SLIPVEC
En 1927, André Gillier, sous la marque Jil, confectionne, dans sa bonneterie de Troyes, les premiers slips à poche (slip kangourou) dont la marque s'attribue la paternité.
Quel est la différence entre culotte et slip ?
Par définition, le slip est taille baisse et plus échancré qu'une culotte.
La culotte couvre aussi plus les hanches, les cuisses et les fesses.
Par commodité, le slip est souvent associé à l'homme quand la culotte est associée au sous-vêtement féminin.
Pourquoi Appelle-t-on un slip kangourou ?
La réponse est simple : la fente transversale du slip rappelle la poche du kangourou.
C'est pourquoi le modèle s'appelle : le slip kangourou.
Savez-vous que l'idée de la poche kangourou ne vient pas d'Australie ?
Pourquoi on appelle un slip ?
Étymologie.
Attesté en (191.
3) De l'anglais slip (« ce qui glisse, ce qui permet de faire glisser ») et de l'anglais slip on ; il s'agit toutefois d'un faux anglicisme.
Dans le sens de Caleçon-ceinture pour la pratique des sports.: De correct vestons ont remplacé le slip réglementaire.
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1 CALIBRACION DE MODELO NUMERICO PARA PAQUETES DE
SlipVec = 0;. BackSlipVec = 0;. MaxStress = 0;. % run once w/ L=Le/2. ValueMap = barpull(le backendslip |
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Role of oblique convergence in the active deformation of the
INTRODUCTION. Forearcs of many subduction zones undergo rapid arc-parallel extension revealed by a sys- tematic rotation of interplate earthquake slip vec-. |
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Fig. 2. Histograms of the normalized residual azimuths between the 677 transform fault slip vectors and the directions predicted by the NUVEL-1 and NUVEL-G |
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mates of velocities along trenches where earthquake slip vec- tors are subject to systematic biases induced by forearc defor- mation [Jarrard |
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Determination of the Amurian Plate Motion
N-S slip directions are not consistent with the slip vec- tors in the Baikal Rift. We chose the westward dip- ping direction for the three reverse fault |
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Cenozoic Global Plate Motions
10 nov 1986 faults and lineated magnetic anomalies as well as slip vec- tors determined from analysis of earthquake focal mechan-. |
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Anchorage of Large-Diameter Reinforcing Bars Grouted into Ducts
function [SlipVec StressVec BackSlipVec] = testsim(L db |
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Do the 1998 Antarctic Plate earthquake and its aftershocks delineate
1 ago 2000 and/or magnetic anomaly lineations and earthquake slip vec- tors derived from centroid moment tensors. We used spread-. |
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Partition de la déformation dans un prisme daccrétion sédimentaire
The location of the deformation is showed by the homogeneity of directions of slip vector in the second series of experiments (geometry2, models 19 and 20) in |
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Demets_jgr93pdf
Fig 2 Histograms of the normalized residual azimuths between the 677 transform fault slip vectors and the directions predicted by the NUVEL-1 and NUVEL-G |
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Role of oblique convergence in the active - GeoScienceWorld
Slip vectors of thrust earth- quakes at the curved Himalayan deformation front are normal to it Seismicity (Molnar and Lyon-Caen, 1989) and active north-south– |
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Current tectonics of the Tonga-New Hebrides region - Horizon IRD
Compression (P) axes and slip vec- tors from thrust-type focal mechanisms are shown in the Fig 3, while tension (T) axes from norma and strike-slip fault type |
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Minimization of shears for pencil glide in body-centered cubic crystals
The amount of slip on each of the active slip systems is determined by maximizing the work done by the admissible stress state during plastic flow Chin and |
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Geophysical Journal International - CORE
Here slip on the interface itself is by thrust faulting with slip vectors oblique to the arc but parallel to the overall Nubia-Aegean convergence: there is no evidence |
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Interactive comment on “Seismicity and - Solid Earth
4 déc 2020 · It is only the direction of the slip vec- tor which is constrained by the orientation of the principal stress axes and the relative stress magnitude |
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Dynamic stress field of a kinematic earthquake source model with
The bimodal character of Dc/Dtot frequency–magnitude distribution was found Dc approaches the final slip Dtot near the edge of both the fault and asperity We |
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