Geodesic
Infinitely small bending slipping of component surfaces of revolution
Matematičeskie zametki, Tome 10 (1971) no. 5, pp. 549-554.

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Necessary and sufficient conditions are found such that the internally coalesced surface $\Sigma=S_1+S_2$ should have a parallel $L\in S_2$ which divides the surface $\Sigma$ into two parts so that the part $\Sigma_L$, which does not contain a pole of the surface $S_2$, should permit nontrivial bending slipping along $L$. 
@article{MZM_1971_10_5_a9,
     author = {I. Ivanova-Karatopraklieva},
     title = {Infinitely small bending slipping of component surfaces of revolution},
     journal = {Matemati\v{c}eskie zametki},
     pages = {549--554},
     publisher = {mathdoc},
     volume = {10},
     number = {5},
     year = {1971},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/MZM_1971_10_5_a9/}
}
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I. Ivanova-Karatopraklieva. Infinitely small bending slipping of component surfaces of revolution. Matematičeskie zametki, Tome 10 (1971) no. 5, pp. 549-554. http://geodesic.mathdoc.fr/item/MZM_1971_10_5_a9/