong to 4 types ( collateral synthetic , collateral convergent , overlapping , and approaching transfer styles ) .

结果表明，旋转平面状正断层围限块体的滑脱深度与脆韧性转换带上顶面深度一致，为10&15公里；

The calculated result shows that the detachment depth of the tilted block controlled by rotational planar normal fault is about 10-15km , which is the same as the depth of the top surface of brittle-ductile transition zone ;

在脆性和脆-韧性转换带，制约苏鲁高压-超高压变质带侵位的主导应力作用方式为自南东东往北西西方向的挤压，它在时间和空间上具有一定的稳定性。

In the brittle and brittle-ductile transition belts , the dominant mode of stress action constraining the emplacement of the Sulu high-pressure and ultrahigh-pressure metamorphic belt is ESE-WNW compression , which shows certain stability in time and space .

主可容空间转换带是目前发现气藏数量最丰富，产量最高的地区，也是目前的技术条件所能达到的现实勘探目标区。

Presently , the primary accommodation transformation zones are the most prolific gas areas where the largest number of gas reservoirs have been discovered , and they are also the practical exploration target areas at current technical conditions .