The estimation of crustal structure and thickness is essential in understanding the formation evolution terrestrial planets. Initial planetary missions with seismic instrumentation on board face additional challenge dealing activity levels that are only poorly constrained a priori. For example, lack plate tectonics Mars leads to low seismicity, which could, turn, hinder application many data an...

Abstract We analyze high-frequency receiver functions from two seismic stations to characterize the sediment properties around eastern coast of Kalimantan. First, we compute teleseismic events using time-domain deconvolution method. The obtained are then stacked H-κ stacking approach determine properties. computed show complicated waveforms for station located near Kutai Basin. These may indica...

The deep crustal deformation in the east Pamir response to Cenozoic collision with Tien Shan and Tarim Basin is so far poorly constrained. We present new insights into structure of its surrounding regions using P receiver functions from 40 temporary permanent seismic stations. thickness reaches a maximum 88 km beneath central southern decreases sharply 50–60 along 41–50 below Basin. most promin...