1) Fault-depressed stagnant lacustrine basin
断陷闭流湖盆
2) closed depression lacustrine basin
闭流坳陷湖盆
1.
Type Ⅰclimatic sequence of an integrated closed depression lacustrine basin is composed of four parasequences: LPWST,TST,HST and FRWST.
闭流坳陷湖盆以发育气候层序为特征,在理想条件下,气候三级周期的变化基本符合正弦曲线;一个完整的闭流坳陷湖盆气候层序Ⅰ型层序应包括4个体系域:低水位进积楔体系域、水进体系域、高位体系域和强制水退楔体系域;同样一个完整的闭流坳陷湖盆气候层序Ⅱ型层序应包括3个体系域:水进体系域、高位体系域和强制水退边缘体系域。
3) faulted lake basin
断陷湖盆
1.
Classification and distribution of glutenite on the steep slope of faulted lake basin in Jiyang depression;
济阳坳陷断陷湖盆陡坡带砂砾岩体分类及展布
2.
The western Liaohe depression belongs to a faulted lake basin.
辽河西部凹陷属断陷湖盆,这种湖盆中的旋回沉积层序的格架不同于被动大陆边缘型盆地的沉积层序格架,可用湖进—湖退(T—R)旋回来进行描述。
4) faulted lacustrine basin
断陷湖盆
1.
Terrestrial sequence stratigraphy and lithological deposit group of sandstone in Jiyang faulted lacustrine basin;
济阳断陷湖盆层序地层学及砂砾岩油气藏群
2.
Discussion on the changing patterns of base-levels in faulted lacustrine basins;
断陷湖盆基准面变化模式探讨
3.
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
5) fault depressed lacustrine basin
断陷湖盆
1.
Based on analysis of the sedimentary response to the variation in accommodation space at different structural positions of the steep slope zone in the fault depressed lacustrine basin, accommodation mechanism for the selecting of a reference well has been discussed, and the principle for the selecting of a reference well has been put forward.
在分析断陷湖盆陡坡带不同构造部位的可容空间变化规律及其沉积响应特征的基础上 ,探讨了断陷湖盆陡坡带参照井选取的可容空间机理 ,并阐明了参照井的选择原则 ;根据参照井处的沉积相迁移特征及体系域叠置样式 ,建立了在参照井的背景下 ,Ⅰ型与Ⅱ型陆相层序划分及其层序界面判识标准 ,以及低水位体系域 (LST)、水进体系域 (TST)、高水位体系域 (HST)及水退体系域 (RST)的识别模式。
6) rift lake basin
断陷湖盆
1.
In a rift lake basin, the differential subsidence of basement in the gentle slope zone of the basin resulted from the episodic movement of boundary faults in the basin can lead to the discordant changes of relative and absolute lake level, water depth and other parameters, that is, the discordant changes of relative lake level, absolute lake level and water depth and those of relative lake lev.
在断陷湖盆中,由于盆地边界断层的幕式活动,导致盆地缓坡带基底发生差异沉降,相对湖平面、绝对湖平面和水深等参数可出现不统一的变化,主要表现在以下两个方面:a)相对湖平面、绝对湖平面和水深3个参数间出现不统一性变化;b)相对湖平面或水深在湖盆的不同构造位置出现不统一性变化。
补充资料：断闭
1.犹隔绝。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条