The structure of Earth's crust can be imaged by various seismological methods. Among these, controlled source seismology and local earthquake tomography are the most widely used. The course will discuss the strengths and weaknesses of each method to image the crustal structure and how both methods can be combined to derive crustal models.
Lernziel
Understand the strengths and weaknesses of controlled source seismology methods and local earthquake tomography to image the structure of Earth's crust.