Abstract
<span>It has been done a research to determine internal earth using receiver function teleseismic analysis <span>method. This method have been done by using MERAMEX (MErapi Amphibious Experiment) data from <span>broadband seismometer BKB. Event of teleseismic is chosen from Honshu Japan with radius 30<span>o <span>and <span>magnitude 7.2. This research begun by analysing radial and vertical characteristic of teleseismic event<br /><span>and using bandpass filter with range 0.003 Hz – 0.5 Hz. Then Iteractive Deconvolution is used to get <span>velocity model. The result of this model shows crustal model that has 4 Km thick upper crust, a 26 Km <span>thick lower crust and 10 Km thick Moho transition zone, with velocity increasing gradually.</span></span></span></span></span></span><br /></span></span></span>
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