1) Accommodation space
可容空间
1.
Study on controlling factors of accommodation space for terrestrial rifted lake basin;
陆相断陷湖盆可容空间控制因素探讨
2.
Research on the accommodation space transformation system in the Es_3~z member of the Gu nan sag;
孤南洼陷古近系沙三段中亚段可容空间转换系统研究
3.
Effects of volcanic activities on the distribution of accommodation space during the development of volcanic sequence in Xinyang Depression;
阳信洼陷火山活动在层序发育晚期对可容空间的影响
2) Accommodation
[英][ə,kɔmə'deɪʃn] [美][ə'kɑmə'deʃən]
可容空间
1.
Genesis and evolution of accommodation transformation systems in 2nd member of Upper Triassic Xujiahe Formation,Chuanxi foreland basin;
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
2.
Simulation experiment on the changed characteristics of the accommodation in faulted lacustrine basins;
断陷湖盆可容空间变化特征的模拟实验研究
3.
Influenced by tectonic movements,the accommodation,the center of sedimentation and the formation thickness changed in the Silurian of Tarim Basin.
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。
3) accommodation
[英][ə,kɔmə'deɪʃn] [美][ə'kɑmə'deʃən]
可容纳空间
1.
The concepts of base level of deposition and accommodation are the theoretic foundation of the high-resolution sequence stratigraphy, illuminating, the incorporate relationship of denudation, transport and deposition in sedimentary basin in origin.
沉积基准面、可容纳空间是高分辨率层序地层学的理论基础之一,其从成因上解释了沉积盆地物质剥蚀、搬运与沉积的一体化关系。
2.
The analysis of the accommodation change mechanism and features in a reversed structure based on its evolution characteristics in the basin r.
根据松辽盆地的构造演化特征,讨论了构造反转背景下可容纳空间的变化机制和特征,认为在构造反转背景下影响可容纳空间的主要因素有以下3种:①受挤压所导致的扭曲变形引起盆地基底局部的下沉和缓慢的沉降;②沉积物的重力差异压实导致盆地均衡失调引起基底的差异沉降;③挤压作用引起沉积物供应效率的变化。
3.
Furtherly in the light of the high or low accommodation, and the thickness of the uprising periods .
以高分辨率层序地层学理论和技术方法为指导 ,运用短期基准面旋回界面的识别标志将百色盆地那读组短期基准面旋回层序划分为向上“变深”的非对称型 (A型 )、向上变浅的非对称型 (B型 )、向上变深复变浅的对称型 (C型 )等三种基本结构类型 ,再根据可容纳空间大小和上下两个半旋回的厚度进一步划分为七个亚类型 :即低可容纳空间向上“变深”的非对称型 (A1型 ) ,高可容纳空间向上“变深”的非对称型 (A2 型 ) ,低可容纳空间向上变浅的非对称型(B1型 ) ,高可容纳空间向上变浅的非对称型 (B2 型 ) ,完全—近完全对称型 (C1型 ) ,以上升半旋回为主的不完全对称型 (C2 型 ) ,以下降半旋回为主的不完全对称型 (C3 型 )。
4) accommodation space
可容纳空间
1.
Sequence stratigraphy of the Silurian strata and accommodation spaces in central Tarim Basin,Xinjiang;
塔中志留系层序及其可容纳空间分析
2.
Research on the Kuqa foreland basin in Northern Tarim basin and previous studies on lithospheric flexural simulations of foreland basins show that accommodation space from the forebulge to the foredeep develops inconsistently due to compressional tectonism, which results in the forebulge rising while the foredeep subsides.
结合前人对前陆盆地岩石圈挠曲变形模拟的认识,经过对库车前陆盆地的实例分析 表明,前陆盆地挤压构造活动引起前渊带沉降、而前隆带隆升,导致可容纳空间发育在横向上不协调。
5) accommodation diagram
可容空间图解
6) transformation of accommodation space
可容纳空间转换
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