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1)  progradational sequence
进积型沉积序列
2)  retrograding sequence
退积型沉积序列
1.
Progradational sequence and retrograding sequence both ca.
进积型沉积序列和退积型沉积序列在八道湾组辫状河三角洲中都有发育,但以退积型沉积序列为主。
3)  depositional sequence
沉积序列
1.
Based on the bore section, combining with the study on lithology, well logging, seismic facies and sequence type, the structure of the sequence in the deeply down-faulted Dongying Sag is analyzed emphasizing on the low-stand fan depositional type, its controlling factors and depositional sequence.
以钻井剖面相分析资料为基础,结合岩性、测井、地震响应特征及层序类型分析,研究东营凹陷深陷期层序的构成,着重探讨其中低位扇的沉积相类型、发育的控制因素及沉积序列。
2.
On the basis of an analysis of the characteristics of Quaternary depositional sequences and sporopollen assemblages in the Gonghe basin,combined with the thermoluminescent dating,the authors have studied the environmental change in the basin since the Quaternary and divided the change into two major phases:the early .
通过对共和盆地第四系沉积序列特征和孢粉组合特征的分析,结合热释光测年,本文较详细地研究了共和盆地第四纪以来的环境变迁,并将其分为两大阶段:早期为湖相沉积阶段(中更新世晚期~0 079Ma),气候相对温和。
3.
It can be divided into 3 depositional sequences(succession of strata), i.
可划分为三个沉积序列(层序)。
4)  sedimentary sequence
沉积序列
1.
Description of Cretaceous sedimentary sequence of the Yaojia Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系姚家组沉积序列精细描述:岩石地层、沉积相与旋回地层
2.
Description of Cretaceous sedimentary sequence of the second and third member of the Qingshankou Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系青山口组二、三段沉积序列精细描述:岩石地层、沉积相与旋回地层
3.
Description of Cretaceous sedimentary sequence of the first member of the Qingshankou Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系青山口组一段沉积序列精细描述:岩石地层、沉积相与旋回地层
5)  sedimentary succession
沉积序列
1.
Tempestite sedimentary succession have been discovered through the study of the outcrop of the up of Cambrian to the low of Ordovician in the Bachu area of the Tarim Basin.
通过对塔里木盆地巴楚达板塔格上寒武—下奥陶统剖面实测,于鹰山组上部发现风暴岩沉积序列。
2.
The feature of the sedimentary succession of the epicontinental sea basin in the study area was an- alyzed by means of the stochastic math model,Markov chain.
运用马尔柯夫链随机性教学模型对研究区陆表海盆地沉积序列特性进行了分析研究。
6)  hydrochemical depositional sequence
水化学沉积序列
1.
There are two pressure systems in the vertical direction,of which the lower high-pressure system shows reverse hydrochemical depositional sequence,while the upper part with normal pressure system has a little different hydrochemical depositional sequences in different areas.
在纵向上的两个压力系统中,下部高压层地层水发育为反向水化学沉积序列,上部常压层的水化学沉积序列在不同区域有所差异。
补充资料:动脉-动脉分流型双胎阻断序列征


动脉-动脉分流型双胎阻断序列征


  在早期如果双胎中一个胎儿的动脉压大于另一个,动脉压低者接受另一胎儿的血。用过的动脉血又注入髂血管,故注入下身的血多于上身。结果造成许多已形成和正在形成的组织发育阻断,退化而致形态发生不全成为畸形。常失去的组织有头部、心脏、上肢、肺脏、胰脏、上部肠。阻断破坏重者只留下一些残余组织,如无定形双胎,有轻有重,几乎无一例相同。供血的胎儿心脏大,代偿失调,继发肝功能异常,低血色素贫血,水肿,有时如水泡样。
  
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