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1)  sequential product
序列积
1.
Then by comparing ◇-product with the sequential product,we give some algebraic properties of ◇-products and some counter examples.
通过量子计算和量子信息理论中两个物理量concurrence和fidelity引入正算子方块积的概念,类比序列积代数性质的相关结果,给出了方块积的一些代数性质和反例,并对不同H ilbert空间之间保持concurrence或fidelity的变换进行了刻画。
2.
For every A,B or A,B P(H),we defined the sequential product of A,B by AB= ABA.
本文主要研究序列积的相关代数性质。
2)  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)。
3)  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
4)  strata accumulation series
垒积序列
5)  product sequence
乘积序列
6)  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。
补充资料:积积
1.长久累积。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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