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The Earth's Heterogeneous Mantle
We use teleseismic body wave tomography to reveal anomalous P wave velocity variations in the upper mantle beneath south-east Australia. Data are sourced from the WOMBAT transportable seismic array, the largest of its kind in the southern hemisphere, which enables horizontal resolution of approximately 50 km to be achieved over a large region that includes Victoria, New South Wales and southern South Australia. In order to account for long-wavelength structure that is lost due to the use ofdoi:10.1007/978-3-319-15627-9_2 fatcat:kndv2dqhsbgclociv4sukyb7za