可容空间

文中探讨了参照井选择的可容空间机理；

In this paper , accommodation mechanics to select reference well has been discussed ;

纵向上，由于各时期基准面升降造成可容空间在不同时期差别较大，因此发育的砂体类型也有一定的差别。

Since the sedimentary accommodation , caused by the changes of base level , has a great difference in geologic time , the types of sand body have vertically a certain difference .

据此，采用Fischer图解法，求取了其可容空间变化速率曲线。

The accommodation change curves of the terrigenous sequences were obtained by using Fischer diagram .

在LSC2长期旋回内，随着可容空间和A/S值的增加，中期旋回流动单元的类型呈现由劣到优的变化趋势；

In the long-term LSC2 cycle , the types of flow units in a medium-term cycle tend to upgrade with increased accommodations and A / S values ;

基准面与可容空间变化分析及应用

The Analysis of Base-level and Accommodation Space Change and Its Application

单断湖盆可容空间转化枢纽及数学证明

Accommodation Transform Hinge of Half-Graben Lacustrine Basin and Verified by Mathematics

河流平衡剖面的迁移产生陆上可容空间；

The transfer of fluvial balance sections can form subaerial accommodation space .

陆相湖盆可容空间变化与油气的关系

The Relationship between Accommodation Space Changes and Oil-Gas Reservoir

气候变化对可容空间及层序发育的影响

The influence of climate change on accommodation space changes and evolution of sequences

陆相断陷湖盆中可容空间变化特征探讨

An approach to the accommodation space changes of the fault depression lake basin

陆相湖盆古地形、可容空间的体积变化率与层序结构的关系

Relationship between Paleotopography and Volumetric Change Rate of Lacustrine Basin to the Sequence Structure

通过编制基准面变化曲线可以分析可容空间变化，预测层序发育情况。

Mapping base-level variation curve may analyze containable space and predict the sequence development situation .

可容空间持续存在，导致湖侵体系域十分发育。

Thousand-Islet Lake Continuous existence of accommodation space led to well-developed lacustrine transgressive system tracts ( LTST ) .

泌阳断陷陡坡带陆相层序发育的可容空间图解探讨

On accommodation diagram of developing mechanics of terrigenous sequence in the steep slope zone of Biyang fault depression

川西前陆盆地上三叠统须家河组二段可容空间转换系统的成因与演化

Genesis and evolution of accommodation transformation systems in 2nd member of Upper Triassic Xujiahe Formation , Chuanxi foreland basin

边界断层的活动或盆地整体坳陷产生盆地可容空间。

And the movement of boundary faults or the depression of the whole basin will produce basin accommodation space .

论述了可容空间转换系统的组成成分和划分方案。

At the same time , the composition and division scheme of the accommodation space transformation have also been expatiated .

断陷湖盆中层序发育、演化取决于相对湖平面（可容空间）的变化和沉积物供给。

Sequence development and evolution are determined by relative lake level ( accommodation ) change and sediment delivery in rift-subsidence lake basin .

陆相沉积环境与海相沉积环境有很大的差异，相应的可容空间及层序演化控制因素也不同。

There are many differences between terrestrial and marine environment with different controlling factors of corresponding containable space and the sequence evolution .

综合考虑可容空间、沉积物供给以及两者的匹配关系，建立了5种层序地层模式。

In consideration of accommodation , supply of sediments and mutual relationship of them , five kinds of sequence stratigraphy models were established .

构造运动、全球海平面变化和气候的相互作用控制了沉积物供给量以及可容空间被充填的规模。

The interaction of tectonics , change of global sea level and climate controlled the sediment supply and the scale of filled accommodation .

实际可容空间变化往往由多因素复合作用所致，尤其湖平面变化与基底构造沉降的叠合。

In general , actual accommodation change is caused by multiple factors , especially by the congruence of denivellation and basement tectonics subsidence .

受构造运动的影响，塔里木盆地志留系可容空间发生变化，沉积中心随之迁移，地层厚度发生变化。

Influenced by tectonic movements , the accommodation , the center of sedimentation and the formation thickness changed in the Silurian of Tarim Basin .

除了盆地形成、沉积充填序列受构造活动控制外，沉积层序的发育也受控于断层幕式活动引起的可容空间及沉积物供给变化的控制。

Besides , sedimentary sequence is also controlled directly by the changes of accumulation space and sediment supply resulted from episode movement of faults .

水下可容空间增量与同期供给的沉积物体积之间的对比关系控制层序的演化和体系域的形成。

The correlative relationship between increment of subaquatic accommodation space and synchronous sedimentary volume controlled the evolution of sequence and the formation of system tracts .

济阳坳陷永921地区沙四段可容空间变化速率与储层特征的关系

Relationship between reservoir quality and creative accommodation rate in the fourth member of Shahejie formation of Lower Tertiary in Yong 921 area of Jiyang Depression

这些可容空间转换系统主要是由于构造应力场的挤压沉降作用和推覆隆升作用在平面上的交互出现所致。

These accommodation transformation systems have mainly been caused by the tectonic stress fields that lead to the alternating occurrence of compressional subsidence and nappe uplifting .

基准面及可容空间变化分析，有助于对层序内部结构的认识和层序的正确识别与划分。

With the analysis of base-level and accommodation space change , we can understand the internal structure of sequence better , recognize and classify sequences more accurately .

受沉积物供给速率、可容空间增长速率及盆缘断裂产状等因素控制可划分出退积型、加积型、前积型、陡坡型和缓坡型5种扇三角洲类型。

Controlled by sediment flux rate , available accommodation expansion rate and basin-bounded fault , fan deltaic depositional system style can be generally divided into five types , i.

传统的层序地层学认为，在海（湖）平面统一升降的过程中，盆地中的可容空间的变化是统一的。

According to the classic sequence stratigraphy concept , the change of the accommodation space of the basin is unified in the seesaw process of the sea level .