• Aucun résultat trouvé

Toutes Opérations Nombres 1 à 9 (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Toutes Opérations Nombres 1 à 9 (A)"

Copied!
2
0
0

Texte intégral

(1)

Tableaux Entrées-Sorties (A)

Remplissez les cases vides. Utilisez les colonnes du milieu pour montrer votre démarche.

Règle Règle

Entrée + 3 Sortie Entrée - 4 Sortie

8 9 11 8 1 2 9 5 7 9 Règle Règle

Entrée × 7 Sortie Entrée ÷ 1 Sortie

8 4 28 7 6 9 63 5 1 6 Règle Règle

Entrée × 7 Sortie Entrée - 3 Sortie

5 5 7 4 8 1 14 2 6 3 MathsLibres.com

(2)

Tableaux Entrées-Sorties (A) Solutions

Remplissez les cases vides. Utilisez les colonnes du milieu pour montrer votre démarche.

Règle Règle

Entrée + 3 Sortie Entrée - 4 Sortie

5 8 9 5 8 11 12 8 1 4 6 2 6 9 5 1 4 7 13 9 Règle Règle

Entrée × 7 Sortie Entrée ÷ 1 Sortie

8 56 4 4 4 28 7 7 6 42 9 9 9 63 5 5 1 7 6 6 Règle Règle

Entrée × 7 Sortie Entrée - 3 Sortie

5 35 8 5 1 7 7 4 8 56 4 1 2 14 5 2 6 42 6 3 MathsLibres.com

Références

Documents relatifs

We note that a ∼55-Ma ophiolite obduction at equatorial paleolatitudes and a ∼34-Ma TH-Lhasa collision advocated by Aitchison and Ali (2) are entirely inconsistent with the

The collision between the Tibetan Himalayan microcontinent and Asia at approximately 50 Ma, and the subsequent closure of the Greater India Basin south of this microcontinent,

The paleobiogeographical distribution of chitinozoan ( “mixed layer”) marine zooplankton biotopes for the Hirnantian glacial maximum (440 Ma) are reconstructed and compared to

The results for NCEP AAM during the period of overlap with the ERA40 data (1993–2002; dashed black line) show considerable phase discrepancy with LOD, generally increasing with

base of the mantle and infer an average estimate for the mantle electromagnetic time constant from the way the signal is distorted by fitting the synthetic ridge.. functions to

The strongest detected pressure drop is 9.2 Pa (Banfield et al., 2020; Lorenz et al., 2020a), which is the deepest vortex-induced pressure drop detected to date on Mars. The sample

The rotational constants, energy values, and the angles between the internal rotor axis and the principal axes of conformer I calculated using the B3LYP and

We developed a method of estimating the EEF from magnetometer measurements of near-polar orbiting satellites as they cross the magnetic equator, by recovering a clean signal of