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Image of the Moho Discontinuity with Receiver Function Analysis
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 5th Congress of Balkan Geophysical Society, May 2009, cp-126-00004
Abstract
We tried to determine the velocity discontinuities in the crust and uppermost mantle using receiver function method. After calculation of receiver functions, we convert the time axis to the depth axis and we observed 2-D images up to 80 km depth. This study showed the Moho depth changes place by place between 25 and 35 km in western Turkey.