UNIQUENESS OF COMPLETE HYPERSURFACES WITH BOUNDED HIGHER ORDER MEAN CURVATURES IN SEMI-RIEMANNIAN WARPED PRODUCTS
Glasgow mathematical journal, Tome 54 (2012) no. 1, pp. 201-212

Voir la notice de l'article provenant de la source Cambridge

DOI

In this paper, we deal with complete hypersurfaces immersed with bounded higher order mean curvatures in steady state-type spacetimes and in hyperbolic-type spaces. By applying a generalised maximum principle for the Yau's square operator [11], we obtain uniqueness results in each of these ambient spaces.
DOI : 10.1017/S0017089511000541
Mots-clés : Primary 53C42, Secondary 53B30, 53C50, 53Z05, 83C99
AQUINO, C. P.; LIMA, H. F. DE. UNIQUENESS OF COMPLETE HYPERSURFACES WITH BOUNDED HIGHER ORDER MEAN CURVATURES IN SEMI-RIEMANNIAN WARPED PRODUCTS. Glasgow mathematical journal, Tome 54 (2012) no. 1, pp. 201-212. doi: 10.1017/S0017089511000541
@article{10_1017_S0017089511000541,
     author = {AQUINO, C. P. and LIMA, H. F. DE},
     title = {UNIQUENESS {OF} {COMPLETE} {HYPERSURFACES} {WITH} {BOUNDED} {HIGHER} {ORDER} {MEAN} {CURVATURES} {IN} {SEMI-RIEMANNIAN} {WARPED} {PRODUCTS}},
     journal = {Glasgow mathematical journal},
     pages = {201--212},
     year = {2012},
     volume = {54},
     number = {1},
     doi = {10.1017/S0017089511000541},
     url = {http://geodesic.mathdoc.fr/articles/10.1017/S0017089511000541/}
}
TY  - JOUR
AU  - AQUINO, C. P.
AU  - LIMA, H. F. DE
TI  - UNIQUENESS OF COMPLETE HYPERSURFACES WITH BOUNDED HIGHER ORDER MEAN CURVATURES IN SEMI-RIEMANNIAN WARPED PRODUCTS
JO  - Glasgow mathematical journal
PY  - 2012
SP  - 201
EP  - 212
VL  - 54
IS  - 1
UR  - http://geodesic.mathdoc.fr/articles/10.1017/S0017089511000541/
DO  - 10.1017/S0017089511000541
ID  - 10_1017_S0017089511000541
ER  - 
%0 Journal Article
%A AQUINO, C. P.
%A LIMA, H. F. DE
%T UNIQUENESS OF COMPLETE HYPERSURFACES WITH BOUNDED HIGHER ORDER MEAN CURVATURES IN SEMI-RIEMANNIAN WARPED PRODUCTS
%J Glasgow mathematical journal
%D 2012
%P 201-212
%V 54
%N 1
%U http://geodesic.mathdoc.fr/articles/10.1017/S0017089511000541/
%R 10.1017/S0017089511000541
%F 10_1017_S0017089511000541

Cité par Sources :