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1)  measurable fuzzy set-valued mapping
可测Fuzzy集值映射
1.
This paper establishes the concept of measurable fuzzy set-valued mapping,elabroates convergences for thesequence of fuzzy set-valued mappings,and presents the integrals of measurable fuzzy set-valued mapping and itspropeties.
本文建立了可测Fuzzy集值映射,引入了Fuzzy集值映射的收敛性,并给出了可测Fuzzy集值映射的积分和它的性质。
2)  fuzzy set values mapping
Fuzzy集值映射
1.
And the relation a-mong fuzzy and fuzzy set values mapping,the properties of set values mapping,the L-fuzzy relations and elemen-tary fuzzy point values mapping are discussed as well.
本文首先用Fuzzy集合论的公理系统阐述Fuzzy关系,进而讨论Fuzzy关系与Fuzzy集值映射,Fuzzy集值映射的性质,以及L-Fuzzy关系与基本Fuzzy点值映射。
3)  Measurable set valued mapping
可测集值映射
1.
Egorov convergence theorem for measurable set valued mapping s sequence in separable and self reflexive Banach space was studied under various topological convergent meanings,almost everywhere convergent property of measurable set valued mapping sequence was discussed.
讨论了取值可分自反 Banach空间中可测集值映射序列的 Egorov型收敛定理 ,在几种不同拓扑收敛意义下 ,刻画了可测集值映射序列的几乎处处收敛 。
4)  Measurable set-valued mapping
可测集值映射
1.
On the basis of the definition of set-valued fuzzy Choquet integrals, aiming at the general measurable set-valued mapping, some important properties with respect to this kind of set-valued fuzzy Choquet integrals further were studied , which will extend the applications of this kind of integral theory.
在集值模糊Choquet积分定义的基础上,针对一般可测集值映射,进一步研究这种集值模糊Choquet积分的一些重要性质,从而使这种积分的理论具有更广泛的应用。
5)  L fuzzy set valued mapping
L-fuzzy集值映射
1.
The concepts of L fuzzy upper(lower,Vietoris) topology,upper(lower) continuity and L fuzzy continuity of L fuzzy set valued mappings in L fuzzy topological spaces are introduced Some basic properties of the three L fuzzy topologies are discussed Six character theorems respecting upper(lower) continuous and continuous L fuzzy set valued mappings and their operation properties are given as wel
研究了这 3种 L-fuzzy拓扑的基本性质 ,给出 L-fuzzy集值映射的上连续性、下连续性和连续性的 6种特征定理及其运算性
6)  measurable interval valued Fuzzy sets
可测区间值Fuzzy集
补充资料:测地映射


测地映射
geodesic mapping

测地映射[笋司比盆“.月,笔;re叭e3。,ee劝e oT浦一a盆e-““卜射影擎射(ProJ。=ti说maPping) 将空间U中的测地直线变到空间V中的测地线的映射f.测地映射f:U~V是一个局部同胚(如果U,V是光滑流形,则为微分同胚),这里U,V是测地线所在的空间. 如果一个空间局部地容许一个将它映至E让无d空间的测地映射,则此空间称为射影平粤的(侧。沈i侧yflat).一个R汹tnaxm空间到另一个R汹叮叮m空间的测地映射在例外情形下是存在的.在Rrlnalln空间当中仅仅常曲率空间才是射影平坦的(【1】).对所有射影平坦Ri。刀ann度量的描述构成了Hil伙滋第四问题([21). 在具有仿射联络的空间的理论中,人们不提测地映射,而是讨论联络的测地变换,它把联络变至同一流形上的另一个联络,且保持测地线.从联络r;、到联络弃升的变换是测地映扑如果条件f苏可苏干从呜+川必*满足,这里价,是余向量场.具有仿射联络的空间是射影平坦的充要条件是射影曲率张量为零.
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