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Les différents types d’ondes sismiques :   - 3 questions  - schéma à compléter – annoter – donner un titre
S2 S1
S2 S1 Épicentre Stations sismiques Ondes sismiques Rais sismiques foyer hypocentre Séisme et propagation des ondes sismiques
Les différents types d’ondes sismiques :  a –  Décrire l’enregistrement et établir un lien entre  le sismogramme et le séisme. ,[object Object]
correspond à un déplacement du sol donc au passage d’une onde sismique
durée très courte du phénomène  - quelques secondes,[object Object]
Chaque série commence par des oscillations de grande amplitude qui s’atténuent progressivement,[object Object]
Les différents types d’ondes sismiques :  c – Quels  paramètres peut-on utiliser pour décrire le sismogramme ? ,[object Object]
Durée du phénomène
Début de l’enregistrement des différentes ondes ,[object Object]
Heure d’arrivée des ondes 5h 53’20’’ 10’’ 53’ 00’’ 50’’ 40’’ 5h 52’ 30’’ 90 10 20 30 40 50 60 100 70 80 110 120 Distance (km) Heure d’arrivée des ondes en fonction de la distance des stations sismiques
Calcul des vitesses  Réponses attendues : Vp : 6 à 6,5 km.sec-1 Vs : 3.5 à 4 km.sec-1
III. Propagation des ondes sismiques au sein du globe  

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Tp1 correction

  • 1. Les différents types d’ondes sismiques : - 3 questions - schéma à compléter – annoter – donner un titre
  • 3. S2 S1 Épicentre Stations sismiques Ondes sismiques Rais sismiques foyer hypocentre Séisme et propagation des ondes sismiques
  • 4.
  • 5. correspond à un déplacement du sol donc au passage d’une onde sismique
  • 6.
  • 7.
  • 8.
  • 10.
  • 11. Heure d’arrivée des ondes 5h 53’20’’ 10’’ 53’ 00’’ 50’’ 40’’ 5h 52’ 30’’ 90 10 20 30 40 50 60 100 70 80 110 120 Distance (km) Heure d’arrivée des ondes en fonction de la distance des stations sismiques
  • 12. Calcul des vitesses Réponses attendues : Vp : 6 à 6,5 km.sec-1 Vs : 3.5 à 4 km.sec-1
  • 13.
  • 14. III. Propagation des ondes sismiques au sein du globe  
  • 15.
  • 16. Repérer une absence d’enregistrement des ondes P. Indiquer les distances entre l’épicentre et les stations qui n’enregistrent pas d’ondes sismiques. Disparation des ondes pour une distance angulaire comprise entre 100° et 115 ° « Zone d’ombre » Changement brutal dans la vitesse de propagation des ondes sismiques Proposer une explication à l’absence d’enregistrement d’ondes dans cette zone Existence d’une zone qui empêche le passage des ondes